Bacteria will immediately start growing once the meat becomes warmer than 40 degrees.
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In Northern Europe, ticks are proliferating as forests recover and the climate becomes warmer.
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That's because if the air over the desert of the Great Basin becomes warmer, its relative humidity will decrease.
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"During the ice ages, the bands of vegetation moved up and down as the environment becomes warmer or colder," Dearing said.
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Transmission in the U.S. may start to happen as the weather becomes warmer, however, the propagation of the virus is less predictable.
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When the climate becomes warmer, the vine will accelerate its growth and its sugar development, and the development of flavor and aroma gets decoupled from acid and sugar.
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There, the process becomes a pseudo-adiabatic process whereby the liquid water or salt that condenses is assumed to be removed upon formation by idealized instantaneous precipitation. The pseudoadiabatic process is only defined for expansion because a compressed parcel becomes warmer and remains undersaturated.
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Retrieved 5 September 2012. Retrieved 5 September 2012. Retrieved 7 September 2012. As the climate becomes warmer in the future, there is likely to be more tourism pressure on the coasts, but the effects of this may be mitigated by a move towards lower- impact activities like bathing.
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Cold air travels over warm lake water. The air becomes warmer, moister, less dense, so that it rises; when it passes over land, the reduced airspace causes the air to "pile up" resulting in "frictional convergence." This lifts the air even further to where it cools, turning into droplets or snowflakes. The result is enhanced snowfall.
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Hence, such an air mass becomes warmer relative to the atmosphere. As warmer air is less dense, such an air mass would tend to continue to rise. Conversely, if the adiabatic lapse rate is higher than the ambient lapse rate, an air mass displaced upward cools more rapidly than the air in which it is moving. Hence, such an airmass becomes cooler relative to the atmosphere.
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If the slopes are covered with ice and snow, the mountain breeze will blow during the day, carrying the cold dense air into the warmer, barren valleys. The slopes of hills not covered by snow will be warmed during the day. The air that comes in contact with the warmed slopes becomes warmer and less dense and flows uphill. This is known as an anabatic wind or valley breeze.
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The endangered Black-necked cranes migrate to the middle and southern part of Tibet every winter, and may be seen on the reservoir. The cranes migrate from the frozen Changtang Grassland in northern Tibet in mid- to late-October, and overwinter in Linzhou (Lhünzhub) County. They return when the weather becomes warmer, in late March. They are the only species of crane that lives and breeds at these high elevations.
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Gib asks her where she heard about people getting frozen, and she tells him that it was all over the papers when Georgie Olson died of pneumonia. After seeing Gib's reaction to the news, Livy becomes warmer towards him. On the sixteenth of December, Gib's birthday, a blizzard blows up and Mr. Thornton is stuck is town. Mrs. Thornton arranges a surprise party for Gib, and she and the others give him presents.
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The mean temperature during the summer is around . It's the sunniest season, averaging as much as 10 hours of sunshine per day in January with an average of 7–8 clear days and only 5-7 overcast days. Spring and fall are transition seasons featuring mild temperatures during the day and cool to cold nights. Spring starts out with cool temperatures during the day and very cold nights which progressively becomes warmer.
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After the concert, Robert, fascinated by Sophia, suggests arranging a photo shooting and writing an article about her. Soon Robert and Sophia's relationship becomes warmer and takes a romantic turn thus triggering Jeans' fierce jealousy. Sophia suggests Robert visit her favorite childhood place – a gorge known as the "Gate to Heaven", which she used to visit with her late father, photographer Edgar Martirosyan. Edgar had been taken prisoner and killed during the war in 1992.
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Therefore, bodies of water stay at a more even temperature, while land temperature are more variable. During warmer months sunlight heats the surfaces of both land and oceans, but land temperatures rise more quickly. As the land's surface becomes warmer, the air above it expands and an area of low pressure develops. Meanwhile, the ocean remains at a lower temperature than the land, and the air above it retains a higher pressure.
