Sentences Generator
And
Your saved sentences

No sentences have been saved yet

420 Sentences With "most tropical"

How to use most tropical in a sentence? Find typical usage patterns (collocations)/phrases/context for "most tropical" and check conjugation/comparative form for "most tropical". Mastering all the usages of "most tropical" from sentence examples published by news publications.

type: All Declarative Interrogative Exclamative

structure: All Simple Compound Complex Compound-Complex

length: All <=10 words 10-20 words 20-30 words 30-50 words

After working for decades, you may be tempted to find the most tropical, relaxing destination on the map.
Kardashian West called the Pink Lips scent the most tropical with lots of coconut (without smelling like overpowering sunscreen!).
A: Most tropical storms are "steered" by winds that push them along, including over land where they eventually lose power.
Chasing the Deal It's high season in most tropical destinations, but a few deals can be found, especially at all-inclusive resorts.
Rubber Plant (Ficus elastica): The deep burgundy leaves on these beauties make them a stand-out among the deep green of most tropical plants.
Good news for all the teachers out there: The U.S.'s most tropical state is in super-recruiter mode for its Department of Education.
Then on Friday and Saturday, Florence may be drawn to the southwest, moving in the opposite direction compared to most tropical storms and hurricanes in this region.
And, as with most tropical locations, the weather might not always cooperate with your plans, so it might be wise to wait until you arrive to plan off-site activities.
"Whereas most tropical regions are likely to experience production losses due to rising temperatures, production in temperate regions is expected to benefit from warmer climate and longer growing seasons," the report said.
With most tropical storms and hurricanes, the strong winds are felt much farther from the center, and the clouds extend outward as much as 1,000 miles away from the actual center of the hurricane.
The U.N. Development Programme report shows that staying under 1.5 degrees of warming would reduce by a full month the length of extreme heat waves each year for most tropical regions by mid-century, compared with 2 degrees.
They are less picky about water quality than most tropical fish, and thus make good beginner's fish.
Most tropical cyclones impacting California do so in the month of September. September 1939 was "unprecedented" in having four tropical cyclones impact the state.
The 1992 Pacific typhoon season had no official bounds; it ran year-round in 1992. Despite this, most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. In the West Pacific basin, tropical depressions have the "W" suffix added to their number.
This species has one of the widest distributions within the family, being known from most tropical areas. It favors bog environments. Palhinhaea cernua is sometimes cultivated.
The larvae feed on decaying vegetable matter and carrion. Distribution is now most tropical and temperate regions worldwide, having been introduced. In Europe it is mainly Mediterranean.
They are found in most tropical and many subtropical regions all over the world, particularly in Africa, Asia, islands in the Pacific, tropical America, and southeastern Europe.
The 1979 Pacific typhoon season featured the most intense tropical cyclone recorded globally, Typhoon Tip. The season also experienced above-average tropical cyclone activity. The season had no official bounds; it ran year- round in 1979, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The Danish band Laid Back made a song titled "Sunshine Reggae" with a tropical-feel, and since then, most tropical styled reggae has been known as Sunshine Reggae.
The 1999 Pacific typhoon season was the last Pacific typhoon season to use English names as storm names. It was a very inactive season, featuring the lowest number of Typhoons on record. It had no official bounds; it ran year- round in 1999, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
Crenicichla is a genus of cichlids native to South America commonly known as the pike cichlids. They are found in most tropical and subtropical freshwater habitats between the Andes and the Atlantic.
The 1969 Pacific typhoon season was the fourth least-active season on record. The season had no official bounds; it ran year-round in 1969, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line.
Today this species occurs as a weed in most tropical regions. It can be found in North, Central, and South America, many Pacific Islands, Asia, parts of Africa outside its native range, and Australia.
The 1983 Pacific typhoon season has no official bounds, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2007-01-05.
The 1984 Pacific typhoon season has no official bounds, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1952 Pacific typhoon season had no official bounds, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1952 Pacific hurricane season.
The 1945 Pacific typhoon season was the first official season to be included in the West Pacific typhoon database. It has no official bounds; it ran year- round in 1945, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line.
The 1964 Pacific typhoon season was the most active tropical cyclone season recorded globally, with a total of 39 tropical storms forming. It had no official bounds; it ran year-round in 1964, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, Hurricane Anna, developed in the eastern Caribbean Sea near the Windward Islands on July 20\.
The 1995 Pacific typhoon season occurred all year round, unusual in that most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1941 Pacific typhoon season has no official bounds; it ran year-round in 1941, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1941 Pacific hurricane season.
The 1942 Pacific typhoon season has no official bounds; it ran year-round in 1942, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1942 Pacific hurricane season.
The 1943 Pacific typhoon season has no official bounds; it ran year-round in 1943, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1943 Pacific hurricane season.
The 1944 Pacific typhoon season has no official bounds; it ran year-round in 1944, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1944 Pacific hurricane season.
The 1955 Pacific typhoon season has no official bounds; it ran year-round in 1955, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1955 Pacific hurricane season.
The 1954 Pacific typhoon season has no official bounds; it ran year-round in 1954, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1954 Pacific hurricane season.
The 1953 Pacific typhoon season has no official bounds; it ran year-round in 1954, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1953 Pacific hurricane season.
The 1950 Pacific typhoon season has no official bounds; it ran year-round in 1950, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1950 Pacific hurricane season.
The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line.
The 1946 Pacific typhoon season has no official bounds; it ran year-round in 1946, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1946 Pacific hurricane season.
The 1971 Pacific typhoon season has no official bounds; it ran year-round in 1971, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1971 Pacific hurricane season.
The 1972 Pacific typhoon season has no official bounds; it ran year-round in 1972, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1972 Pacific hurricane season.
The 1973 Pacific typhoon season has no official bounds; it ran year-round in 1973, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1973 Pacific hurricane season.
The 1957 Pacific typhoon season has no official bounds; it ran year-round in 1957, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1957 Pacific hurricane season.
The 1956 Pacific typhoon season has no official bounds; it ran year-round in 1956, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1956 Pacific hurricane season.
The 1960 Pacific typhoon season had no official bounds; it ran year-round in 1960, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1960 Pacific hurricane season.
The 1961 Pacific typhoon season had no official bounds; it ran year-round in 1961, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1961 Pacific hurricane season.
The 1968 Pacific typhoon season has no official bounds; it ran year-round in 1968, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1968 Pacific hurricane season.
The 1967 Pacific typhoon season has no official bounds; it ran year-round in 1967, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1967 Pacific hurricane season.
The 1978 Pacific typhoon season was a very active season that produced 31 tropical storms, 16 typhoon and one intense typhoon. It has no official bounds; it ran year-round in 1978, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line.
The 1965 Pacific typhoon season has no official bounds; it ran year-round in 1965, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1965 Pacific hurricane season.
The 1975 Pacific typhoon season was one of the deadliest tropical cyclone seasons on record, with nearly 230,000 fatalities occurring during the season. It had no official bounds; it ran year-round in 1975, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center.
The 1970 Pacific typhoon season has no official bounds; it ran year-round in 1970, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Dateline. Storms that form east of the date line and north of the equator are called hurricanes; see 1970 Pacific hurricane season.
The 1976 Pacific typhoon season has no official bounds; it ran year-round in 1976, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1976 Pacific hurricane season.
The 1949 Pacific typhoon season has no official bounds; it ran year-round in 1949, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1949 Pacific hurricane season.
The 1948 Pacific typhoon season has no official bounds; it ran year-round in 1948, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1948 Pacific hurricane season.
The 1947 Pacific typhoon season has no official bounds; it ran year-round in 1947, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1947 Pacific hurricane season.
The 2001 Pacific typhoon season has no official bounds; it ran year-round in 2001, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 2001 Pacific hurricane season.
The 1939 Pacific typhoon season has no official bounds; it ran year-round in 1939, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1939 Pacific hurricane season.
The 1982 Pacific typhoon season had no official bounds; it ran year-round in 1982. On average, most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary.
The 1996 Pacific typhoon season has no official bounds; it ran year-round in 1996, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1993 Pacific typhoon season has no official bounds; it ran year-round in 1993, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1991 Pacific typhoon season has no official bounds; it ran year-round in 1991, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved August 26, 2006.
The 1988 Pacific typhoon season has no official bounds; it ran year-round in 1988, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1987 Pacific typhoon season has no official bounds; it ran year-round in 1987, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2006-08-26.
The 1974 Pacific typhoon season was the only season on record to not feature a Super Typhoon. It has no official bounds; it ran year-round in 1974, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The 1974 season was at the time the only season to not produce a Category 5 equivalent typhoon, a feat that would not be matched until 3 years later and 43 years later.
The 1980 Pacific typhoon season has no official bounds; it ran year-round in 1980, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms which formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA.
The 1986 Pacific typhoon season has no official bounds; it ran year-round in 1986, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA.
The 1985 Pacific typhoon season has no official bounds; it ran year-round in 1985, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA.
Most tropical cyclones form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies.Joint Typhoon Warning Center (2006). 3.3 JTWC Forecasting Philosophies. United States Navy.
The 1990 Pacific typhoon season was another active season. It has no official bounds; it ran year-round in 1990, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary.
Pinguicula gigantea is a tropical Mexican species of Pinguicula. Its dormancy is not regulated by temperature or light. Like most tropical species, its dormancy is triggered by lack of moisture. Very little precipitation falls during the winter in Mexico where this Pinguicula species lives.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Northeast Pacific basin. However, the formation of tropical cyclones is possible at any time of the year. This was shown when a tropical depression formed on December 31\.
The 1989 Pacific typhoon season was a highly above-average season. It has no official bounds; it ran year-round in 1989, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary.
The equator runs through the middle of Africa, as do the Tropic of Cancer and the Tropic of Capricorn, making Africa the most tropical continent. The already hot and dry climate that straddles the equator, makes it the most vulnerable continent to climate change.
Stingless bees can be found in most tropical or subtropical regions of the world, such as Australia, Africa, Southeast Asia, and tropical America.Michener, C D. The bees of the World. Johns Hopkins University Press, 972 pp.Silveira, F A; Melo, G A R; Almeida, E A B. 2002.
The 1981 Pacific typhoon season was a slightly above average season that produced 29 tropical storms, 13 typhoons and two intense typhoons. The season ran throughout 1981, though most tropical cyclones typically develop between May and October.Gary Padgett. May 2003 Tropical Cyclone Summary. Retrieved 2007-01-05.
In the Central Pacific Hurricane Center's (CPHC) area of responsibility (AOR), the season with the most tropical cyclones is the 2015 season with 16 cyclones forming in or entering the region. A season without cyclones has happened a few times since 1966, most recently in 1979.
Relative to other species (pearl millet and sorghum), finger millet has a higher tolerance to cool temperatures. It is grown from about 500 to about 2400 m above sea level (e.g. in Himalaya region). Hence, it can be cultivated on higher elevations than most tropical crops.
Tunga penetrans (chigoe flea or jigger) is a parasitic insect found in most tropical and sub-tropical climates. It is native to Central and South America, and has been inadvertently introduced by humans to sub-Saharan Africa.Cestari TF, Pessato S, Ramos-e-Silva M Tungiasis and myiasis. Clin Dermatol.
Only a few genera are pantropical (e.g. Ixora, Psychotria), many are paleotropical, while Afro-American distributions are rare (e.g. Sabicea). Endemic rubiaceous genera are found in most tropical and subtropical floristic regions of the world. The highest number of species is found in Colombia, Venezuela, and New Guinea.
The Aulopidae are a small family of aulopiform fish. They are found in most tropical and subtropical oceans, and are commonly known as flagfins. The aulopids resemble lizardfishes in appearance, and range up to in length. They have large dorsal fins, the first ray of which is greatly extended.
These dates fall within the period with the most tropical cyclone activity in the Atlantic. No tropical cyclones during this season existed simultaneously. One tropical cyclone has a single known point in its track due to a sparsity of data. Of the season's five tropical cyclones, three reached hurricane status.
Living coral ranges in colour from white to orange-red. Unlike most tropical corals, the polyps are not interconnected by living tissue. Each polyp has up to 16 tentacles and is a translucent pink, yellow or white. Some colonies have larger polyps while others have small and delicate -looking ones.
Common names of Senna sophera include algarrobilla, kasunda, baner. It was formerly called Cassia sophera in English. It is known as kasaundi in Hindi, and kolkasunda (কল্কাসুন্দা) in Bengali. Possibly originating in Bangladesh,Entry for Senna sophera (Linn) Roxb JSTOR Plant Science today the plant is found in most tropical countries.
K. Vanangamudi, V. Anbukkarasi and M. Prabhu The bark can produce fibre of good quality. It is evergreen in most tropical climates. Elsewhere, in the spring, the fresh new leaves are bright green with a bronze hue. The mature leaves are large, deep green, shiny, and hirsute (hairy), especially underneath.
The Families and Genera of Vascular Plants volume VI. Springer- Verlag: Berlin;Heidelberg, Germany. The Huerteales are shrubs or small trees found in most tropical or warm temperate regions. The flowers of Perrottetia have been studied in detail,Merran L. Matthews and Peter K. Endress (2005). "Comparative floral structure and systematics in Celastrales".
Macrouroidinae is a subfamily of rattails from the family Macrouridae, it contains only two species in two genera found in most tropical and temperate ocean. These species lives in deep-water. These fishes have a huge and rounded head with consistency of water-filled balloon, eyes tiny. The chin barbel is absent.
Almost all commercial papaya orchards contain only hermaphrodites. Originally from southern Mexico (particularly Chiapas and Veracruz), Central America, and northern South America, the papaya is now cultivated in most tropical countries. In cultivation, it grows rapidly, fruiting within 3 years. It is, however, highly frost-sensitive, limiting its production to tropical climates.
L. deliciosus), or fir (e.g. L. deterrimus). For most tropical species, host plant range is poorly known, but species in tropical Africa seem to be rather generalist. Lactarius species are considered late-stage colonizers, that means, they are generally not present in early-colonizing vegetation, but establish in later phases of succession.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. This season had an above average number of storms. However, it had a below-average number of hurricanes and major hurricanes. There were also two tropical depressions that did not reach storm strength.
On September 3, the next hurricane developed, though it did not affect land in its duration. The third hurricane struck Georgia, accompanied by damaging waves in north Florida. The final storm was last noted on October 17\. These dates fall within the period with the most tropical cyclone activity in the Atlantic.
The flattest and most tropical Laotian area is the floodplain which stretches between the provinces of Sainyabuli and Champasak. There are many mountain peaks with more than 1.000 meters elevation. Other features include the Pak Kimin ridge near the Nam Heung stream. Sainyabuli Province is home approximately 75% of the nation's 560 domesticated elephants.
Geophila is a genus of herbs in the family Rubiaceae. This genus is pantropical, as it is found in most tropical regions. The name Geophila was once applied to a genus of mushrooms (defined by Lucien Quélet in 1886 with the modern Stropharia inuncta as type species), but this usage is now obsolete and illegitimate.
The 1953 Pacific hurricane season was the least active season on record. The season officially began on May 15 in the northeast Pacific Ocean and on June 1 in the central northern Pacific. They ended on November 30. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean.
The season officially began on May 15 for the Eastern Pacific, and June 1 for the Central Pacific. It ended on November 30 for both regions. These dates delimit the time when most tropical cyclones form in this part of the Pacific Ocean. The first system formed on May 24 and the final depression dissipated on November 16.
