For almost two hours he tried swimming out of the cold current, holding her, eventually getting to the shore.
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We talked about his collaborations, the attention from other musicians, the short film for Giacomo Triglia, the videos that started to circulate, the contacts with a Roman label called Cold Current, the parent label of Centre of Wood, with whom he recorded Separations.
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When the low air pressure and typhoons pass through the Sea of Japan, Sado Island often suffers from Foehn wind, rising the temperature sharply. Located at the junction of the warm and cold current, Sado City enjoys diverse plants and rich aquatic resources.
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Severo-Kurilsk has a subarctic climate (Köppen Dfc). The monthly average temperature is greater than 10 degrees Celsius only in August and September. Due to the influence of the cold current of the Oyashio current , it is cold and humid all year round. The annual precipitation is more than five times that of Siberia.
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Thick clouds for the most part shut out the sun; while the cold current from the Sea of Okhotsk, aided by north-east winds, brings immense ice-floes to the east coast in summer. During the winter, the Sea of Okhotsk turns to ice, rendering the northern coast impassable to marine traffic, and halting the lucrative fisheries there until the thaw.
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Peru is both afflicted and blessed by a peculiar climate due to the Humboldt Current. Before over fishing killed its fishery, Peru had the world's most productive fishery due to the cold Current. It lifts nutrients from the Pacific floor to surface waters. On land, it results in a cold mist that covers coastal Peru to the extent that desert plants have adapted to obtain water from the air instead of from (infrequent) rainfall.
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They continue to do so for some hours, eventually getting caught by a cold current. They wind up at a secret undersea research base, where they are rescued by military police. They learn that Rue was believed dead along with her cousin and Crisler and Mallory have already departed for the Envy, having learned its point of origin, Apophis and Osiris, planetless binary brown dwarfs. They expect that he will arrive in sixteen months.
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Gageodo, also known as Soheuksando due to its location near Heuksan-do, is an island in the Yellow Sea. It is within the administrative boundaries of Sinan County, Jeollanam-do, South Korea, and is connected by the Namhae Star ferry to the city of Mokpo. The island's 9.2 km² are home to about 470 people. Gageodo is meteorologically significant, due to its location near the southern limit of the Yellow Sea Cold Current.
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An expert swimmer, Lieutenant Das swam across about three fourths of the river. But when he was just nearing the other bank of the river, he got caught in an extremely cold current and started going down the river. The two signallers who had the other end of the cable in their hands tried to pull him out of the icy cold waters. But, due to the strong currents, the cable gave way.
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The East Korea Warm Current (동한난류, 東韓暖流) is an ocean current in the Sea of Japan (East Sea). It branches off from the Tsushima Current at the eastern end of the Korea Strait, and flows north along the southeastern coast of the Korean Peninsula. Between 36° and 38° N, it encounters the North Korea Cold Current and veers southeast into the open sea. The boundary between the two currents fluctuates throughout the year, creating large eddies.
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Mulegé is internationally famous for its rich fishing grounds in the Gulf of California. A warm current from the southern and a cold current from the northern Pacific come together in the Mulegé area of the Gulf of California and encourage a great variety of different fish species. The Gulf is sometimes known as the "Sea of Cortez", after the Spanish explorer, Hernán Cortés, who sailed into the area. In the past, Mulegé's economy was largely based on fishing and farming.
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The Falkland Current (also called Malvinas Current or Falklands Current) is a cold water current that flows northward along the Atlantic coast of Patagonia as far north as the mouth of the Río de la Plata. This current results from the movement of water from the West Wind Drift as it rounds Cape Horn. It takes its name from the Falkland Islands (). This cold current mixes with the tropical Brazil Current in the Argentine Sea (see Brazil–Falkland Confluence), giving it its temperate climate.
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The coasts of Kamchatka are relatively flat, and cooled by the cold current of the Sea of Okhotsk to the west, and the East Kamchatka Current that flows down the east coast on the Bering Sea side. The ecoregion includes the Kuril Islands down to Urap Island, the northernmost 800 km of islands that stretch down from the peninsula. The Commander Islands lie in the 175 km to the east of the middle of the peninsula in the Bering Sea. The area is volcanic, and the soils are Andosol (black volcanic).