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During La Niña, Miami becomes warmer and drier than normal. 2015 was a record-breaking year for the southern part of the state, with four cities breaking records by a wide margin. It was also an El Niño year that ended with a December several degrees above normal. While the climate for much of the state is humid subtropical, South Florida qualifies as one of several tropical classifications (Köppen Aw, Am, or Af).
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Snowfall is common during the winter months. Winters are cloudy and are characterised by low amounts of sunshine, ranging from only 0.5 hours of sunshine per day in December to 4.1 hours in March. At the winter solstice daylight lasts for only 6 hours. Spring starts out cool, with freezing temperatures common in March and April but gradually becomes warmer in late May when daytime temperatures average although nighttime temperatures still remain cool, averaging from March to May.
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There is another possible mechanism for rapid methane release. As the Arctic Ocean becomes more and more ice free, the ocean absorbs more of the incident energy from the sun. The Arctic Ocean becomes warmer than the former ice cover and much more water vapour enters the air. At times when the adjacent land is colder than the sea, this causes rising air above the sea and an off-shore wind as air over the land comes in to replace the rising air over the sea.
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Plants operating in hot climates may have to reduce output if their source of condenser cooling water becomes warmer; unfortunately this usually coincides with periods of high electrical demand for air conditioning. If a good source of cooling water is not available, cooling towers may be used to reject waste heat to the atmosphere. A large river or lake can also be used as a heat sink for cooling the condensers; temperature rises in naturally occurring waters may have undesirable ecological effects, but may also incidentally improve yields of fish in some circumstances.
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In 2005, British researchers noticed that the net flow of the northern Gulf Stream had decreased by about 30% since 1957. Coincidentally, scientists at Woods Hole had been measuring the freshening of the North Atlantic as Earth becomes warmer. Their findings suggested that precipitation increases in the high northern latitudes, and polar ice melts as a consequence. By flooding the northern seas with excessive fresh water, global warming could, in theory, divert the Gulf Stream waters that usually flow northward, past the British Isles and Norway, and cause them to instead circulate toward the equator.
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How Foehn is produced Some more localized phenomena than global atmospheric movement are also due to convection, including wind and some of the hydrologic cycle. For example, a foehn wind is a down-slope wind which occurs on the downwind side of a mountain range. It results from the adiabatic warming of air which has dropped most of its moisture on windward slopes. Because of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than at the same height on the windward slopes.
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Stormwater that runs over paved areas and land becomes warmer. Effective stormwater management reduces such thermal pollution, which is important for cold water species such as Lake Trout. The group works very closely with the City of Traverse City, numerous townships, and scores of project partners and volunteers from myriad organizations and businesses throughout the Grand Traverse region to protect Grand Traverse Bay from stormwater pollution. Macrophyte Bed Study: Macrophytes include rooted aquatic plants such as cladophora and algae such as chara, both of which are on the rise in Grand Traverse Bay.
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The storms that result from combining warm and cold temperatures have a huge affect in the northern region of the Agulhas Current. As it goes down the continent of Africa, the atmosphere becomes warmer, and the weather mellows out into a steady rainfall, giving South Africa and West Madagascar humidity and storms. Another factor contributing to weather conditions in the South African- Madagascar region is the contribution of the South Equatorial Madagascar Current. This particular current travels westward from the Indian Ocean, hitting the east coast of Madagascar.
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Springtime conditions generally run from late February through early June, during which time the overall trend gradually becomes warmer and drier and the landscape briefly turns lush and green. This is the windiest season of all, with a powerful west wind on most afternoons. During stormy periods in spring, conditions are usually cloudy and cool, while most sunny and calm days become intensely warm, especially from April onward. Springtime temperatures often vary more from one week to the next than they do from one month to the next.
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In the third book, Emily saves him from the Elf King's guards when they attempted to arrest him, using a stunning staff to electrocute him. He tells Emily that his father is being possessed by something, and that he wanted to destroy whatever was controlling his dead body by destroying the amulet of the king. In the fifth book, they find out it was the Voice. In the sixth book, Trellis becomes warmer to the crew of the Luna Moth, especially Luger, playing a game of Othello together and exchanging witty banter.