The 1960 Atlantic hurricane season was the least active season since 1952. The season officially began on June 15, and lasted until November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, an unnamed storm, developed in the Bay of Campeche on June 22\.
The 1940 Atlantic hurricane season was a generally average period of tropical cyclogenesis in 1940. Though the season had no official bounds, most tropical cyclone activity occurred during August and September. Throughout the year, fourteen tropical cyclones formed, of which nine reached tropical storm intensity; six were hurricanes. None of the hurricanes reached major hurricane intensity.
The 1981 Atlantic hurricane season was a fairly active season that featured 22 tropical depressions and 12 storms. The season officially began on June 1, 1981, and lasted until November 30, 1981. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. Almost all of the named storms made landfall.
The North Pacific albatrosses are large seabirds from the genus Phoebastria in the albatross family. They are the most tropical of the albatrosses, with two species (the Laysan and black-footed albatrosses) nesting in the Northwestern Hawaiian Islands, one on sub-tropical islands south of Japan (the short-tailed albatross), and one nesting on the equator (the waved albatross).
Hurricane Nora was the strongest November storm at that time. The season officially started on May 15, 1991, in the eastern Pacific, and on June 1, 1991, in the central Pacific. It lasted until November 30, 1991, in both basins. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
This makes it an ideal fish for keeping in an unheated aquarium in cold climates. In fact, White Clouds are more active and healthier when kept at temperatures lower than those at which most tropical tanks are kept. Water hardness (dH) should be from 5 to 19, and pH levels should range between 6.0 and 8.0.
Hurricane Frances over Florida in 2004 June through November is hurricane season in the Atlantic Basin and Caribbean Sea, with the most tropical activity occurring between mid-August to mid- October.National Weather Service Office in Tampa Bay, Florida (2009). Tampa Bay Area Tropical Weather Page. National Weather Service Southern Region Headquarters. Retrieved on 2009-02-06.
Also, all of the 14 named storms developed west of 150°E. The season ran throughout 2010, though most tropical cyclones tend to develop between May and October. The season's first named storm, Omais, developed on March 24 while the season's last named storm, Chaba dissipated or became extratropical on October 30. During the season only three storms were notable.
This article encompasses the 1840–1849 Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
A Blue Hawaii is typically served on the rocks. As with most tropical drinks, there are many variations in preparation, presentation, and ingredients. Hence, it is often blended with ice, margarita-like, to be served as a frozen cocktail. Many variations of glassware are used, the more whimsical the better: tiki mugs, cocktail glasses, parfait glasses, or carved out coconuts or pineapples.
The 1954 Pacific hurricane season featured below-average activity, with eleven tropical storms identified. The season officially started on May 15 and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. The majority of the year's storm remained offshore and caused little to no adverse impact on land.
New World Blackbirds Princeton, New Jersey: Princeton University Press The greater coverts and primaries are thinly fringed with white. The wing linings are yellow and the outer tail feathers have small white tips. The bill and eyes are dark black, and the legs are blue-grey. Like most tropical oriole species, the females are similar or identical to the males in coloring.
The 1936 Atlantic hurricane season officially began on June 1, 1936, and lasted until November 30, 1936. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The 1936 season was fairly active, with 20 tropical cyclones including 3 tropical depressions. Seven storms became hurricanes, of which one became a major hurricane.
The 1941 Atlantic hurricane season was the period during 1941 in which tropical cyclones formed in the Atlantic Basin. It was a relatively inactive hurricane season, with only six known storms. It officially began on June 16, 1941, and lasted until November 1, 1941. These dates delimit the period of each year when most tropical cyclones tend to form in the Atlantic basin.
The 2019 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. It was the fourth consecutive above-normal Atlantic hurricane season. The season officially began on June 1, 2019 and ended on November 30, 2019. These dates, adopted by convention, historically describe the period in each year when most tropical systems form.
The natural range of rubber ranges from Nepal in the north to Indonesia, Bhutan, northeastern India, Burma and China (Yunnan) and Malaysia. It has been widely introduced in most tropical regions of the world, including Hawaii and the West Indies. Finally, in Europe, it can be found in the sheltered gardens of the Côte d'Azur and on the Spanish and Italian coast.
Retrieved 2007-01-05. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes.
Pueraria phaseoloides is a plant species in the pea family (Fabaceae) and its subfamily Faboideae. It is a forage crop and cover crop used in the tropics. It is known as puero in Australia and tropical kudzu in most tropical regions. It is closely related to other species in the genus Pueraria and it is crossable with the other species of Pueraria.
The 1997 Pacific typhoon season was a record-breaking season featuring 11 tropical cyclones reaching super typhoon intensity, tying the record with 1965 with the most violent tropical cyclones globally. It has no official bounds; it ran year-round in 1997, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.Gary Padgett. May 2003 Tropical Cyclone Summary.
The season officially began on June 1, 1973, and lasted until November 30, 1973. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the first system formed on April 18, more than a month before the official start. Three more depressions formed before June 1; however, none attained storm intensity.
Celaenorrhinus is a genus of skipper butterflies which are commonly termed sprites. An alternate name is flats, for their habit of holding their wings flat when resting, but this is also used for related genera. They belong to the spread-winged skipper subfamily (Pyrginae), and therein are the type genus of tribe Celaenorrhini. Celaenorrhinus species are found in most tropical regions.
The 1964 Atlantic hurricane season featured the highest number of U.S.-landfalling hurricanes since 1933. The season officially began on June 15, and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The season was above average, with thirteen named storms, seven hurricanes, and five major hurricanes.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The season slightly exceeded these bounds when tropical storm One-E formed on May 13. Few storms formed this season, but it was very eventful. Twelve tropical cyclones formed during this season, of which five made landfall and two other impacted land areas.
The genus Exochaenium (22 species) is endemic to sub-Saharan Africa, with species occurring in most tropical and sub-tropical regions of the continent, particularly on the Katanga plateau (Angola, Democratic Republic of Congo and Zambia), with many extending to the Sudano-Zambesian and Guineo-Congolian regions. The genus is monophyletic and is used to study the variation and evolution of herkogamy.
The 1955 Pacific hurricane seasons began on May 15, 1955, in the northeast Pacific Ocean and on June 1, 1955, in the central Pacific. They ended on November 30, 1955. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean. Before the satellite age started in the 1960s, data on east Pacific hurricanes is extremely unreliable.
Euops is a genus of the leaf-rolling weevils (family Attelabidae) containing more than 300 species. It is spread over most tropical and subtropical regions but is missing from America. The centre of its radiation is New Guinea and Australia where it is the only representative of the subfamily Attelabinae. Females of Euops have mycangia in the space between metathorax and abdomen.
The 2006 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this basin is north of the Equator and west of the Malay Peninsula. The IMD and JTWC monitor this basin.
These dates fall within the period with the most tropical cyclone activity in the Atlantic. At two points during the season, pairs of tropical cyclones existed simultaneously. Four of the cyclones only have a single known point in their tracks due to a sparsity of data, so storm summaries for those systems are unavailable. Of the season's eight tropical cyclones, four reached hurricane status.
The 1990 Atlantic hurricane season was the most active Atlantic hurricane season since 1969, with a total of 14 named storms. The season also featured eight hurricanes, one of which intensified into a major hurricane. It officially began on June 1, 1990, and lasted until November 30, 1990. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
This species can be found throughout the tropical and sub-tropical waters of the Pacific Ocean and Indian Oceans. Warm currents such as the Agulhas Current in the western Indian Ocean have a major influence on their seasonal distribution. It is common in equatorial waters, but it is not usually seen close to islands and coral reef. It is considered the most tropical billfish species.
The 1900s Pacific hurricane seasons all began on May 15, 1900, in the northeast Pacific Ocean and on June 1, 1900, in the central Pacific. They ended on November 30, of each year. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean. Before the satellite age started in the 1960s, data on east Pacific hurricanes is extremely unreliable.
In plants such as peanuts, potatoes, and some grasses, the pest has been reported to attack the root systems. Adult male This pest occurs in most tropical areas of the world, including Asia, the Middle East, Africa, Australia, and Oceania. The hibiscus mealybug arrived in Egypt from India in 1912 and in Hawaii in 1984. Finally, it appeared in Grenada, Trinidad, and St. Kitts in the 1990s.
These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin and are adopted by convention. However, tropical cyclogenesis is possible at other times of the year, as demonstrated by the formation of Subtropical Storm Andrea on May 20, marking the record fifth consecutive year where a tropical or subtropical cyclone developed before the official start of the season.
Like most tropical climates, Key West has a two-season wet and dry climate. The period from November through April is normally sunny and quite dry, with only 25 percent of the annual rainfall occurring. May through October is normally the wet season. During the wet season some rain falls on most days, often as brief, but heavy tropical downpours, followed by intense sun.
First Federal Science Congress, Proceedings, 1960, Salisbury, Southern Rhodesia, v. 1, pp. 271–276. In this tropical soil scheme the M horizon is the main biomantle and the SL horizon constitutes its base. Stonelayers occupy the base of biomantles in many, if not most, tropical soils and in many midlatitude soils. Where present they often function as subsurface “French drains” for soil-water movements and storage.
The 1942 Atlantic hurricane season was one of seven seasons to feature multiple hurricane landfalls in Texas. The season officially lasted from June 16, 1942, to October 31, 1942. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. A total of 11 tropical storms from 1943 are listed in the Atlantic hurricane database, with two additional tropical depressions.
The final storm, Hurricane Five, was last observed on September 17. These dates fall within the period with the most tropical cyclone activity in the Atlantic. At one point during the season, two tropical cyclones existed simultaneously. Two of the cyclones only have a single known point in their tracks due to a sparsity of data, so storm summaries for those systems are unavailable.
The 2012 Pacific typhoon season was a slightly below average but destructive season, though rather active since 2004. It produced 25 named storms, fourteen typhoons, and four intense typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2012, though most tropical cyclones typically develop between May and October.
These dates, adopted by convention, historically describe the period in each year when most tropical systems form. Although two tropical depressions formed in June, the first named storm, Alberto, did not arise until August 4\. The season's final storm, an unnamed subtropical storm, became extratropical on October 29\. The 2000 season produced 15 cyclones of at least tropical (14) or subtropical (1) storm strength.
The 1966 Atlantic hurricane season featured the tropical cyclone with the longest track in the Atlantic basin – Hurricane Faith. Also during the year, the Miami, Florida Weather Office was re-designated the National Hurricane Center. The season officially began on June 1, and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
Retrieved 2006-08-26. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1990 Pacific hurricane season.
Retrieved on 2006-08-26. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the Date Line and north of the equator are called hurricanes; see 1997 Pacific hurricane season.
The most tropical songs are crafted using elements from Caribbean music genres such as reggae, dancehall, soca music and ska in its beats and instrumentation. Rolling Stones writer Christopher R. Weingarten said the beats of the record are "mostly booming or bouncy" and the "swagger is all over the place". The album has 15 tracks; its standard edition has 10 tracks while the deluxe edition has 12.
The 1903 Atlantic hurricane season featured seven hurricanes, the most in a season since 1893. The first tropical cyclone was initially observed in the western Atlantic Ocean near Puerto Rico on July 21\. The tenth and final system transitioned into an extratropical cyclone well northwest of the Azores on November 25\. These dates fall within the period with the most tropical cyclone activity in the Atlantic.
The 1975 Atlantic hurricane season featured the first tropical storm to be upgraded to a hurricane based solely on satellite imagery - Hurricane Doris. The season officially began on June 1 and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The season was near average, with nine tropical storms forming, of which six became hurricanes.
The 1965 Pacific hurricane season officially started May 15, 1965, in the eastern Pacific, and June 1, 1965, in the central Pacific, and lasted until November 30, 1965. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean. A total of ten systems were observed. The most notable storm was Tropical Storm Hazel, which killed six people in Mexico.
The 1946 Atlantic hurricane season resulted in no fatalities in the United States. The season officially began on June 15, 1946, and lasted until November 15, 1946. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the first storm, developed in the Gulf of Mexico on June 13, while the final system dissipated just offshore Florida on November 3\.
The 1969 Pacific hurricane season was an event in meteorology. It officially started on May 15, 1969, in the eastern Pacific and lasted until November 30, 1969. However, the first named storm, Ava, did not form until July 1, the latest date that the first named storm of a season formed. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
The 1977 Atlantic hurricane season had the fewest tropical storms since the 1965 season. The season officially began on June 1, and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first tropical depression of the season developed on June 13, 12 days after the start of the season, in the western Caribbean Sea.
The 1979 Atlantic hurricane season was the first season to include both male and female names, as well as the common six-year rotating lists of tropical cyclone names. The season officially began on June 1, and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was slightly below average, with nine systems reaching tropical storm intensity.
The 1886 Atlantic hurricane season ran through the early summer and the first half of fall in 1886. This is the period of each year when most tropical cyclones form in the Atlantic basin. It was a very active year, with ten hurricanes, seven of which struck the United States, an event that would not occur again until 99 years later. Four hurricanes became major hurricanes (Category 3+).
The 1858 Atlantic hurricane season was one of only three Atlantic hurricane seasons on record in which every tropical cyclone intensified into a hurricane (the others were in 1852 and 1884). The first hurricane was first observed over the northwestern Caribbean Sea on June 12\. The sixth and final storm was last noted on October 26\. These dates fall within the period with the most tropical cyclone activity in the Atlantic.
These dates, adopted by convention, historically describe the period in each year when most tropical systems form. This season's first storm, Tropical Storm Arlene, formed on June 11, while the last, Hurricane Lenny, dissipated on November 23\. Altogether, 12 tropical storms formed during the season, including eight hurricanes of which five intensified into major hurricanes. There were also four tropical depressions that did not reach tropical storm strength.
These dates, adopted by convention, historically delimit the period in each year when most tropical systems form. The season's first storm, Tropical Storm Andrea formed on June 5, and its final storm, an unnamed subtropical storm, dissipated on December 7\. Altogether, there were 13 named tropical storms during the season. Two of which attained hurricane strength, but neither intensified into a major hurricane, the first such occurrence since the 1994 season.
The 1957 Pacific hurricane season was a moderately active year in which 13 tropical cyclones formed. The hurricane season ran through the summer and fall months which conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone developed on July 15. The final storm dissipated on December 6, becoming one of the few Pacific storms to exist outside of the seasonal dates.
The 1965 Atlantic hurricane season was the first to use the modern-day bounds for an Atlantic hurricane season, which are June 1 to November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was a slightly below average season, with 10 tropical cyclones developing and reaching tropical storm intensity. Four of the storms strengthened into hurricanes.
The years between 1950 and 1959 featured the 1950s North Indian Ocean cyclone seasons. Each season was an ongoing event in the annual cycle of tropical cyclone formation. The North Indian tropical cyclone season has no bounds, but they tend to form between April and December, peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 1963 Atlantic hurricane season featured one of the deadliest tropical cyclones on record in the Atlantic basin: Hurricane Flora. The season officially began on June 15, and lasted until November 15\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was a near-average season in terms of tropical storms, with a total of nine named storms.
Coral reefs form complex marine ecosystems with tremendous biodiversity. Reefs comprise some of the densest and most diverse habitats in the world. The best- known types of reefs are tropical coral reefs which exist in most tropical waters; however, reefs can also exist in cold water. Reefs are built up by corals and other calcium-depositing animals, usually on top of a rocky outcrop on the ocean floor.
