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1 климатический цикл
1) Geology: climatic cycle (напр. период Брюкнера)2) Agriculture: climatic cycle (цикл повторяемости засушливых и влажных лет)3) Ecology: climate cycle4) Makarov: climatic cycle (напр., период Брюкнера)5) General subject: climatic cwmУниверсальный русско-английский словарь > климатический цикл
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2 приобретать ... значение
Приобретать (большое) значениеEnvironment considerations relating to storage have assumed major importance particularly in light of today's economic and regulatory climate.The combined cycle process may make a significant impact in the next decade as an efficient, clean, cost effective producer of large quantities of electricity.Русско-английский научно-технический словарь переводчика > приобретать ... значение
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3 конъюнктура
сущ.( создавшееся положение) situation;state of affairs; экон. business climate (conditions); business (trade) cycle; conditions; conjuncture; economic trend; situation; state of the market- конъюнктура рынка
- деловая конъюнктура
- кредитная конъюнктура
- международная конъюнктура
- общехозяйственная конъюнктура
- рыночная конъюнктура
- экономическая конъюнктуравлиять на рыночную \конъюнктурау — to influence (manipulate) the market
изучать \конъюнктурау рынка — to study market conditions
изучение \конъюнктураы — marketing research
колебания \конъюнктураы — fluctuations of business (of the market)
оживление (подъём) \конъюнктураы — business revival; economic boom; cyclical upswing
спад (понижение) \конъюнктураы — downward business trend; slowing down of economic activity
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4 конъюнктура
сущ.( создавшееся положение) situation; state of affairs; экон business climate (conditions); business (trade) cycle; conditions; conjuncture; economic trend; situation; state of the marketоживление (подъём) конъюнктуры — business revival; economic boom; cyclical upswing
- деловая конъюнктураспад (понижение) конъюнктуры — downward business trend; slowing down of economic activity
- кредитная конъюнктура
- международная конъюнктура
- неустойчивая конъюнктура рынка
- общехозяйственная конъюнктура
- рыночная конъюнктура
- экономическая конъюнктура -
5 прогноз конъюнктуры
1. business forecastingспад конъюнктуры; деловой спад — business contractions
2. business cycle forecastРусско-английский большой базовый словарь > прогноз конъюнктуры
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6 сезонная миграция
сезонная миграция
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
seasonal migration
The periodic movement of a population from one region or climate to another in accordance with the yearly cycle of weather and temperature changes. (Source: RHW)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > сезонная миграция
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7 циркуляция морской воды
циркуляция морской воды
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > циркуляция морской воды
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8 сезонная миграция
сезонная миграция
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
seasonal migration
The periodic movement of a population from one region or climate to another in accordance with the yearly cycle of weather and temperature changes. (Source: RHW)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > сезонная миграция
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9 циркуляция морской воды
циркуляция морской воды
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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10 сезонная миграция
сезонная миграция
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
seasonal migration
The periodic movement of a population from one region or climate to another in accordance with the yearly cycle of weather and temperature changes. (Source: RHW)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > сезонная миграция
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11 циркуляция морской воды
циркуляция морской воды
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > циркуляция морской воды
См. также в других словарях:
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