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Isentropic draw-down is the draw-down of warmer, drier air from aloft. When the approaching winds are insufficiently strong to propel the low- level air up and over the mountain barrier, the airflow is said to be 'blocked' by the mountain and only air higher up near mountain-top level is able to pass over and down the lee slopes as foehn winds. These higher source regions provide foehn air that becomes warmer and drier on the leeside after it is compressed with descent due to the increase in pressure towards the surface.
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If this energy balance is shifted, Earth's surface becomes warmer or cooler, leading to a variety of changes in global climate.. A number of natural and man-made mechanisms can affect the global energy balance and force changes in Earth's climate. Greenhouse gases are one such mechanism. Greenhouse gases absorb and emit some of the outgoing energy radiated from Earth's surface, causing that heat to be retained in the lower atmosphere. As explained above, some greenhouse gases remain in the atmosphere for decades or even centuries, and therefore can affect Earth's energy balance over a long period.
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The cave system is unusual for containing three different microclimatic layers which makes it extremely interesting in terms of biodiversity to scientists. The first of the cave system's entrance is permanently covered in thick layers of snow and ice and has an average air temperature of . The cave system progressively becomes warmer in deeper areas, with an average air temperature of in the middle part and at the bottom. Empty shells of Zospeum tholussum were encountered by the team beginning at a depth of and down to the lake at the bottom of the cave, which is about beneath the Trojama cave entrance.
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It is known as overturning. In the Pacific Ocean, the rest of the cold and salty water from the Atlantic undergoes haline forcing, and becomes warmer and fresher more quickly. The out-flowing undersea of cold and salty water makes the sea level of the Atlantic slightly lower than the Pacific and salinity or halinity of water at the Atlantic higher than the Pacific. This generates a large but slow flow of warmer and fresher upper ocean water from the tropical Pacific to the Indian Ocean through the Indonesian Archipelago to replace the cold and salty Antarctic Bottom Water.
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In 2005, British researchers noticed that the net flow of the northern Gulf Stream had decreased by about 30% since 1957. Coincidentally, scientists at Woods Hole had been measuring the freshening of the North Atlantic as Earth becomes warmer. Their findings suggested that precipitation increases in the high northern latitudes, and polar ice melts as a consequence. By flooding the northern seas with an enormous amount of extra fresh water, global warming could, in theory, divert the Gulf Stream waters that usually flow northward, past the British Isles and Norway, and cause them to instead circulate toward the Equator.
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March is the wettest month of the city, and remains cool, but towards the end of the month becomes warmer. Western Disturbances continues to affect the weather, producing hailstorms and causing rains with strong winds, and the chances of snowfall on the mountains around the city, and occasional chances of snowfall in the city mostly during the first two decades of the month. The likelihood of thunderstorms is very high during the month, with the possibility of some incredible thunders in the city followed by heavy downpour. On 8 March 2007 light snowfall occurred in the city.
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A föhn or foehn is a type of dry, warm, down-slope wind that occurs in the lee (downwind side) of a mountain range. Föhn can be initiated when deep low pressures move into Europe drawing moist Mediterranean air over the Alps. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes.
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It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Föhn winds can raise temperatures by as much as 14 °C (25 °F) in just a matter of hours. Switzerland, southern Germany and Austria have a warmer climate due to the Föhn, as moist winds off the Mediterranean Sea blow over the Alps.
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Temperature can also greatly affect the ability of aquatic organisms to move through water. This is because temperature not only affects the properties of the water, but also the organisms in the water, as most have an ideal range specific to their body and metabolic needs. Q10 (temperature coefficient), the factor by which a rate increases at a 10 °C increase in temperature, is used to measure how organisms' performance relies on temperature. Most have increased rates as water becomes warmer, but some have limits to this and others find ways to alter such effects, such as by endothermy or earlier recruitment of faster muscle.
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Banksia prionotes grows as a tree up to high in southern parts of its distribution, but in northern parts it is usually a shorter tree or spreading shrub, reaching about in height; it diminishes in size as the climate becomes warmer and drier further north. It has thin, mottled grey, smooth or grooved bark, and tomentose young stems. The alternate dull green leaves are long, and wide, with toothed leaf margins made up of triangular lobes, and often a wavy surface. Flowers occur in a typical Banksia flower spike, an inflorescence made up of hundreds of small individual flowers, or florets, densely packed around a cylindrical axis.