The 1924 Atlantic hurricane season featured the earliest known Category 5 hurricane - a tropical cyclone with maximum sustained winds exceeding 155 mph (250 km/h). The first system, Tropical Storm One, was first detected in the northwestern Caribbean Sea on June 18\. The final system, an unnumbered tropical depression, dissipated on November 24\. These dates fall within the period with the most tropical cyclone activity in the Atlantic.
Most tropical specimens were preserved as dried heads and feet. One dodo was reportedly sent as far as Nagasaki, Japan in 1647, but it was long unknown whether it arrived. Contemporary documents first published in 2014 proved the story, and showed that it had arrived alive. It was meant as a gift, and, despite its rarity, was considered of equal value to a white deer and a bezoar stone.
The years before 1890 featured the pre-1890 North Indian Ocean cyclone seasons. Each season was an ongoing event in the annual cycle of tropical cyclone formation. The North Indian tropical cyclone season has no bounds, but they tend to form between April and December, peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Retrieved 2006-08-26. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms forming in the Western Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA.
The 1905 Atlantic hurricane season featured five known tropical cyclones, two of which made landfall in the United States. The first system was initially observed near the Windward Islands on September 6\. The last system to dissipate, the fourth storm, transitioned into an extratropical cyclone on October 11, while located well southeast of Newfoundland. These dates fall within the period with the most tropical cyclone activity in the Atlantic.
The 1974 Atlantic hurricane season featured Hurricane Fifi, the deadliest Atlantic tropical cyclone since the 1900 Galveston hurricane. The season officially began on June 1 and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, a tropical depression, developed over the Bay of Campeche on June 22 and dissipated by June 26\.
The years between 1940 and 1949 featured the 1940s North Indian Ocean cyclone seasons. Each season was an ongoing event in the annual cycle of tropical cyclone formation. The North Indian tropical cyclone season has no bounds, but they tend to form between April and December, peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Most tropical cyclone prediction models indicated a northwesterly track that never happened, and also over-intensified the system. In addition, advisories on Tropical Depression Genevieve were discontinued on October 3, and only resumed three days later. Later analysis determined that Genevieve had been a tropical depression for this whole time. Tropical Storm Genevieve never came near land, and consequently no watches or warnings were required for any location.
Hurricane Henriette brushed the Baja California Peninsula in early September. The season officially started on May 15, 1995, in the Eastern Pacific, and on June 1, 1995, in the Central Pacific, and lasted until November 30, 1995. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The season saw eleven tropical cyclones form, of which ten became tropical storms.
The 1968 Pacific hurricane season ties the record for having the most active August in terms of tropical storms. It officially started on May 15, 1968, in the eastern Pacific and June 1 in the central Pacific and lasted until November 30, 1968. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. Several notable systems formed during the season.
Opisthoproctus soleatus is a species of fish in the family Opisthoproctidae. It was first described in 1888 by Léon Vaillant. The species lives in most tropical seas, but is more common in the eastern Atlantic, from western Ireland to Mauritania and from Sierra Leone to Angola, and also in the South China Sea. O. soleatus can grow to a standard length of and usually live from about deep.
The 1979 Pacific hurricane season was an inactive Pacific hurricane season. It officially started on May 15, 1979, in the eastern Pacific, and June 1, 1979, in the central Pacific, and lasted until November 30, 1979. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean. With ten storms, less than two-thirds of the average of seventeen, this season was very inactive.
The summit was formerly surrounded by glaciers, including the two largest out of the four glaciers remaining in the country (the other two smaller glaciers were on Pico Bolívar). The glaciers on Humboldt Peak (as most tropical glaciers) have been receding fast since the 1970s. By 2009, all but one glacier, the Humboldt Glacier, had vanished. The remaining glacier covers an area of 0.1 km2 and is forecast to melt completely within a decade.
In forests where rattan grows, its economic value can help protect forest land, by providing an alternative to loggers who forgo timber logging and harvest rattan canes instead. Rattan is much easier to harvest, requires simpler tools and is much easier to transport. It also grows much faster than most tropical wood. This makes it a potential tool in forest maintenance, since it provides a profitable crop that depends on rather than replaces trees.
Papyrus growing wild on the banks of the Nile in Uganda Papyrus can be found in tropical rain forests, tolerating annual temperatures of and a soil pH of 6.0 to 8.5. It flowers in late summer, and prefers full sun to partly shady conditions. Like most tropical plants, it is sensitive to frost. In the United States, it has become invasive in Florida and has escaped from cultivation in Louisiana, California, and Hawaii.
The 2019 Pacific hurricane season was a near average season which produced nineteen named storms, though most were rather weak and short-lived. Only seven hurricanes formed, the fewest since 2010. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin.
The 1984 Atlantic hurricane season was the busiest since 1971, though the season was below average in hurricanes and major hurricanes. It officially began on June 1, 1984, and lasted until November 30, 1984. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The 1984 season was an active one in terms of named storms, but most of them were weak and stayed at sea.
Although most tropical cyclones that become extratropical quickly dissipate or are absorbed by another weather system, they can still retain winds of hurricane or gale force. In 1954, Hurricane Hazel became extratropical over North Carolina as a strong Category 3 storm. The Columbus Day Storm of 1962, which evolved from the remains of Typhoon Freda, caused heavy damage in Oregon and Washington, with widespread damage equivalent to at least a Category 3\.
These dates conventionally delimit the period of each year when most tropical cyclones form in the eastern Pacific basin. However, the formation of a storm is possible at any time. The second storm of the season, Hurricane Barbara, brought widespread heavy rains to much of Southwestern Mexico and Central America. Damage estimates from the storm range from $50 to $356 million (2013 USD); four people were killed and four others are reportedly missing.
A scientific study which examined genetic and morphological variation in magnificent frigatebirds found both expected and also highly unexpected results. As predicted by the flight capacity of the species, the authors found signatures of high gene flow across most of the distribution range. This included evidence of recent gene flow among Pacific and Atlantic localities, likely across the Isthmus of Panama. This geological formation is a strong barrier to movement in most tropical seabirds.
Similar to tropical cyclones, extratropical cyclones cause an offshore rise of water. However, unlike most tropical cyclone storm surges, extratropical cyclones can cause higher water levels across a large area for longer periods of time, depending on the system. In North America, extratropical storm surges may occur on the Pacific and Alaska coasts, and north of 31°N on the Atlantic Coast. Coasts with sea ice may experience an "ice tsunami" causing significant damage inland.
In the east Pacific basin, the 1997 season featured two Category 5 hurricanes, Guillermo and Linda, the latter of which was the strongest on record before Patricia took that title during the 2015 season. The North Pacific basin broke the record for having the most tropical cyclones reaching Category 4 and 5 intensities with 17 that season. However, the 2015 season surpassed it with 21 tropical cyclones during the 2014–16 El Niño event.
These dates, adopted by convention, historically describe the period in each year when most tropical systems form. The season's first system, Hurricane Allison, developed on June 3; its last, Hurricane Tanya, became extratropical on November 2\. The season produced 21 tropical cyclones, of which 19 intensified into tropical storms, 11 of which became hurricanes, and five became major hurricanes. The four most notable storms during the season were hurricanes Luis, Marilyn, Opal and Roxanne.
D. reflexa var. angustifolia has the ability to grow in a mixture of both shade and sun, both inside and outside the home. If planted outside, it needs to be located in U.S. Department of Agriculture hardiness zones 10b and above because of the fact that most tropical plants cannot survive frost or winter. Additionally, it would prefer to have some shelter during the hot afternoon sun if planted outside in direct sunlight.
The 2019 Pacific typhoon season was the costliest Pacific typhoon season on record, just ahead of the previous year. The season was fairly above-average, producing 29 named storms, 17 typhoons, and five super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2019, though most tropical cyclones typically develop between May and October.
The 2009 Pacific hurricane season was the most active Pacific hurricane season since 1994. The season officially started on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.
The 1970 Atlantic hurricane season was the first season of the most recent low-activity era (“cold phase”) of tropical cyclone formation in the Atlantic. It was also the first year in which reconnaissance aircraft flew into all four quadrants of a tropical cyclone. The season officially began on June 1 and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
The 1990 Pacific hurricane season was a very active season which observed 21 named storms within the basin. The season also produced the fourth highest ACE index value on record. The season was officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
A well-organized ITCZ disturbance with deep convection organized further over the northeastern Pacific Ocean on July 28. It developed into a tropical depression later that day, while southwest of the southern tip of Baja California. The position of Fabio's formation was much further south and west than where most tropical cyclones form during the same time period. The depression moved westward while gradually strengthening and it developed into Tropical Storm Fabio on July 29.
The 2006 Pacific typhoon season was a below-average season that produced a total of 23 named storms, 15 typhoons, and six super typhoons. The season ran throughout 2006, though most tropical cyclones typically develop between May and October. The season's first named storm, Chanchu, developed on May 9, while the season's last named storm, Trami, dissipated on December 20. Also, this season was more active, costly, and deadly than the previous season.
Hurricane Andrew approaching South Florida in August 1992. In the period between 1975 and 1999, 83 tropical or subtropical cyclones affected the state, which collectively resulted in $51.1 billion (2017 dollars) in damage, primarily from Hurricane Andrew, and 54 direct casualties. The 1985 season was the year with the most tropical cyclones affecting the state, with a total of eight systems. Every year included at least one tropical cyclone affecting the state.
The Hispaniolan oriole is a slender-billed black and yellow oriole that lacks white markings on the wings. It shows more yellow than most Caribbean orioles, except for the Bahama oriole (Icterus northropi). The adult males and females are black overall, with distinctive yellow patches on shoulders, rump, and under-tail coverts extending to the lower breast. Like most tropical oriole species, the females are similar or identical to the males in coloring.
The 1999 Atlantic hurricane season had five Category 4 hurricanes - the highest number recorded in a single season in the Atlantic basin, later tied in 2005. The season officially began on June 1, and ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was a fairly active season, mostly due to a persistent La Niña that developed in the latter half of 1998.
The 2014 Atlantic hurricane season was a below-average season in terms of named storms, and an average season in terms of both hurricanes and major hurricanes. It produced nine tropical cyclones, eight named storms, the fewest since the 1997 Atlantic hurricane season, six hurricanes and two major hurricanes. It officially began on June 1, 2014, and ended on November 30, 2014. These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin.
Tropical rainforests have existed on earth for hundreds of millions of years. Most tropical rainforests today are on fragments of the Mesozoic era supercontinent of Gondwana. The separation of the landmass resulted in a great loss of amphibian diversity while at the same time the drier climate spurred the diversification of reptiles. The division left tropical rainforests located in five major regions of the world: tropical America, Africa, Southeast Asia, Madagascar, and New Guinea, with smaller outliers in Australia.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA.
Lophelia pertusa is a reef building, deep water coral, but it does not contain zooxanthellae, the symbiotic algae which lives inside most tropical reef building corals. Lophelia lives between and over depth, but most commonly at depths of , where there is no sunlight, and a temperature range from about . As a coral, it represents a colonial organism, which consists of many individuals. New polyps live and build upon the calcium carbonate skeletal remains of previous generations.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the formation of Tropical Storm Arthur caused the season to start one day early. It was the only year on record in which a major hurricane existed in every month from July through November in the North Atlantic. Bertha became the longest-lived July tropical cyclone on record for the basin, the first of several long-lived systems during 2008.
The 1976 Atlantic hurricane season featured only one fully tropical storm throughout both the Caribbean Sea and the Gulf of Mexico, a rare occurrence. The season officially began on June 1 and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the first system, a subtropical storm, developed in the Gulf of Mexico on May 21, several days before the official start of the season.
The 1947 Atlantic hurricane season was the first Atlantic hurricane season to have tropical storms labeled by the United States Air Force. The season officially began on June 16, 1947, and ended on November 1, 1947. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the first tropical cyclone developed on June 13, while the final system was absorbed by a cold front on December 1\.
Red- footed booby Egg, Collection Museum Wiesbaden This species breeds on islands in most tropical oceans. When not breeding it spends most of the time at sea, and is therefore rarely seen away from breeding colonies. It nests in large colonies, laying one chalky blue egg in a stick nest, which is incubated by both adults for 44–46 days. The nest is usually placed in a tree or bush, but rarely it may nest on the ground.
The 1980 Atlantic hurricane season was tied with 1932, 1969, and 1994 for having the most named storms form in the Atlantic Ocean during the month of November – only to be surpassed in 2001 and 2005. The season officially began on June 1, 1980, and lasted until November 30, 1980. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic Ocean. The season was fairly active, with fifteen tropical cyclones forming.
Many lemurs that eat leaves tend to do so during times of fruit scarcity, sometimes suffering weight loss as a result. Most lemur species, including most of the smallest lemurs and excluding some of the indriids, predominantly eat fruit (frugivory) when available. Collectively, lemurs have been documented consuming fruit from at least 86 native plant families and 15 alien plant families. As with most tropical fruit eaters, the lemur diet is dominated by fruit from Ficus (fig) species.
The 2010 Pacific hurricane season is the least active Pacific hurricane season, along with 1977, since reliable records began in 1971, the season produced eight named storms. Only three hurricanes formed and two major hurricanes. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin.
The 1983 Pacific hurricane season was the longest season ever recorded at that time, which was later surpassed by the 2015 and 2016 seasons. It was a very active Pacific hurricane season. The season started on May 15, 1983 in the eastern Pacific, and on June 1, 1983 in the central Pacific, and lasted until November 30, 1983. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
The 2018 Pacific typhoon season was at the time, the costliest Pacific typhoon season on record, until the record was beaten by the following year. The season was above-average, producing 29 storms, 13 typhoons, and 7 super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2018, though most tropical cyclones typically develop between May and October.
The 2016 Pacific typhoon season is considered to have been the fourth-latest start for a Pacific typhoon season since reliable records began. It was an average season, with a total of 26 named storms, 13 typhoons, and six super typhoons. The season ran throughout 2016, though typically most tropical cyclones develop between May and October. The season's first named storm, Nepartak, developed on July 3, while the season's last named storm, Nock-ten, dissipated on December 28.
The 2015 Pacific typhoon season was a slightly above average season that produced 27 tropical storms, 18 typhoons, and nine super typhoons. The season ran throughout 2015, though most tropical cyclones typically develop between May and November. The season's first named storm, Mekkhala, developed on January 15, while the season's last named storm, Melor, dissipated on December 17. The season saw at least one named tropical system forming in each of every month, the first time since 1965.
In geophysical fluid dynamics, the f-plane approximation is an approximation where the Coriolis parameter, denoted f, is set to a constant value. This approximation is frequently used for the analysis of highly idealized tropical cyclones. Using a constant Coriolis parameter prevents the formation of beta gyres which are largely responsible for the North-westward direction of most tropical cyclones. Rossby waves also depend on variations in f, and do not occur in the f-plane approximation.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1972 Atlantic hurricane season was a significantly below average season, having only four fully tropical named storms – the fewest since 1930. It officially began on June 1, 1972, and lasted until November 30, 1972. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, Subtropical Storm Alpha, developed on May 23 off the Southeast United States and struck Florida, causing minor damage and two fatalities.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
Furthermore, there were total of two major hurricanes, Category 3 or greater on the Saffir–Simpson hurricane wind scale. It officially started on May 15 in the Eastern Pacific, and on June 1 in the Central Pacific; they both ended on November 30, 2000. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.
The 1989 Pacific hurricane season officially started on May 15, 1989, in the eastern Pacific, and June 1, 1989, in the central Pacific, and lasted until November 30, 1989. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. A total of 17 storms and 9 hurricanes formed, which was near long-term averages. Four hurricanes reached major hurricane status (Category 3 or higher) on the Saffir-Simpson Hurricane Scale.
