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1 ледяной покров
2) American: glaze3) Engineering: ice cover, sheet ice (на поверхности водоёма)4) Agriculture: ice sheet (на водоёме)5) Construction: floe7) Sakhalin energy glossary: sheet ice8) Makarov: ice cover (ледяные образования, покрывающие полностью или частично поверхность моря, реки, озера), ice layer, sheet ice (на поверхности водоёмов)9) General subject: ice shape (на водоёме), sheet ice (на поверхности водоёма) -
2 ледяной щит
1) General subject: ice sheet2) Marine science: ice foot (у подножья ледника) -
3 Антарктический ледниковый покров
General subject: Antarctic ice shape, Antarctic inlandsisУниверсальный русско-английский словарь > Антарктический ледниковый покров
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4 горный ледяной покров
General subject: mountain ice shapeУниверсальный русско-английский словарь > горный ледяной покров
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5 ледяной покров, образующийся в результате нарастания льда от берегов
General subject: accretional ice shapeУниверсальный русско-английский словарь > ледяной покров, образующийся в результате нарастания льда от берегов
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6 ледяной покров, образующийся в результате смерзания отдельных льдин
General subject: abrasional ice shapeУниверсальный русско-английский словарь > ледяной покров, образующийся в результате смерзания отдельных льдин
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7 ледяной покров, образующийся в результате смерзания отдельных льдин и снега
General subject: agglomeritic ice shapeУниверсальный русско-английский словарь > ледяной покров, образующийся в результате смерзания отдельных льдин и снега
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8 покровный лёд
General subject: ice shape -
9 покровный лед
General subject: ice shape -
10 форма льда
Aviation: ice shape -
11 сплошной ледяной покров
1) Ice formation: ice sheet2) General subject: continuous shape of ice, solid ice coverУниверсальный русско-английский словарь > сплошной ледяной покров
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12 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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13 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-английский словарь нормативно-технической терминологии > циркуляция морской воды
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14 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
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15 особенности строения ледяной породы, обусловленные формой, размерами и ориентировкой кристаллов льда
Универсальный русско-английский словарь > особенности строения ледяной породы, обусловленные формой, размерами и ориентировкой кристаллов льда
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16 принимать форму
•Such glaciers are shaped into long, narrow ice streams.
•In a certain range of Reynolds numbers, the wake arranges itself into a double row of vortices.
•The variation may take the form (or shape) of amplitude modulation.
•The airship tail surfaces have taken on three typical configurations (or forms).
Русско-английский научно-технический словарь переводчика > принимать форму
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17 класс наземных ледников, форма которых не зависит от рельефа земной поверхности, а обусловлена распределением пита
General subject: inland glaciers not confined by the underlying topography, their shape determined by the distribution of nourishment and ice dischargeУниверсальный русско-английский словарь > класс наземных ледников, форма которых не зависит от рельефа земной поверхности, а обусловлена распределением пита
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18 министерство иностранных дел
1. oreign fficeкопия, остающаяся в делах — office copy
2. oreign inistryФорин оффис, Министерство иностранных дел — Foreign Office
3. State Department4. the Foreign Officeпомочь делу — to mend the matter, to mend matters
5. ministry of foreign affairs6. Ministry of Foreign Affairs; State Department; Foreign OfficeРусско-английский большой базовый словарь > министерство иностранных дел
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19 отливать в форму
1. injected into the mould2. inject into the mould
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