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Systematic errors which change during an experiment (drift) are easier to detect. Measurements indicate trends with time rather than varying randomly about a mean. Drift is evident if a measurement of a constant quantity is repeated several times and the measurements drift one way during the experiment. If the next measurement is higher than the previous measurement as may occur if an instrument becomes warmer during the experiment then the measured quantity is variable and it is possible to detect a drift by checking the zero reading during the experiment as well as at the start of the experiment (indeed, the zero reading is a measurement of a constant quantity).
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The Chinook is a föhn wind, a rain shadow wind which results from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes (orographic lift). As a consequence of the different adiabatic rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. As moist winds from the Pacific (also called "Chinooks") are forced to rise over the mountains, the moisture in the air is condensed and falls out as precipitation, while the air cools at the moist adiabatic rate of 5 °C / 1000 m (3.5 °F / 1000 ft). The dried air then descends on the leeward side of the mountains, warming at the dry adiabatic rate of 10 °C / 1000 m (5.5 °F / 1000 ft).
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The limiting factor is the temperature of the cooling water and that, in turn, is limited by the prevailing average climatic conditions at the power station's location (it may be possible to lower the temperature beyond the turbine limits during winter, causing excessive condensation in the turbine). Plants operating in hot climates may have to reduce output if their source of condenser cooling water becomes warmer; unfortunately this usually coincides with periods of high electrical demand for air conditioning. The condenser generally uses either circulating cooling water from a cooling tower to reject waste heat to the atmosphere, or once-through cooling (OTC) water from a river, lake or ocean. In the United States, about two-thirds of power plants use OTC systems, which often have significant adverse environmental impacts.
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The pennant cloud is not seen in westerly winds, although many of the same processes occur - it is just that the air is usually drier and may be warmer, as well as being less stable – so that convection from the surface is deeper and not capped near the mountaintop level. (Low cloud can sometimes be seen on the Rock, early in the morning in westerly winds, but this disappears as temperatures rise. It is also likely that the very steep eastern slope of the Rock tends to make the downwind flow too turbulent for cloud formation.) Around dawn, the flow is relatively smooth through the cloud, but later in the morning, as it becomes warmer, some convective overturning develops within the plume as temperatures rise. Formation of the cloud is classically very near the top of the ridge-line of the Rock at nearly 400 m altitude, but the base is usually a little lower in the turbulent flow to the west.
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Despite initial good fortune, the ship is driven south by a storm and eventually reaches the icy waters of the Antarctic. An albatross appears and leads the ship out of the ice jam where it is stuck, but even as the albatross is fed and praised by the ship's crew, the mariner shoots the bird: The crew is angry with the mariner, believing the albatross brought the south wind that led them out of the Antarctic. However, the sailors change their minds when the weather becomes warmer and the mist disappears: They soon find that they made a grave mistake in supporting this crime, as it arouses the wrath of spirits who then pursue the ship "from the land of mist and snow"; the south wind that had initially blown them north now sends the ship into uncharted waters near the equator, where it is becalmed: Engraving by Gustave Doré for an 1876 edition of the poem. "The Albatross" depicts 17 sailors on the deck of a wooden ship facing an albatross.
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Conversely, a sinking parcel is compressed and becomes warmer even though no heat is added. Air at the top of a mountain is usually colder than the air in the valley below, but the arrangement is not unstable: if a parcel of air from the valley were somehow lifted up to the top of the mountain, when it arrived it would be even colder than the air already there, due to adiabatic cooling; it would be heavier than the ambient air, and would sink back toward its original position. Similarly, if a parcel of cold mountain-top air were to make the trip down to the valley, it would arrive warmer and lighter than the valley air, and would float back up the mountain. So cool air lying on top of warm air can be stable, as long as the temperature decrease with height is less than the adiabatic lapse rate; the dynamically important quantity is not the temperature, but the potential temperature--the temperature the air would have if it were brought adiabatically to a reference pressure.
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