Parrots, also known as psittacines (), are the 402 species of birds that make up the order Psittaciformes, found in most tropical and subtropical regions, of which 387 are extant. The order is subdivided into three superfamilies: the Psittacoidea ("true" parrots), the Cacatuoidea (cockatoos), and the Strigopoidea (New Zealand parrots). Parrots have a generally pantropical distribution with several species inhabiting temperate regions in the Southern Hemisphere as well. The greatest diversity of parrots is in South America and Australasia.
On average, 10.1 named storms occur each season, with an average of 5.9 becoming hurricanes and 2.5 becoming major hurricanes (Category 3 or greater). The most active season was 2005, during which 28 tropical cyclones formed, of which a record 15 became hurricanes. The least active season was 1914, with only one known tropical cyclone developing during that year. The Atlantic hurricane season is a time when most tropical cyclones are expected to develop across the northern Atlantic Ocean.
The 2000 Pacific typhoon season marked the first year using names contributed by the World Meteorological Organization. It was a rather below-average season, producing a total of 23 tropical storms, 13 typhoons and 4 intense typhoons. The season ran throughout 2000, though typically most tropical cyclones develop between May and October. The season's first named storm, Damrey, developed on May 7, while the season's last named storm, Soulik, dissipated on January 4 of the next year.
The 1997 Atlantic hurricane season was a below-average season and is the most recent season to feature no tropical cyclones in August - typically one of the most active months. The season officially began on June 1, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The 1997 season was inactive, with only seven named storms forming, with an additional tropical depression and an unnumbered subtropical storm.
The 1964 Pacific hurricane season was the least active Pacific hurricane season on record since 1953. The season officially started on May 15 in the eastern Pacific and June 1 in the Central Pacific Hurricane Center's area of responsibility and lasted until November 30 in both regions. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. During this season only six tropical storms developed, of which two intensified into hurricanes.
The Pacific Ocean lies to the west of California. Sea temperatures in most of the state rarely exceed 70 °F (21 °C), even in summer, because of up- welling deep waters with dissolved nutrients. Therefore, most sea life in and around California resembles both Arctic and tropical, biotopes, leaning more towards the latter in the south coast and vice versa. The sea off California is remarkably fertile, a murky green filled with fish, rather than the clear dead blue of most tropical seas.
Soil types are highly variable in the tropics and are the result of a combination of several variables such as climate, vegetation, topographic position, parent material, and soil age. Most tropical soils are characterized by significant leaching and poor nutrients, however there are some areas that contain fertile soils. Soils throughout the tropical rainforests fall into two classifications which include the ultisols and oxisols. Ultisols are known as well weathered, acidic red clay soils, deficient in major nutrients such as calcium and potassium.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1996 Pacific hurricane season. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center.
Some species join mixed feeding flocks now and then; others defend the blooming and fruiting trees and bushes where they forage. Unlike most tropical Asian passerines, the nests of leafbirds are not located low down in the forest, but are instead found on the ends of branches near the tree crown. As such the nests of many species have rarely, if ever, been seen. The nests are open cups; of the few known, they are built of fine stems, leaf parts and rootlets.
In most tropical areas the local dispensaries sell prickly heat powder, a talc admixture containing drying milk proteins (Labilin) and Triclosan to fight the infection. These include cooling menthol to help alleviate difficulty getting to sleep. This is an effective treatment—the powder stays on the skin longer and treats bacteria dispersed into bed linens, providing a reasonably dry refuge area for healing. Miliaria often covers large areas, and generous use of Cortisone may be contraindicated for reasons stated on package warnings.
The Highlands are at particular risk of deforestation and associated soil erosion. Furthermore, the region, lying south of the Sahel are at particular risk of desertification and frequent drought. The Highlands experience, as most tropical regions, two seasons; the rainy season (kremti) is from June-September while the dry season is from September to June. The average temperature for Asmara, which is above sea level is approximately 16°C, but other places range from about 10°C to 25°C.
The 1885 Atlantic hurricane season ran through the summer and the first half of fall in 1885. This is the period of each year when most tropical cyclones form in the Atlantic basin. In 1885 there were two tropical storms and six hurricanes in the Atlantic basin. However, in the absence of modern satellite monitoring and remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher.
The 2017 Pacific hurricane season was significantly less active than the previous three Pacific hurricane seasons, featuring eighteen named storms, nine hurricanes, and four major hurricanes. Despite the considerable amount of activity, most of the storms were weak and short-lived. The season officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific; they both ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin.
The 1985 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1986 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1987 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD. Prior to 1992, this season had the most tropical storms in North Indian recorded history, with 8 storms forming.
The 2020 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation in which tropical cyclones form in the western Pacific Ocean. The season runs throughout the year, though most tropical cyclones typically develop between May and October. The season has been unusually inactive, with only 21 tropical cyclones and 16 named storms forming since May 8. Additionally, the JTWC recorded no tropical cyclone development in the month of July, the first such occurrence since reliable records began.
The 1971 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1973 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1972 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1974 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The season officially started May 15, 1976, in the eastern Pacific, and June 1, 1976, in the central Pacific, and lasted until November 30, 1976. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. In practice, the season lasted from the formation of the first storm on June 2 to the dissipation of the last on October 30. This season had a slightly below average number of tropical storms, with fourteen.
The 1975 Pacific hurricane season officially started May 15, 1975, in the eastern Pacific, and June 1, 1975, in the central Pacific, and lasted until November 30, 1975. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean. The 1975 Pacific hurricane season was slightly above average, with 17 tropical storms forming. Of these, 9 became hurricanes, and 4 became major hurricanes by reaching Category 3 or higher on the Saffir-Simpson Hurricane Scale.
The 1980 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1982 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1983 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1984 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1975 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1976 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1977 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1979 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1981 Pacific hurricane season was a slightly below average Pacific hurricane season. The season officially started on May 15 in the eastern Pacific basin and June 1 in the central Pacific basin. Both basins' seasons ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone of the season was designated on May 30, and the final storm of the season, Hurricane Otis, dissipated on October 30.
The 1985 Pacific hurricane season is the third-most active Pacific hurricane season on record. It officially started on May 15, 1985, in the eastern Pacific, and on June 1, 1985, in the central Pacific, and lasted until November 30, 1985. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. At the time, the 1985 season was the most active on record in the eastern north Pacific, with 28 tropical cyclones forming.
The 1980 Pacific hurricane season officially started May 15, 1980, in the eastern Pacific and June 1, 1980, in the central Pacific, lasting until November 30, 1980. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern and central Pacific Ocean. This season was relatively uneventful; since no tropical cyclones made landfall, there were no reports of casualties or damage. Overall, the 1980 season was slightly below the long-term average, with 16 tropical cyclones forming.
The 2005 Pacific hurricane season was a near-average season which produced fifteen named storms, only seven hurricanes formed and two major hurricanes. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.
Due to its geographical roots, tropical music generally combines elements from European and African traditions. An example of this is the process of binarization of ternary rhythms brought from Africa, which took place originally in Cuba, later spreading throughout the rest of the Caribbean and Latin America. The presence of syncopated polyrhythms of African origin make most tropical music naturally dance-oriented. Tropical music instrumentation also includes both European (tres, piano, trumpet, timbales) and African-descended (congas, bongos, marimba) instruments.
Only seven of them intensified into hurricanes, and only four of those became major hurricanes: Irene, Katia, Ophelia, and Rina. The season officially began on June 1 and ended on November 30, dates which conventionally delimit the period during each year in which most tropical cyclones develop in the Atlantic Ocean. However, the first tropical storm of the season, Arlene, did not develop until nearly a month later. The final system, Tropical Storm Sean, dissipated over the open Atlantic on November 11.
These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1991 Pacific hurricane season. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center.
The 1882 Atlantic hurricane season ran through the summer and early fall of 1882. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1882 Atlantic season there were two tropical storms, two Category 1 hurricanes, and two major hurricanes (Category 3+). However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher.
The 1998 Pacific hurricane season was a below average Pacific hurricane season. It had six major hurricanes, which was well above average. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in that region. The first tropical cyclone developed on June 11, about ten days later than the normal start of the season.
The 1880 Atlantic hurricane season ran through the summer and fall of 1880. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1880 Atlantic season there were two tropical storms, seven hurricanes, and two major hurricanes (Category 3+). However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher.
The 2011 Pacific typhoon season was a below average season that produced a total of 21 named storms, 8 typhoons, and four super typhoons. This season was much more active than the previous season, although both seasons were below the Pacific typhoon average of 26. The season ran throughout 2011, though most tropical cyclone tend to develop between May and October. The season's first named storm, Aere, developed on May 7 while the season's last named storm, Washi dissipated on December 19.
Cuban orioles are nesting songbirds and, along with some other tropical orioles, may pair with one mate for the rest of their lives. From February to July Cuban orioles build hanging nests similar to baskets out of material from palm and banana tree leaves. Clutch sizes are typically three greenish-white eggs with grey or olive spots and scrawl. Similar to most tropical orioles, Cuban oriole pairs may maintain a year-round territory and will defend their nest from predators.
The 1989 North Indian Ocean cyclone season was a below-average season in annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1988 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1981 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1998 North Indian Ocean cyclone season was an active season in annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 2006–07 South Pacific cyclone season was an event in the annual cycle of tropical cyclone formation. It began on November 1, 2006 and ended on April 30, 2007. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season, and the "tropical cyclone year" runs from July 1, 2006 to June 30, 2007.
The 2002 Atlantic hurricane season was a near-average Atlantic hurricane season. It officially started on June 1, 2002 and ended on November 30, dates which conventionally limit the period of each year when most tropical cyclones develop in the Atlantic Ocean. The season produced fourteen tropical cyclones, of which twelve developed into named storms; four became hurricanes, and two attained major hurricane status. While the season's first cyclone did not develop until July 14, activity quickly picked up: eight storms developed in the month of September.
The 1962 Pacific hurricane season was a moderately active Pacific hurricane season that included two hurricane landfalls. The 1962 Pacific hurricane season officially started on May 15, 1962 in the eastern Pacific and June 1, 1962 in the Central Pacific Hurricane Center's area of responsibility and lasted until November 30, 1962 in both regions. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The first of two hurricane landfalls, Hurricane Valerie, struck northwestern Mexico in June.
Hurricanes Ione (left) and Kirsten (right) undergoing a 200px The 1974 Pacific hurricane season featured one of the most active periods of tropical cyclones on record with five storms existing simultaneously. The season officially started May 15 in the eastern Pacific, and June 1 in the central Pacific, and lasted until November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean. With 17 named storms and 11 hurricanes, this season was slightly above average.
In the middle of February, the monsoon trough persisted over the Mozambique Channel and spawned a circulation on February 15 to the west of Juan de Nova Island. Thunderstorms increased around the circulation, and later that day, MFR began tracking the system as a tropical depression. Despite warm air temperatures, the system did not develop a warm core like most tropical cyclones as it moved to the southeast. On February 16, the storm passed about south of Juan de Nova Island, producing gusts of .
The 1883 Atlantic hurricane season ran through the summer and the first half of fall in 1883. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1883 Atlantic season there was one tropical storm, one Category 1 hurricane, and two major hurricanes (Category 3+). However, in the absence of modern satellite monitoring and remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher.
EF2 (T4-T5) tornadoes are the lower end of "significant", yet are stronger than most tropical cyclones (though tropical cyclones affect a much larger area and their winds take place for a much longer duration). Well-built structures can suffer serious damage, including roof loss, and collapse of some exterior walls may occur at poorly built structures. Mobile homes, however, are totally destroyed. Vehicles can be lifted off the ground, and lighter objects can become small missiles, causing damage outside of the tornado's main path.
The 1986 Atlantic hurricane season was a below average season that produced 10 depressions, 6 named storms, 4 hurricanes, and 0 major hurricanes. The season officially began on June 1, 1986, and lasted until November 30, 1986. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. During the 1986 season, the first subtropical depression formed in the first week of June, while the last tropical cyclone dissipated at the end of the third week of November.
The 2014 Pacific hurricane season was the fifth-busiest season since reliable records began in 1949, alongside the 2016 season. The season officially started on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they both ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. Entering the season, expectations of tropical activity were high, with most weather agencies predicting a near or above average season.
The 2011 Pacific hurricane season was a below average in terms of named storms season and hurricanes, although it had above average number of major hurricanes. During the season, 13 tropical depressions formed along with 11 tropical storms, 10 hurricanes and six major hurricanes. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30\. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin.
Separation from the sea at low tide means that water is not renewed, fish crowding within the pool means that oxygen is quickly depleted, and absence of light at night means that there is no photosynthesis to replenish the oxygen. Examples of tidepool species that perform ASR include the tidepool sculpin, Oligocottus maculosus, the three-spined stickleback, and the mummichog. But ASR is not limited to the intertidal environment. Most tropical and temperate fish species living in stagnant waters engage in ASR during hypoxia.
Track map of all storms during the season. This timeline documents all of the events of the 2009-10 South-West Indian Ocean cyclone season which is the period that tropical cyclones formed in the Indian Ocean. Within the Indian Ocean most tropical cyclones form within the cyclone season which began on November 1 and will end on April 30. The scope of this article is limited to tropical cyclones that form in the Indian Ocean 30°E and 90°E to the south of the equator.
The 1939 Atlantic hurricane season officially began on June 12, 1939, and lasted until November 7, 1939. These dates mark the period of each year when most tropical cyclones form in the Atlantic basin. The 1939 season had below normal activity, with only six tropical storms, of which two became hurricanes and one became a major hurricane, equivalent to Category 3 status or higher on the modern-day Saffir-Simpson Hurricane Scale. The first tropical cyclone formed on June 12, and the last dissipated on November 6.
The 2000–01 South Pacific cyclone season was an event in the annual cycle of tropical cyclone formation. It began on November 1, 2000 and ended on April 30, 2001. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season, and the "tropical cyclone year" runs from July 1, 2000 to June 30, 2001.
The 1956 Atlantic hurricane season featured a decent number of tropical cyclones, although most tropical storms and hurricanes affected land. There were twelve tropical storms, a third of which became hurricanes. One of the hurricanes strengthened to the equivalent of a major hurricane, which is a Category 3 or greater on the Saffir-Simpson scale. The strongest hurricane of the season was Betsy, which was also the most damaging storm of the season: it destroyed 15,000 houses and left $40 million in damage in Puerto Rico.
Tropical systems were present during 73 days, which was significantly higher than the average of 58 for this basin. Tropical cyclones in this basin are monitored by the Regional Specialized Meteorological Center (RSMC) in Réunion. The season started on November 1, 2001, and ended on April 30, 2002; for Mauritius and the Seychelles, the season continued until May 15\. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin; however, storms formed both before and after the designated season.
These dates, adopted by convention, historically describe the period in each year when most tropical systems form. Even so, there were no named storms during either the opening or closing months of the season, as the first, Hurricane Arthur, developed on July 1, and the last, Tropical Storm Hanna, dissipated on October 28\. Altogether, eight tropical storms formed during the season, including six hurricanes of which two intensified into major hurricanes. There was also one tropical depression that failed to reach tropical storm strength.
The 2005 Pacific typhoon season was the least active typhoon season since 2000, producing twenty-three named storms, thirteen becoming a typhoons, and three super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2005, though most tropical cyclones typically develop between May and October. The season's first named storm, Kulap, developed on January 13, while the season's last named storm, Bolaven, dissipated on November 20.