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The North Korea Cold Current (NKCC) is a cold water oceanic current in the Sea of Japan (East Sea of Korea) that flows southward from near Vladivostok along the coastline of the eastern Korean Peninsula. It is a branch of the Liman Current from the Sea of Okhotsk and has a flow rate of about a half knot. The NKCC meets the northward flowing East Korean Warm Current at latitude 37–38° N, causing the flow to separate from the peninsula. At about latitude 40° N, the NKCC meets the Tsushima Warm Current.
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The North Icelandic Jet is a deep-reaching current that flows along the continental slope of Iceland. The North Icelandic Jet advects overflow water into the Denmark Strait and constitutes a pathway that is distinct from the East Greenland Current. It is a cold current that runs west across the top of Iceland, then southwest between Greenland and Iceland at a depth of about 600 metres (almost 2,000 feet). The North Icelandic Jet is deep and narrow (about 12 mile wide) and can carry more than a million cubic meters of water per second.
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Map of Labrador Current The Labrador Current is a cold current in the North Atlantic Ocean which flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Canada near Nova Scotia. Near Nova Scotia, this cold water current meets the warm northward moving Gulf Stream. The combination of these two currents produces heavy fogs and has also created one of the richest fishing grounds in the world. In spring and early summer, the Labrador Current transports icebergs from the glaciers of Greenland southwards into the trans-Atlantic shipping lanes.
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This cold current moderates the summer weather in the coastal valleys of Northern California. Lying between the Spring Mountain appellation and the cold ocean current is a gap in the coastal mountains between Bodega and Tomales Bay and extending through the Santa Rosa Plain. Summer heat in the interior of California creates a low pressure area that draws cold air from the coast through this coastal gap and across the broad Santa Rosa plain. This on-shore air movement is bumped north by Sonoma Mountain pushing the cold air flow towards Santa Rosa Creek, the Northern Mayacamas Mountains, and directly at the Spring Mountain District AVA.
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During summer, regions of Mediterranean climate are strongly influenced by the subtropical ridge which keeps atmospheric conditions very dry with minimal cloud coverage. In some areas, such as coastal California, the cold current has a stabilizing effect on the surrounding air, further reducing the chances for rain, but often causing thick layers of marine fog that usually evaporates by mid-day. Similar to desert climates, in many Mediterranean climates there is a strong diurnal character to daily temperatures in the warm summer months due to strong heating during the day from sunlight and rapid cooling at night. In winter, the subtropical ridge migrates towards the equator, making rainfall much more likely.
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View of Punta Arenas, Chile, in winter The overall climate is cool and dry. The east coast is warmer than the west, especially in summer, as a branch of the southern equatorial current reaches its shores, whereas the west coast is washed by a cold current. However, winters are colder on the inland plateaus east of the slopes and further down the coast on the southeast end of the Patagonian region. For example, at Puerto Montt, on the inlet behind Chiloé Island, the mean annual temperature is and the average extremes are , whereas at Bahía Blanca near the Atlantic coast and just outside the northern confines of Patagonia, the annual temperature is and the range much greater, as temperatures above 35°C and below −5°C are recorded every year.
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The Falkland Islands' fishing waters form part of the 2.7 million square kilometre Patagonian Shelf large marine ecosystem and are located on a spur from the Patagonian Continental Shelf. Most of the fishing takes place in water up to deep on this spur or on the Burdwood Bank - another spur lying on an undersea ridge to the south of the Falkland Islands and separated from the islands by a deep channel known as the Falklands Trough. At its highest point, the Burdwood Bank is below sea level. The principal ocean currents in the Falkland Island waters are the West Wind Drift, a cold current from the Southern Pacific Ocean that flows westwards to the south of the Burdwood Bank and the north flowing cold Falklands current, an offshoot of the West Wind Drift that curls around the east of Falklands Plateau and along the Falklands and Patagonian escarpments.
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