The 1890 Atlantic hurricane season is tied for the third least active hurricane season on record, behind 1914 and 1930. The first system was initially observed on May 27 and the last storm, Hurricane Four, dissipated over Central America on November 1\. These dates fall within the period with the most tropical cyclone activity in the Atlantic. The first storm moved slowly north-northwestward, bringing heavy rains and extensive flooding to Cuba, which caused at least three fatalities and at least $1 million (1890 USD) in damage.
The 1881 Atlantic hurricane season ran through the summer and early fall of 1881. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1881 Atlantic season there were three tropical storms and four hurricanes, none of which became major hurricanes (Category 3+). However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher.
The 1994 Pacific hurricane season was the final season of the eastern north Pacific's consecutive active hurricane seasons that unofficially started in 1982. The season officially started on May 15, 1994, in the eastern Pacific, and on June 1, 1994, in the central Pacific, and lasted until November 30, 1994. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone formed on June 18, while the last system dissipated on October 26.
The 1999 Pacific hurricane season was one of the least active Pacific hurricane seasons on record. The season officially began on May 15 in the Eastern Pacific, and on June 1 in the Central Pacific; in both basins, it ended on November 30\. These dates conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone of the season, Hurricane Adrian, developed on June 18, while the final storm of the season, Tropical Storm Irwin, dissipated on October 11\.
Eight tropical storms formed in August this year, a record for the most active August in the East Pacific, excluding Virginia. The eight named storms forming in August this year also made it the most tropical storms to ever form in a month in the East Pacific since 1966. However, this record was tied during the 2009 Pacific hurricane season. Because of a lack of Hurricane Hunter data, a majority of the intensity readings from this season were later removed from the best track file.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, tropical cyclone formation is possible at any time of the year, as illustrated when the first tropical depression formed on May 10, five days prior to the official start of the season. The second named storm of the season, Hurricane Bud, struck Baja California Sur in mid-June, causing minor damage. Tropical Storm Carlotta stalled offshore of the Mexican coastline, where it also caused minor damage.
The 2017 North Indian Ocean cyclone season was a below average season in the annual cycle of tropical cyclone formation. This season produced only three named storms, of which one only intensified into a very severe cyclonic storm. The North Indian Ocean cyclone season has no official bounds but cyclones tend to form between April and December with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Collectively, the three storms killed at least 316 people. The season started on November 1, 1999, and ended for most of the basin on April 30, 2000; for Mauritius and the Seychelles, the season continued until May 15\. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin; Despite the destructive nature of the season, it began later than usual. Cyclone Astride originated toward the end of December, bringing rainfall and gusty winds to northern Madagascar while in the region.
The canna rust fungus grows best under high relative humidity and extended periods of leaf wetness (roughly ≥20 °C). This type of environment can be caused by high soil moisture, tall weeds surrounding the Canna, and dense shading that prevents moisture from evaporating from the leaf surface. The fungus can survive in most tropical environments where the canna lily grows due to the tropics high relative moisture throughout the growing season. P. thaliae has been reported throughout Europe and extends throughout the northern hemisphere.
The 2008–09 South-West Indian Ocean cyclone season was a slightly above average event in tropical cyclone formation. It began on November 15, 2008, and officially ended on April 30, 2009, with the exception for Mauritius and the Seychelles, for which it ended on May 15, 2009. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical cyclones in this basin were monitored by the Regional Specialised Meteorological Centre in Réunion.
The 1996 Atlantic hurricane season had the most major hurricanes since 1950, which are Category 3 or higher on the Saffir-Simpson scale. The season was above-average, featuring a total of thirteen named storms, nine hurricanes, and six major hurricanes. The season officially began on June 1, 1996 and ended on November 30, 1996, dates which conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The season's first tropical cyclone, Tropical Storm Arthur, developed on June 17, while the final cyclone, Hurricane Marco dissipated on November 26\.
Taitung has a tropical monsoon climate, with a wet season from May to October, a dry season from November to April, and consistently very warm to hot temperatures with high humidity. Unlike most tropical climates, however, the dry season is foggy rather than sunny, so that moisture availability during this period is greater than the low rainfall and warm temperatures would suggest. The highest record of temperature of Taiwan was recorded in Taitung on May 9, 2004, with temperatures peaking above 40 degrees Celsius for the first time in Taiwan's recorded history.
The 2012 Atlantic hurricane season was the final year in a consecutive string of three very active seasons, although many of the storms were weak and short- lived. It is tied with 1887, 1995, 2010, and 2011 for the fourth-most active Atlantic hurricane season on record, with 19 tropical storms. It was also the third-costliest season, behind 2005 and 2017. The season officially began on June 1 and ended on November 30, dates that conventionally delimit the period during each year in which most tropical cyclones form in the Atlantic Ocean.
The 1908 Atlantic hurricane season ran from June 1 to November 30 in 1908. These dates conventionally delimit the year in which most tropical cyclones form in the Atlantic basin. However, this season got off to a very early start, with a Category 2 hurricane forming on March 6, making it the third earliest hurricane on record to form in the Atlantic Basin after Hurricane One in 1938 and Hurricane Alex in 2016. It is the only known Atlantic tropical cyclone to exist in the month of March.
The only other significant storm of the season was Hurricane Jimena, which passed just to the south of Hawaii, the first storm to directly threaten Hawaii for several years. The season officially started on May 15, 2003, in the eastern Pacific Ocean, and on June 1, 2003, in the central Pacific, and lasted until November 30, 2003. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The season saw 16 tropical storms form, of which 7 became hurricanes, which is about average.
Track map of all storms in the season. The 2011 Pacific hurricane season officially started on May 15, 2011 in the eastern Pacific, designated as the area east of 140°W, and on June 1, 2011 in the central Pacific, which is between the International Date Line and 140°W, and lasted until November 30, 2011\. These dates typically limit the period of each year when most tropical cyclones form in the eastern Pacific basin. This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation.
The 1961 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1987 Atlantic hurricane season was a below-average hurricane season that was limited by an ongoing El Niño. The season officially began on June 1, 1987, and lasted until November 30, 1987, although activity began on May 24 when a tropical depression developed east of the central Bahamas. The June through November dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first cyclone to attain tropical storm status was an unnamed tropical storm which formed on August 9, nearly a month later than usual.
The 1964 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1962 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1963 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
Most tropical cyclones form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies. When the subtropical ridge position shifts due to El Niño, so will the preferred tropical cyclone tracks. Areas west of Japan and Korea tend to experience much fewer September–November tropical cyclone impacts during El Niño and neutral years. During El Niño years, the break in the subtropical ridge tends to lie near 130°E which would favor the Japanese archipelago.
The Argentine brown bat is known to be able to reproduce year round, most tropical species of bats do not hibernate or use torpor in off seasons so the bats are able to exhibit reproductive habits through the year. It is more common for the Argentine brown bat to breed during the rainy season when there is more food available. Females can hold sperm for up to three months until fertilization occurs. Gestation takes about three months before the litter is born, usually little size is only one to two.
The 2007 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons on record. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
These dates, adopted by convention, historically describe the period in each year when most tropical systems form. However, storm formation is possible at any time of the year, as demonstrated in 1972 by the formation of Subtropical Storm Alpha on May 23\. The season's final storm, Subtropical Storm Delta, dissipated on November 7\. The season produced nineteen tropical or subtropical cyclones, of which seven intensified into tropical or subtropical storms; three became hurricanes, of which only but only one, Betty, had sustained winds greater than minimum hurricane force.
The 1988 Atlantic hurricane season was a near average season that proved costly and deadly, with 15 tropical cyclones directly affecting land. The season officially began on June 1, 1988, and lasted until November 30, 1988, although activity began on May 30 when a tropical depression developed in the Caribbean Sea. The June through November dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first cyclone to attain tropical storm status was Alberto on August 8, nearly a month later than usual.
Topographic map of North Carolina The list of North Carolina hurricanes before 1900 encompasses 139 tropical cyclones that affected the U.S. state of North Carolina. Collectively, cyclones in North Carolina during the time period resulted in over 775 direct fatalities during the period. Seven cyclones affected the state in the 1893 season, which was the year with the most tropical cyclones devastating the state during the time period. From the beginning of the official Atlantic hurricane record in 1851 to 1899, there were 12 years without a known tropical cyclone affecting the state.
New inlet created by Hurricane Isabel (USGS) The period from 1980 to the present encompasses 120 tropical or subtropical cyclones that affected the state. Collectively, cyclones in North Carolina during the time period resulted in over $10 billion in damage (2010 USD), primarily from hurricanes Fran and Floyd. Additionally, tropical cyclones in North Carolina were responsible for 77 direct fatalities and at least 44 indirect casualties during the period. Eight cyclones affected the state in the 1985 season, which was the year with the most tropical cyclones striking the state.
It also became the second consecutive season to feature at least one Category 5 hurricane, with Hurricane Matthew reaching such strength in the previous season. All ten of the season's hurricanes occurred in a row—the greatest number of consecutive hurricanes in the satellite era, and tied for the highest number of consecutive hurricanes ever observed in the Atlantic basin. The season officially began on June 1 and ended on November 30. These dates historically describe the period of year when most tropical cyclones form in the Atlantic basin and are adopted by convention.
The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
Unlike most tropical cyclones that form in the eastern Pacific Ocean, Irwin's track was very unusual. The system which originally started moving westward, turned north, then east and again back south, and east until dissipation, on October 17, as a remnant low. Also, between October 11 and 14, Irwin weakened into a tropical depression twice and again re-strengthened back to a tropical storm before finally weakening into a tropical depression on October 15. The depression turned west again and dissipated into a remnant low in the late hours of October 16.
The 1995 Atlantic hurricane season is tied with 1887, 2010, 2011, and 2012 for the fourth-most active Atlantic hurricane season on record, with 19 tropical storms. It is also considered to be the start of an ongoing era of high- activity tropical cyclone formation. The season produced twenty-one tropical cyclones, nineteen named storms, as well as eleven hurricanes and five major hurricanes. The season officially began on June 1 and ended on November 30, dates which conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin.
Tracks of hurricanes over Florida from 1900 to 1949 The list of Florida hurricanes from 1900 to 1949 encompasses 108 Atlantic tropical cyclones that affected the U.S. state of Florida. Collectively, tropical cyclones in Florida during the time period resulted in about $4 billion (2008 USD) in damage. Additionally, tropical cyclones in Florida were directly responsible for about 3,550 fatalities during the time period, most of which from the 1928 Okeechobee Hurricane. The 1947 season was the year with the most tropical cyclones affecting the state, with a total of 6 systems.
The 2009–10 South Pacific cyclone season began on December 3, 2009 with the formation of Tropical Disturbance 01F, 32 days after the cyclone season had officially begun on November 1, 2009. The season ended on April 30, 2010. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season; the "tropical cyclone year" began on July 1, 2009 and ended on June 30, 2010.
The geology of the Boura Mountains is complex. The dense mountain forest sits at an altitude of between 550–900 m above sea level, and has a mean annual rainfall of 200–280 mm. The highlands experience, as most tropical regions, two seasons; the rainy season is from mid-June to mid-September and the dry season from October to June. In addition to rainfall, the Boura Mountains receive additional precipitation in the form of fog and winter rains which sustain isolated forests of Juniperus, Buxus, Acacia, Acacia tortilis, Juniperus procera, etc.
Hybrids are routinely found in the Rio Grande Valley of southern Texas, though this may be a recent phenomenon. Most tropical parulas can be distinguished from the northern parula by their lack of white eye crescents, but this may be ambiguous in hybrids. One should also look for the distribution and extent of non-yellow coloration on the breast, and the extent of yellow below the cheek and on the belly. In addition, a partially leucistic tropical parula female was seen in 2005, at Reserva Buenaventura in El Oro Province, Ecuador.
The 1982 Atlantic hurricane season was an extremely inactive Atlantic hurricane season featuring only six tropical storms, the record-tying lowest in the satellite era until the record was surpassed one year later, when only four named storms formed. The season officially began on June 1, 1982, and lasted until November 30, 1982. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. This season produced five named storms and an unnamed subtropical storm (no subtropical storms were named between 1974 and 2001).
The 1965 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1966 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1967 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1969 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
The 1968 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India.
Track map of all storms during the season. This timeline documents all of the events of the 2009–10 South Pacific cyclone season which is the period that tropical cyclones formed in the southern Pacific Ocean. Within the Southern Pacific Ocean, most tropical cyclones form within the cyclone season which began on November 1 and will end on April 30, though occasionally cyclones form outside these times. The scope of this article is limited to tropical cyclones that form in the Indian Ocean 160°E and 120°W to the south of the equator.
The 1986 Pacific hurricane season saw several tropical cyclones contribute to significant flooding to the Central United States. The hurricane season officially started May 15, 1986, in the eastern Pacific, and June 1, 1986 in the central Pacific, and lasted until November 30, 1986 in both regions. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. A total of 17 named storms and 9 hurricanes developed during the season; this is slightly above the averages of 15 named storms and 8 hurricanes, respectively.
The 2014 Pacific typhoon season was a slightly below average season, featuring 23 tropical storms, 11 typhoons, 8 super typhoons, and 7 Category 5 typhoons. The season's peak months August and September saw minimal activity caused by an unusually strong and a persistent suppressing phase of the Madden–Julian oscillation (MJO). The season ran throughout 2014, though most tropical cyclones typically develop between May and October. The season began with the development of Tropical Storm Lingling on January 18, and ended after Tropical Storm Jangmi which dissipated on January 1 of the next year.
The 1968 Atlantic hurricane season was one of five Atlantic hurricane seasons during the satellite era not to feature a major hurricane, the others being 1972, 1986, 1994, and 2013. The season officially began on June 1 and lasted until November 30, dates which conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was a below average season in terms of tropical storms, with a total of eight nameable storms. The first system, Hurricane Abby, developed in the northwestern Caribbean Sea on June 1\.
The 2001–02 South Pacific cyclone season was a below-average year in which only five named storms formed or entered the South Pacific basin. It began on November 1, 2001 and ended on April 30, 2002. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season, and the "tropical cyclone year" runs from July 1, 2001 to June 30, 2002.
The 2015 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
In terms of their habitat, N. nepalensis are found in different elevations as they can migrate along elevational gradients depending on their thermal optimum and the surrounding temperature. In most tropical areas, they are found at high elevations in cool temperatures. Yet, they can also be found in lower elevations likely due to their tolerance to warmer weather. Under certain circumstances such as limited resources and competitions from other insects or vertebrates, N. nepalensis would cooperate with individuals of the same species to optimize their chances of reproduction and survival.
Most tropical cyclones form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies. When the subtropical ridge position shifts due to El Nino, so will the preferred tropical cyclone tracks. Areas west of Japan and Korea tend to experience much fewer September–November tropical cyclone impacts during El Niño and neutral years. During El Niño years, the break in the subtropical ridge tends to lie near 130°E which would favor the Japanese archipelago.
Ginger moved ashore in North Carolina, producing heavy rains and damaging winds. An unnamed storm in August attained hurricane status further north than any other Atlantic hurricane. Between 11 and 12 September, five tropical cyclones were active at the same time, the record for the Atlantic basin; this record was later matched in 1995 and in 2020. The season officially began on June 1, and lasted until November 30, 1971; these dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
As is typical for bird-eating raptors, peregrine falcons are sexually dimorphic, with females being considerably larger than males. Peregrine falcons have a flicker fusion frequency of 129 Hz (cycles per second), very fast for a bird of its size, and much faster than mammals. The peregrine's breeding range includes land regions from the Arctic tundra to the tropics. It can be found nearly everywhere on Earth, except extreme polar regions, very high mountains, and most tropical rainforests; the only major ice-free landmass from which it is entirely absent is New Zealand.
The 1992 Pacific hurricane season is the most active Pacific hurricane season on record, featuring 27 named storms, and the second-costliest Pacific hurricane season in history, behind the 2013 season. The season also produced the second-highest ACE value on record in the basin, only surpassed by the 2018 season. The season officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
The 1993 Pacific hurricane season was a slightly above-average Pacific hurricane season with seven named storms directly impacting land. The season officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone developed on June 11, over a month after the traditional start of the season. The final named storm of the season, Tropical Storm Norma, dissipated on October 14.
The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993.(Note: Creation of an account in the website is required in order to access data.) Only two cyclonic storms formed, below the average of four to six. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line in Oceania and East Asia. Storms that form in the Pacific east of the date line and north of the equator in Oceania, North America, Central America, and northwestern South America are called Pacific hurricanes.
The list of North Carolina hurricanes before 1900 encompasses 139 tropical cyclones that affected the U.S. state of North Carolina. Collectively, cyclones in North Carolina during the time period resulted in over 775 direct fatalities during the period. Seven cyclones affected the state in the 1893 season, which was the year with the most tropical cyclones impacting the state during the time period. From the beginning of the official North Atlantic hurricane record in 1851 to 1899, there were 12 years without a known tropical cyclone affecting the state.
Cuban orioles are songbirds and are capable of producing birdsong. Though it has not been observed in Cuban orioles, male and female song has been observed in the Bahama and Puerto Rico orioles as well as most tropical songbirds. Therefore, it is likely that Cuban oriole males and females are capable of singing but further study is required before this can be confirmed. The long song of the Cuban oriole is approximately three seconds with 11-12 notes and its short song is two seconds with 5-6 notes.
Track map of the storms during the season The 1991 Pacific hurricane season produced 16 tropical depressions, 14 of which became tropical storms or hurricanes. The season officially started on May 15, 1997 in the Eastern Pacific—designated as the area east of 140°W—and on June 1, 1997 in the Central Pacific, which is between the International Date Line and 140°W. The season officially ended in both basins on November 30, 1997. These dates typically limit the period of each year when most tropical cyclones form in the eastern Pacific basin.
The 1999 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. Ten days into the start of the season, Tropical Storm Alberto developed in the Caribbean Sea, and after four months of activity, Hurricane Isaac dissipated on October 3 south of Newfoundland. Compared to the devastating 2005 Atlantic hurricane season, 2006 was not severe in terms of deaths and damage. Three tropical storms made landfall in the United States. The first of them, Tropical Storm Alberto, made landfall in Florida with winds of 50 mph (80 km/h), causing flooding and light damage.
These dates historically describe the period each year when most tropical cyclones form in the North Atlantic basin. However, the first named storm, Ana, developed on May 8, nearly a month before the official start of the season, the first pre-season cyclone since Beryl in 2012 and the earliest since Ana in 2003. The formation of Ana marked the first in a series of six consecutive seasons with pre-season activity, spanning from 2015 to 2020. The season concluded with Kate transitioning into an extratropical cyclone on November 11, almost three weeks before the official end.
The 1959 Atlantic hurricane season had a then record-tying number of tropical cyclones – five – develop before August 1\. The season was officially to begin on June 15, 1959 and last until November 15, 1959, the period of each year when most tropical cyclones form in the Atlantic basin, however in actuality the season began early when Tropical Storm Arlene formed on May 28\. Tropical Storm Arlene struck Louisiana and brought minor flooding to the Gulf Coast of the United States. The next storm, Beulah, formed in the western Gulf of Mexico and brought negligible impact to Mexico and Texas.
Jacaranda is a genus of 49 species of flowering plants in the family Bignoniaceae, native to tropical and subtropical regions of Latin America and the Caribbean. It has been planted widely in Asia especially in Nepal. A cosmopolitan plant, Jacaranda mimosifolia is quite common in Southern California, Florida, Mexico, Argentina, Brazil, South Africa, Botswana, Zimbabwe, Australia, New Zealand, Israel, Italy, Portugal, Spain (particularly in Málaga) and Zambia and has been introduced to most tropical and subtropical regions to the extent that it has entered the popular culture. The generic name is also used as the common name.
70 The light rainfall was evident throughout southeastern Florida, except for the Florida Keys, where thunderstorms enhanced the precipitation. This aspect of the storm was considered highly unusual, as most tropical cyclones are characterized by heavy rainfall. According to one study, the unusual precipitation patterns can be attributed to one of two possible conditions: "the air might have been too dry", or "the horizontal convergence of air might have been insufficient to produce a large enough transport of moisture upwards". The intense winds blew salt water several miles inland; due to the lack of rainfall, the salt burned vegetation throughout the region.
The 2013 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones formed in the North Indian Ocean and Arabian Sea. The season had no official bounds, but cyclones typically formed between May and December, with the peak from October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
The 2009 Atlantic hurricane season was a below-average Atlantic hurricane season that produced eleven tropical cyclones, nine named storms, three hurricanes, and two major hurricanes. It officially began on June 1 and ended on November 30, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The season's first tropical cyclone, Tropical Depression One, developed on May 28, while the final storm, Hurricane Ida, dissipated on November 10. The most intense hurricane, Bill, was a powerful Cape Verde-type hurricane that affected areas from the Leeward Islands to Newfoundland.
Palm trees along a street in the Truman Annex Key West has a tropical savanna climate (Köppen Aw, similar to the Caribbean islands). Like most tropical climates, Key West has only a small difference in monthly mean temperatures between the coolest month (January) and the warmest month (July)with the annual range of monthly mean temperatures around . According to the National Weather Service, the Florida Keys and Miami Beach are the only places within the contiguous United States to have never recorded a frost or freeze. The lowest recorded temperature in Key West is on January 12, 1886, and January 13, 1981.
The 1933 Atlantic hurricane season is the third-most active Atlantic hurricane season on record, only behind 2005 and 2020. The season set the pre-satellite era record for most tropical storms formed within a single season, in addition to producing the highest Accumulated Cyclone Energy (ACE) on record in the Atlantic basin, with a total of 259. The season ran through the summer and the first half of fall in 1933, with activity as early as May and as late as November. A tropical cyclone was active for all but 13 days from June 28 to October 7\.
The 2018 North Indian Ocean cyclone season was the most active North Indian Ocean cyclone season since 1992, with the formation of fourteen depressions and seven cyclones. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.
The 1982 Pacific hurricane season, with 23 named storms, ranks as the fourth- most active Pacific hurricane season on record, tied with 2018. It was at that time the most active season in the basin until it was later surpassed by the 1985 season. It officially started June 1, 1982, in the eastern Pacific, and June 1, 1982, in the central Pacific, and lasted until October 31, 1982, in the central Pacific and until November 15, 1982, in the Eastern Pacific. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.
A raised coral atoll or uplifted coral atoll is an atoll that has been lifted high enough above sea level by tectonic forces to protect it from scouring by storms and enable soils and diverse – often endemic – species of flora and fauna to develop.Benton TG. (1995). Biodiversity and biogeography of Henderson Island’s insects. Biological journal of the Linnean Society 56:245–59 With the exception of Aldabra Island in the Indian Ocean and Henderson Island in the Pacific Ocean, most tropical raised atolls have been dramatically altered by human activities such as species introduction, phosphate mining and even bomb testing.
Extent of Tropical and subtropical coniferous forest regions Tropical and subtropical coniferous forests are a tropical forest habitat type defined by the World Wide Fund for Nature. These forests are found predominantly in North and Central America and experience low levels of precipitation and moderate variability in temperature. Tropical and subtropical coniferous forests are characterized by diverse species of conifers, whose needles are adapted to deal with the variable climatic conditions. Most tropical and subtropical coniferous forest ecoregions are found in the Nearctic and Neotropical realms, from the Mid-Atlantic states to Nicaragua and on the Greater Antilles, Bahamas, and Bermuda.
Most tropical cyclones form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies. Areas west of Japan and Korea tend to experience many fewer September–November tropical cyclone impacts during El Niño and neutral years. During El Niño years, the break in the subtropical ridge tends to lie near 130°E, which would favor the Japanese archipelago. Within the Atlantic Ocean vertical wind shear is increased, which inhibits tropical cyclone genesis and intensification, by causing the westerly winds in the atmosphere to be stronger.
The 1962 Pacific typhoon season had no official bounds; there was activity in every month but January, March, and June, but most tropical cyclones form in the northwestern Pacific Ocean between May and November and this conventionally delimits the season. The majority of the Pacific typhoons in 1962 formed in the Pacific Ocean north of the equator and west of the International Date Line with two exceptions: Tropical Depressions Fifty and Sixty-three formed in the Central Pacific. All tropical depressions are assigned a number. Most systems reaching tropical storm strength were assigned a name; all typhoons were named.
The harbor at Saint Thomas, normally shielded from most tropical disturbances, saw extensive impacts; the harbor was most susceptible to a hurricane approaching from the south, as was the case in the 1916 hurricane. Steamers were grounded upon the island by the force of the wind- driven waves. Beached ships included the ocean liners Calabria and Wasgenwald of the Hamburg America Line and the Danish dredge St. Hilda. Calabria and Wasgenwald, both German ships, were interned in the Danish West Indies since the start of World War I. Calabria was considered a total loss and St. Hilda was reduced to smaller fragments.
Track map of all Atlantic tropical cyclones during 1998 The 1998 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. This Atlantic hurricane season saw an above-average number of named tropical storms, and included a single-day record for number of hurricanes simultaneously in progress, with four active on September 25: Georges, Ivan, Jeanne and Karl. The season officially began on June 1, 1998 and ended on November 30, 1998. These dates, adopted by convention, historically describe the period in each year when most tropical systems form.
Despite the season turned out to be active, most tropical cyclones developed during the second half of the year, with only one typhoon, Chanchu developing during the month of May. Some minor systems also developed before May, with the first tropical system of the year, Agaton, developing to the east of Philippines on January 20, bringing minor damages as it crossed the country few days later. Tropical cyclogenesis had become much favorable during late June with formations of Jelawat and Ewiniar. It was also during the same time when NOAA had stated that the weak 2006–07 El Niño had started.
Surf from 1947 Fort Lauderdale hurricane In the period between 1900 and 1949, 108 tropical cyclones affected the state, which collectively resulted in about $4.5 billion (2017 dollars) in damage. Additionally, tropical cyclones in Florida were directly responsible for about 3,500 fatalities during the period, most of which were from the 1928 Okeechobee hurricane. The 1947 season was the year with the most tropical cyclones affecting the state, with a total of six systems. The 1905, 1908, 1913, 1927, 1931, 1942, and 1943 seasons were the only years during the period in which a storm did not affect the state.
Radar image of Hurricane Donna making landfall In the period between 1950 and 1974, 85 tropical or subtropical cyclones impacted the state, which collectively resulted in about $7 billion (2017 dollars) in damage, primarily from Hurricanes Donna and Dora. Additionally, the storms were directly responsible for 93 fatalities and indirectly for 23 more deaths. Several tropical cyclones produced over 20 inches (500 mm) of rainfall in the state, including Hurricane Easy, which is the highest total during the period. The 1969 season was the year with the most tropical cyclones affecting the state, with a total of eight systems.
Navarre Beach largely destroyed by Hurricane Dennis The period from 2000 to the present has been marked by several devastating North Atlantic hurricanes; , 79 tropical or subtropical cyclones have affected the U.S. state of Florida. Collectively, cyclones in Florida over that period resulted in over $123 billion in damage, most of it from Hurricane Irma. Additionally, tropical cyclones in Florida were responsible for 145 direct fatalities and at least 92 indirect ones during the period. Eight cyclones affected the state in both 2004 and 2005, which were the years with the most tropical cyclones impacting the state.
Within the basin, most tropical cyclones have their origins within the South Pacific Convergence Zone or within the Northern Australian monsoon trough, both of which form an extensive area of cloudiness and are dominant features of the season. Within this region a tropical disturbance is classified as a tropical cyclone, when it has 10-minute sustained wind speeds of more than 65 km/h (35 mph), that wrap halfway around the low level circulation centre, while a severe tropical cyclone is classified when the maximum 10-minute sustained wind speeds are greater than 120 km/h (75 mph).
Within the basin, most tropical cyclones have their origins within the South Pacific Convergence Zone or within the Northern Australian monsoon trough, both of which form an extensive area of cloudiness and are dominant features of the season. Within this region a tropical disturbance is classified as a tropical cyclone, when it has 10-minute sustained wind speeds of more than 65 km/h (35 mph), that wrap halfway around the low level circulation centre, while a severe tropical cyclone is classified when the maximum 10-minute sustained wind speeds are greater than 120 km/h (75 mph).
The 2017 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. This Atlantic hurricane season saw above- normal activity; it was the seventh most active season on record and the most active since 2005. The season officially began on June 1, 2017 and ended on November 30, 2017. These dates, adopted by convention, historically describe the period in each year when most tropical systems form. However, storm formation is possible at any time of the year, as demonstrated in 2017 by the formation of the season's first named storm, Tropical Storm Arlene, on April 19\.
Track map of the storms during the season The 1997 Pacific hurricane season was the most active season since the 1994 season, producing 24 tropical depressions, 19 of which became tropical storms or hurricanes. The season officially started on May 15, 1997 in the Eastern Pacific—designated as the area east of 140°W—and on June 1, 1997 in the Central Pacific, which is between the International Date Line and 140°W. The season officially ended in both basins on November 30, 1997. These dates typically limit the period of each year when most tropical cyclones form in the eastern Pacific basin.
The 1998 Atlantic hurricane season was one of the most disastrous Atlantic hurricane seasons on record, featuring the highest number of storm-related fatalities in over 218 years and one of the costliest ever at the time. The season had above average activity, due to the dissipation of the El Niño event and transitioned to La Niña conditions. It officially began on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean. The first tropical cyclone, Tropical Storm Alex, developed on July 27, and the season's final storm, Hurricane Nicole, became extratropical on December 1.
TCWC Wellington warns on systems from 25°S to 40°S and from 160°E to 120°W This is the period of the year when most tropical cyclones form within the South Pacific Ocean. During the season at least 16 people were killed from tropical disturbances whilst overall damage was estimated at $ (2004 USD; $ USD). The most damaging tropical disturbance was Cyclone Heta which caused at least $ (2004 USD; $ USD) in damage to six different countries and left three dead. The deadliest tropical disturbance of the season was Tropical Depression 10F, which was responsible for eleven deaths and caused $ (2004 USD; $ USD) in damage.
Track map of all storms during the season Below is a timeline of the 2007-08 South-West Indian Ocean cyclone season, documenting all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation. The 2007-08 South-West Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It began on November 15, 2007, ended on April 30, 2008, with the exception for Mauritius and the Seychelles, which ended May 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin, which is west of 90°E and south of the Equator.
The 2020–21 South-West Indian Ocean cyclone season is a future event of the annual cycle of tropical cyclone and subtropical cyclone formation. It will officially begin on November 15, 2020, and will officially end on April 30, 2021, with the exception for Mauritius and the Seychelles, for which it will officially end on May 15, 2021. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion.
These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion. The first tropical cyclone was an unnamed moderate tropical storm that formed northeast of Madagascar on September 13, 2018, two months before the official start of the season. Two cyclones formed in the month of November, with Intense Tropical Cyclone Alcide forming on November 5, and Severe Tropical Storm Bouchra entering the basin from the Australian region on November 9.
The 2015–16 season marked the period of the year when most tropical cyclones form within the South Pacific Ocean to the east of 160°E. The season officially ran from November 1, 2015 to April 30, 2016, however a tropical cyclone could form at any time between July 1, 2015 and June 30, 2016 and would count towards the season total. During the season, tropical cyclones are officially monitored by the Fiji Meteorological Service and the Meteorological Service of New Zealand (MetService). Other warning centres like the Australian Bureau of Meteorology and the United States Joint Typhoon Warning Center (JTWC) will also monitor the basin.
The 2012 Pacific hurricane season was a moderately active Pacific hurricane season that saw an unusually high number of tropical cyclones pass west of the Baja California Peninsula. The season officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. However, with the formation of Tropical Storm Aletta on May 14 the season slightly exceeded these bounds. Hurricane Bud intensified into the first major hurricane of the season, one of three to do so in the month of May.
The stonelayer (SL) forms at rates roughly proportional to the numbers of bioturbators and the intensity and style of burrowing. Conveyor-belt soil invertebrates (ants, termites, worms, etc.) are the primary biosorters in most tropical, subtropical, and some midlatitude soils, and thus often produce deep, two-layered biomantles if the soils contain gravels, as many do. Small fossorial vertebrates (pocket gophers, moles, tuco tucos, etc.), on the other hand, tend to be dominant biosorters in many midlatitude soils, especially deserts, prairies, and steppes. In more humid areas, like northeastern U.S. and W. Europe, conveyor- belt ants and worms are probably dominant or co-dominant.
The system drifted northwest while gradually intensifying, and was situated south of the Georgia coast late on September 16. While most tropical systems in the vicinity tend to continue northward along the Eastern Seaboard, the cyclone curved westward and moved ashore near the Florida–Georgia state border after achieving a peak intensity with maximum sustained winds of . It progressed inland over southern Georgia as it quickly weakened, but its intensity leveled off after around 18:00 UTC on September 17. The storm skirted the northern Gulf of Mexico as it swerved slightly south of due west, weakening to a tropical depression over southeastern Louisiana.
The 2018 Atlantic hurricane season was the third in a consecutive series of above-average and damaging Atlantic hurricane seasons, featuring 15 named storms, 8 hurricanes, and 2 major hurricanes, which caused a total of over $50 billion (2018 USD) in damages and at least 172 deaths. The season officially began on June 1, 2018, and ended on November 30, 2018. These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin and are adopted by convention. However, the formation of Tropical Storm Alberto on May 25 marked the fourth consecutive year in which a storm developed before the official start of the season.
The 2017 Pacific typhoon season was a below-average season in terms of Accumulated Cyclone Energy and the number of typhoons and super typhoons, and the first since the 1977 season to not produce a Category 5-equivalent typhoon on the Saffir-Simpson scale. The season produced a total of 27 named storms, 11 typhoons, and only two super typhoons, making it an average season in terms of storm numbers. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season runs throughout 2017, though most tropical cyclones typically develop between May and October.
Flooding from Hurricane Floyd in September 1999, one of North Carolina's worst natural disasters The list of North Carolina hurricanes from 1980 to 1999 encompasses approximately 68 tropical or subtropical cyclones that affected the U.S. state of North Carolina. Collectively, cyclones in North Carolina during the time period resulted in around $10 billion in damage (2007 USD), primarily from hurricanes Fran and Floyd. Additionally, tropical cyclones in North Carolina were responsible for about 56 direct fatalities and at least 47 indirect casualties during the period. Eight cyclones affected the state in the 1985 season, which was the year with the most tropical cyclones impacting the state.
An adult Brown Fish Owl at Barpeta Assam by Hedayeat Ullah The brown fish owl is an all-year resident throughout most tropical and subtropical parts of the Indian Subcontinent to Southeast Asia and adjoining regions. West of its main range, it is patchily distributed to the Levant (possibly extinct) and southern Asia Minor (recently rediscovered). The typical habitat of brown fish owls is forest and woodland bordering streams, lakes or rice fields. It inhabits mainly the lowlands, from open woodland to dense forest as well as in plantations; in the Himalayas foothills it ranges into submontane forest up to above mean sea level or so but not higher.
Furthermore, some initial estimates suggested that Claudette had reached Category 2 status, with sustained winds of up to 100 mph (155 km/h); these were based on unofficial observations which were not backed up by official data. As slow as Claudette was to strengthen, it was also slow to dissipate over land. Inland hurricane warnings were issued for several counties away from the coastline and winds gusted to at Victoria Regional Airport. It maintained tropical storm intensity for over 24 hours after landfall, a rarity for such a weak storm; most tropical systems weaken rapidly after landfall, as they are separated from the warm waters that power them.
Tropical cyclones can attain some of the lowest pressures over large areas on Earth. However, although there is a strong connection between lowered pressures and higher wind speeds, storms with the lowest pressures may not have the highest wind speeds, as each storm's relationship between wind and pressure is slightly different. In the most recent and reliable records, most tropical cyclones which attained a pressure of 900 hPa (mbar) (26.56 inHg) or less have occurred in the Western North Pacific Ocean. The strongest tropical cyclone recorded worldwide, as measured by minimum central pressure, was Typhoon Tip, which reached a pressure of 870 hPa (25.69 inHg) on October 12, 1979.
Human rights issues are also factored into the movement's food politics, and followers are urged to shun third-world cash crops such as coffee, chocolate, sugar, and most tropical fruits. Hardliners include caffeine in their stance on mind-altering drugs so the first two items are generally abstained from, but consumption of the last two is often given more leeway. In keeping with its Abrahamic view of the natural order, the sexual politics of the hardline movement are very conservative. Sex is not allowed except for the reason of procreation; thus homosexuality is seen as anathema, pornography and masturbation is abjured, birth control is avoided, and abortion is militantly opposed.
During the season, twenty-seven tropical cyclones formed in the Eastern Pacific (east of longitude 140°W), and twenty-four developed further and became tropical storms. Both of these figures constitute records in the basin, as the 1992 season surpassed the season with the most tropical cyclones (1982, 26) and the season with the most named storms (1985, 22). Of these, fourteen reached hurricane strength and eight became major hurricanes—storms that reach Category 3 or higher on the Saffir-Simpson Hurricane Scale. This season had five storms reach tropical storm intensity or higher in the month of October, the only time that had happened in this basin.
Hurricane Michael making landfall in Florida near Mexico Beach as a Category 5 hurricane on October 10, 2018 The list of Florida hurricanes from 2000 to the present has been marked by several devastating North Atlantic hurricanes; as of 2017, 79 tropical or subtropical cyclones have affected the U.S. state of Florida. Collectively, cyclones in Florida during the time period resulted in more than $123 billion in damage (2017 USD). Additionally, tropical cyclones in Florida were responsible for 145 direct fatalities and at least 92 indirect casualties during the period. Eleven cyclones affected the state in 2019, which was the year with the most tropical cyclones affecting the state.
Map plotting the track and intensity of all Atlantic tropical and subtropical cyclones during 1974 according to the Saffir–Simpson scale The 1974 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. There was near-average activity during the season, which officially began on June 1, 1974 and ended on November 30, 1974. These dates, adopted by convention, historically describe the period in each year when most tropical systems form. The first system of the season, Tropical Depression One, formed on June 22\. The final system of the season, Tropical Depression Seventeen, dissipated on November 11.
The 1994 Pacific typhoon season was an extremely active season in the annual cycle of tropical cyclone formation in the Western North Pacific, with a total of 32 tropical storms, where 19 of them reached typhoon strength, during the course of the season, much like the Pacific hurricane season. The season had no official bounds and it ran year-round in 1994, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. Tropical storms that formed west of the date line were assigned a name by the Joint Typhoon Warning Center. The World Meteorological Organization-designated Regional Specialized Meteorological Centre for tropical cyclones for the region is the Japan Meteorological Agency.
These dates conventionally delimit the period of each year when most tropical cyclones form in the eastern Pacific basin. The strongest storm of the season was Hurricane Ioke, which reached Category 5 status on the Saffir-Simpson scale in the central Pacific Ocean; Ioke passed near Johnston Atoll and later Wake Island, where it caused heavy damage but no deaths. The deadliest storm of the season was Hurricane John, which killed six people after striking the Baja California Peninsula, and the costliest storm was Hurricane Lane, which caused $203 million in damage in southwestern Mexico (2006 USD, $ USD). Seasonal activity began on May 27, when Tropical Storm Aletta formed off the southwest coast of Mexico.
The 2011–12 South-West Indian Ocean cyclone season was a slightly above average event in tropical cyclone formation. It began on November 15, 2011, and ended on April 30, 2012, with the exception for Mauritius and the Seychelles, for which it ended on May 15, 2012. These dates conventionally delimit the period of each year when most tropical cyclones form in the region; however, Severe Tropical Storm Kuena developed in early June after the season had officially ended. The basin is defined as the area west of 90°E and south of the Equator in the Indian Ocean, which includes the waters around Madagascar westward to the east coast of Africa.
The 2020 North Indian Ocean cyclone season is an ongoing event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and November, with peaks in late April to May and October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The season began on May 16 with the designation of Depression BOB 01 in the Bay of Bengal, later became Cyclone Amphan, one of the strongest storms in the Bay of Bengal recorded since 1999 Odisha Cyclone and beating the record of Cyclone Nargis as the costliest storm in the basin.
A monsoonal system, the depression featured an extensive circulation with the strongest winds well away from the center, contrary to most tropical cyclones. A scatterometer pass revealed winds up to 65 km/h (40 mph) within a banding feature to the east of the storm's center by the evening of June 13. In accordance with this, the JMA upgraded the depression to Tropical Storm 1407 and assigned the name Hagibis to the cyclone. Despite the presence of gale-force winds, the Joint Typhoon Warning Center (JTWC) deemed the system to be below storm intensity and only issued a Tropical Cyclone Formation Alert early on June 14, indicating that it was likely to become a tropical cyclone within 24 hours.
Track map of the storms during the season The 2006 Pacific hurricane season was the most active since the 2000 season, producing 21 tropical depressions; 19 of which became tropical storms or hurricanes. The season officially started on May 15, 2006 in the eastern Pacific, designated as the area east of 140°W, and on June 1, 2006 in the central Pacific, which is between the International Date Line and 140°W, and lasted until November 30, 2006. These dates typically limit the period of each year when most tropical cyclones form in the eastern Pacific basin. This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation.
The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula. There are two main seas in the North Indian Ocean — the Arabian Sea to the west of the Indian subcontinent, abbreviated ARB by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated BOB by the IMD.
Pando has a hot climate, with temperatures commonly above 26 degrees Celsius (80 Fahrenheit). Pando is the least populous department in Bolivia, the most tropical (lying closest to the Equator in the Amazonian Basin), and the most isolated, due to an absence of effective roads. It was organized at the beginning of the 20th century from what was left of the Acre Territory, lost to Brazil as a result of the so-called Acre War (1903). Its capital city of Cobija (the smallest of all the Bolivian departmental capitals) was named after the much-lamented Bolivian port of the same name on the Pacific Ocean, part of an area lost to Chile following the War of the Pacific.
Track map of the storms during the season The 2005 Pacific hurricane season was the least active season since the 2001 season, producing 16 tropical depressions; 15 of which became tropical storms or hurricanes. The season officially started on May 15, 2005 in the eastern Pacific, designated as the area east of 140°W, and on June 1, 2005 in the central Pacific, which is between the International Date Line and 140°W, and lasted until November 30, 2005. These dates typically limit the period of each year when most tropical cyclones form in the eastern Pacific basin. This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation.
The 1988 Pacific hurricane season was a Pacific hurricane season that saw a below-average amount of tropical cyclones form, the first time since 1981. It officially began May 15, in the eastern Pacific, and June 1, in the central Pacific and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The first named storm, Tropical Storm Aletta, formed on June 16, and the last-named storm, Tropical Storm Miriam, was previously named Hurricane Joan in the Atlantic Ocean before crossing Central America and re- emerging in the eastern Pacific; Miriam continued westward and dissipated on November 2.
The 2018 Pacific hurricane season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the eastern Pacific Ocean. The season officially started on May 15 in the eastern Pacific—east of 140°W—and began on June 1 in the central Pacific—between the International Date Line and 140°W, and ended on November 30\. These dates typically cover the period of each year when most tropical cyclones form in the eastern Pacific basin. Four time zones are utilized in the basin: Central for storms east of 106°W, Mountain between 114.9°W and 106°W, Pacific between 140°W and 115°W, and Hawaii–Aleutian for storms between the International Date Line and 140°W.
The season began with Subtropical Storm Ana on April 20, prior to the official start of the season; the bounds of the season are from June 1 to November 30, which conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. In early September, Hurricane Fabian struck Bermuda as a Category 3 hurricane, where it was the worst hurricane since 1926; on the island it caused four deaths and $300 million in damage (2003 USD). Hurricane Juan caused considerable destruction to Nova Scotia, particularly Halifax, as a Category 2 hurricane, the first hurricane of significant strength to hit the province since 1893. Additionally, Hurricanes Claudette and Erika struck Texas and Mexico, respectively, as minimal hurricanes.
At 19:30 UTC, the JTWC issued a Tropical Cyclone Formation Alert despite satellite imagery only detecting a broad, ill-defined low-level circulation, with a minimum barometric pressure of . By 00:00 UTC on July 23, Dvorak intensity estimates reached T2.5/ and a ship to the north of the system reported winds of , which resulted in the JTWC declaring the system a tropical depression. Initially, the depression was tracking west and was forecast by the JTWC to track across the Philippine Islands. This was in agreement with most tropical cyclone forecast models showing the storm track across the archipelago and the turning northward in the general direction of China, although the JTWC eventually shifted the track further north into the Luzon Straits.
Most tropical cyclones form in a worldwide band of thunderstorm activity near the equator, referred to as the Intertropical Front (ITF), the Intertropical Convergence Zone (ITCZ), or the monsoon trough. Another important source of atmospheric instability is found in tropical waves, which contribute to the development of about 85% of intense tropical cyclones in the Atlantic Ocean and become most of the tropical cyclones in the Eastern Pacific. The majority forms between 10 and 30 degrees of latitude away of the equator, and 87% forms no farther away than 20 degrees north or south. Because the Coriolis effect initiates and maintains their rotation, tropical cyclones rarely form or move within 5 degrees of the equator, where the effect is weakest.
Season track map The 2006 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. Following the intense activity in the 2005 season, forecasts had initially predicted that the 2006 Atlantic hurricane season would be only slightly less active. However, activity was slowed by a rapidly forming El Niño event in 2006, the presence of the Saharan Air Layer over the tropical Atlantic, and the steady presence of a robust secondary high-pressure area to the Azores high centered on Bermuda. The season officially began on June 1, 2006, and lasted until November 30, 2006, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin.
The 2020–21 South Pacific cyclone season is the period of the year when most tropical cyclones form within the South Pacific Ocean to the east of 160°E. The season officially runs from November 1, 2020 to April 30, 2021, however a tropical cyclone could form at any time between July 1, 2020 and June 30, 2021 and would count towards the season total. During the season, tropical cyclones will be officially monitored by the Regional Specialized Meteorological Center (RSMC) in Nadi, Fiji and the Tropical Cyclone Warning Centers in Brisbane, Australia and Wellington, New Zealand. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) will also monitor the basin and issue unofficial warnings for American interests.
These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, as illustrated by Hurricane Pali, which became the earliest Central Pacific tropical cyclone on record, the formation of tropical cyclones is possible at any time of the year. After Pali, however, the active season had a slow start, becoming the first season since 2011 in which no tropical cyclones occurred in May, and also the first since 2007 in which no named storms formed in the month of June. Hurricane Darby brushed the Hawaiian islands as a tropical storm causing only minor damage; while hurricanes Lester and Madeline also threatened to make landfall in Hawaii but weakened significantly before approaching the islands.
The 1994 Atlantic hurricane season was the final season in the most recent Negative Atlantic multidecadal oscillation (“low-activity era” or “cold phase”) of tropical cyclone formation in the Atlantic. Despite the below average activity, the season was very deadly, with most of the deaths occurring during Hurricane Gordon, a devastating late-season tropical cyclone that caused severe impacts to the Caribbean Sea, the Greater Antilles and the United States, and one of the longest-lived Atlantic hurricanes on record at the time. The season produced seven named tropical cyclones and three hurricanes, a total below the seasonal average. The season officially started on June 1 and ended on November 30, dates which conventionally limit the period during which most tropical cyclones form in the Atlantic Ocean.
Photo of one whole and one split mango displaying its seed, which is approximately 1/3 the size of the entire fruit Recalcitrant seeds are seeds that do not survive drying and freezing during ex-situ conservation. By and large, these seeds cannot resist the effects of drying or temperatures less than 10 °C (50 °F); thus, they cannot be stored for long periods like orthodox seeds because they can lose their viability. Plants that produce recalcitrant seeds include avocado, mango, mangosteen, lychee, cocoa, rubber tree, some horticultural trees, aquatic plants, such as Nymphaea caerulea, and several plants used in traditional medicine, such as species of Virola and Pentaclethra. Generally speaking, most tropical pioneer species have orthodox seeds but many climax species have recalcitrant or intermediate seeds.
The three domains (in the Northwest Pacific Basin) of the PAGASA for their monitoring of tropical cyclone activity: PAR (gray broken lines), TCAD (red), and TCID (yellow) Aside from the PAR, PAGASA forecasters have two other areas of responsibilities for tropical cyclone monitoring: the Tropical Cyclone Advisory Domain (TCAD) and the Tropical Cyclone Information Domain (TCID). Together with the PAR, these three areas of the Northwest Pacific Basin are collectively called domains. Since most tropical cyclones come from the broad expanse of ocean east of the country, the eastern boundaries of the PAR, TCAD and TCID are farther from the archipelago than the western boundaries. The TCAD, considered to be the "middle domain," is located between the PAR and the TCID.
The short-wave soon left the area, causing wind shear to decrease and convection quickly re-developed. By early on September 9, Hortense was upgraded to a hurricane, while curving northwestward. Around 0600 UTC on the following day, the storm made landfall near Guánica, Puerto Rico with winds of 80 mph (130 km/h); this made it the first hurricane landfall on the island since Hurricane Hugo in 1989. Initially, most tropical cyclone forecast models anticipated Hortense would pass south of the island and instead strike the Dominican Republic. After two hours, Hortense emerged into the Mona Passage and brushed the eastern tip of Dominican Republic; Punta Cana near the eastern tip of the country reported the calm of the eye on September 10\.
The 2019 Pacific hurricane season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the eastern Pacific Ocean. The season officially started on May 15 in the eastern Pacific—east of 140°W—and June 1 in the central Pacific—between the International Date Line and 140°W, and ended on November 30\. These dates typically cover the period of each year when most tropical cyclones form in the eastern Pacific basin. Four time zones are utilized in the basin: Central for storms east of 106°W, Mountain between 114.9°W and 106°W, Pacific between 140°W and 115°W, and Hawaii–Aleutian for storms between the International Date Line and 140°W.
Also, climate change impact is feared to be significant. Considerable analysis has been conducted on the sustainable yield of firewood production, a major threat to deforestation in most tropical countries. Biological inventory work; assessment of harvesting practices; and computer modeling of the dynamics of treefall, rot and harvest; have been carried out to adduce data on safe harvesting rates. Extensive research has also been conducted on the relation of brush clearance to biodiversity decline and impact on water tables;Andreas Glanznig, Native Vegetation Clearance, Habitat Loss and Biodiversity Decline: an overview of recent native vegetation clearance in Australia and its implications for biodiversity, Biodiversity Series, Paper No. 6, Biodiversity Unit, June 1995 for example, these effects have been analyzed in the Toolibin Lake wetlands region.
The 2017 Pacific hurricane season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the eastern Pacific Ocean. The season officially started on May 15 in the eastern Pacific—east of 140°W—and on June 1 in the central Pacific—between the International Date Line and 140°W—and ended on November 30\. These dates typically cover the period of each year when most tropical cyclones form in the eastern Pacific basin. Four time zones are utilized in the basin: Central for storms east of 106°W, Mountain between 114.9°W and 106°W, Pacific between 140°W and 115°W, and Hawaii–Aleutian for storms between the International Date Line and 140°W.
The 1993 Atlantic hurricane season was a below average Atlantic hurricane season that produced ten tropical cyclones, eight tropical storms, four hurricanes, and one major hurricane. It officially started on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean. The first tropical cyclone, Tropical Depression One, developed on May 31, while the final storm, Tropical Depression Ten, dissipated on September 30, well before the average dissipation date of a season's last tropical cyclone; this represented the earliest end to the hurricane season in ten years. The most intense hurricane, Emily, was a Category 3 on the Saffir–Simpson Hurricane Scale that paralleled close to the North Carolina coastline causing minor damage and a few deaths before moving out to sea.
The 2007 Pacific hurricane season was a below-average Pacific hurricane season, featuring one major hurricane. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the region. The first tropical cyclone of the season, Alvin, developed on May 27, while the final system of the year, Kiko, dissipated on October 23\. Due to unusually strong wind shear, activity fell short of the long-term average, with a total of 11 named storms, 4 hurricanes, and 1 major hurricane. At the time, 2007 featured the second-lowest value of the Accumulated cyclone energy (ACE) index since reliable records began in 1971.
In accordance with climatological norms, September was the most active month of the season, featuring eight tropical cyclones: tropical storms Gaston, Hermine, Matthew, and Nicole, as well as hurricanes Igor, Julia, Karl, and Lisa. This tied 1949, 2002, and 2007 for the most tropical storms observed throughout the month, until it was surpassed by the 2020 season.. Igor attained peak winds of 155 mph (250 km/h) on September 15, cementing its status as the most intense storm of the season. Well above- average activity continued into October, with the formation of hurricanes Otto, Paula, Richard, Shary, and Tomas, one hurricane short of the monthly record set in 1870. Tomas persisted into the subsequent month before dissipating on November 7, heralding the end of the season's tropical cyclone activity.
One storm, the twelfth of the season, was unnamed and was originally excluded from the yearly summary, and three additional storms were discovered in re-analysis. The large quantity of strong storms during the year yielded, prior to modern reanalysis, what was the highest seasonal accumulated cyclone energy (ACE) of the 20th century in the Atlantic basin; 1950 held the seasonal ACE record until broken by the 1995 Atlantic hurricane season. However, later examination by researchers determined that several storms in the 1950 season were weaker than thought, leading to a lower ACE than assessed originally. This season also set the record for the most tropical storms, eight, in the month of October. The tropical cyclones of the season produced a total of 88 fatalities and $38.5 million in property damage (1950 USD).
Starting in World War II, DDT was used as insecticide to combat insect vectors carrying malaria, which was endemic in most tropical regions of the world.James L.A. Webb Jr., Humanity's Burden: A Global History of Malaria (2009); Randall M. Packard, The Making of a Tropical Disease: A Short History of Malaria (2007); Leo B. Slater, War and Disease: Biomedical Research on Malaria in the Twentieth Century (2009). The first goal was to protect soldiers, but it was widely adopted as a public health device. In Liberia, for example, the United States had large military operations during the war and the U.S. Public Health Service began the use of DDT for indoor residual spraying (IRS) and as a larvicide, with the goal of controlling malaria in Monrovia, the Liberian capital.
Elevated sea surface temperatures, contrasting with cold atmospheric air, encourage atmospheric instability, especially within the troposphere. In general, most Medicanes maintain a radius of , last between 12 hours and 5 days, travel between , develop an eye for less than 72 hours, and feature wind speeds of up to ; in addition, a majority are characterized on satellite imagery as asymmetric systems with a distinct round eye encircled by atmospheric convection. Weak rotation, similar to that in most tropical cyclones, is usually noted in a Medicane's early stages, increasing with intensity; Medicanes, however, often have less time to intensify, remaining weaker than most North Atlantic hurricanes and only persisting for the duration of a few days. The theoretical maximum potential intensity of Medicanes is equivalent to the lowest classification on the Saffir–Simpson hurricane wind scale, a Category 1 hurricane.
The system's atmospheric pressure increased throughout 15 January due to the fact it was embedded within a large-scale environment, with its rising pressure due to the general prevalence of higher air pressures throughout the region, and was not a sign of deintensification. Initial wind speeds within the young medicane were generally low, with sustained winds of merely , with the highest recorded value associated with the disturbance being at 0000 UTC on 16 January, slightly below the threshold for tropical storm on the Saffir–Simpson hurricane wind scale. Its structure now consisted of a distinct eye encircled by counterclockwise-rotating cumulonimbi with cloud top temperatures colder than , evidencing deep convection and a regular feature observed in most tropical cyclones. At 1200 UTC on 16 January, a ship recorded winds blowing east-southeast of about south-southwest about north-northeast of the cyclone's center.
Upon moving ashore, an area of convection increased over the center, and the convection initially became better defined as it crossed the Yucatán Peninsula. While most tropical cyclones weaken and become disorganized after landfall, Alex seemed to become stronger when viewed on radar and satellite imagery--the National Hurricane Center noted in one of its forecast discussions that the cyclone's structure more closely resembled a hurricane than a deteriorating storm. Still, after enough time over land, convective activity markedly decreased, and Alex weakened to tropical depression status as it approached the peninsula's western coastline; although post-analysis determined that Alex remained a minimal tropical storm. Late on June 27, the storm emerged into the Gulf of Mexico with a large overall convective structure but little thunderstorm activity near the center due to the interaction with land.
Annual liquid precipitation (rain) averages and is plentiful year-round, but with a slightly drier summer. Annual frozen precipitation (snow) averages in the city. However, neighborhoods away from the immediate coast average slightly more, as the warmer ocean waters and onshore flow can cause snow to transition to sleet or rain along the coast. In Southern Maine, winter-season snowstorms can be intense from November through early April, while warm-season thunderstorms are somewhat less frequent than in the Midwestern, Mid-Atlantic, and Southeastern U.S. Direct strikes by hurricanes or tropical storms are rare, partially due to the normally cooler Atlantic waters off the Maine coast (which usually weaken tropical systems), but primarily because most tropical systems approaching or reaching 40 degrees North latitude recurve (due to the Coriolis force) and track east out to sea well south of the Portland area.
These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialized Meteorological Centre in Réunion. For the second consecutive year in a row, the first system formed before the official start of the season. Afterwards, three storms formed in the month of December: Tropical Cyclone Belna on 2 December, which brought flooding and strong wind to northwestern Madagascar, Very Intense Tropical Cyclone Ambali, which formed a day later and became the first very intense tropical cyclone in the basin since Fantala in 2016, and Tropical Cyclone Calvinia which stalled near Mauritius and brought heavy rain and moderate flooding to the island nation towards the end of the month, crossing into 2020.
The 2007 Atlantic hurricane season was a slightly above-average Atlantic hurricane season, featuring many weak and short-lived storms. Despite the high activity of weak storms during 2007, it was the first season to feature more than one Category 5 landfalling hurricane, a feat that would not be matched until ten years later. It produced 17 tropical cyclones, 15 tropical storms, six hurricanes, and two major hurricanes. It officially started on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean, although as shown by Subtropical Storm Andrea and Tropical Storm Olga in early May and early December, respectively, the formation of tropical cyclones is possible at any time of the year. The first system, Subtropical Storm Andrea, developed on May 9, while the last storm, Tropical Storm Olga, dissipated on December 13\.
The 2015 Pacific hurricane season was the second-most active Pacific hurricane season on record, and featured the strongest tropical cyclone ever observed in the Western Hemisphere: Hurricane Patricia. The season officially started on May 15 in the Eastern Pacific—east of 140°W—and on June 1 in the Central Pacific—between the International Date Line and 140°W—and ended on November 30\. These dates typically cover the period of each year when most tropical cyclones form in the Northeastern Pacific tropical cyclone basin. The season's first storm, Hurricane Andres, developed on May 28; the season's final storm, Tropical Depression Nine-C, dissipated on December 31, well after the official end of the season. Throughout the season, 31 tropical depressions developed, 26 of which became tropical storms, a record-tying 16 of them reached hurricane strength, and a record-breaking 11 achieved major hurricane intensity.
Edwards' alt=An oil painting depicting a red-feathered parrot with yellow wing tips; a large, ungainly, duck-like bird with grey, white and yellow feathers; a parrot with a black back, yellow breast and a yellow and black tail; and a brown- feathered bird with a long bill eating a frog Much information about the bird's appearance comes from a painting attributed to Hoefnagel, based on a bird in the menagerie of Emperor Rudolph II around 1610. It is the only coloured depiction of the species, showing the plumage as reddish brown, but it is unknown whether it was based on a stuffed or living specimen. The bird had most likely been brought alive to Europe, as it is unlikely that taxidermists were on board the visiting ships, and spirits were not yet used to preserve biological specimens. Most tropical specimens were preserved as dried heads and feet.
Cosalá is classified as having a Köppen Tropical Wet and Dry (Aw) Climate, despite being situated about 1 degree above the Tropic of Cancer. Most municipalities to the north of Cosalá, such as Culiacán, have semi-arid to arid climates, as one moves towards the Sonoran-Sinaloan Transitional Subtropical Forests, and into the Sonoran Desert. Cosalá experiences much greater diurnal temperature variations than most Tropical Wet and Dry climates, especially during the winter months, where temperatures regularly drop as low as 10C in January and February (compare this to Mazatlán, located about 1 degree south, inside the Tropic of Cancer, where nighttime temperatures in January and February are about 15C on average). Daytime temperatures also tend to be hotter than most locations further south (highs approaching 37C in May/Jun, compared to 30C-33C for Mazatlán), and as such, Cosala's climate behaves more similarly to a semi-arid climate, in this regard, than a truly tropical climate.
Its island distribution includes the Andamans, Sumatra (including Simeulue and Mentawai off the west side and Riau, Bangka and Belitung off of the east), Java, Borneo and the western and southern Philippines (including Palawan, Calamians, Lubang, Mindoro, Mindanao and apparently recently Bohol). Like most tropical raptors, the changeable hawk-eagle is largely residential, but stragglers from peninsular India have roamed to northeastern Burma and southeastern Thailand and some records in the Lesser Sunda Islands (Bali, Palau and Lombok) may be from vagrants from Java. The species may live in savannah woodland, cultivation with trees, timbered watercourses, tea plantations, forest villages and even suburban edge. Beyond these often degraded haunts they range as well as any of the more forest- clinging Nisaetus into fairly open or less dense parts of undisturbed vast evergreen or deciduous forests (their deciduous ranges mainly occurring in India and the Sunda islands), but also second growth and wetlands.

No results under this filter, show 420 sentences.

Copyright © 2024 RandomSentenceGen.com All rights reserved.