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1 абсорбированная вода
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2 абсорбированная вода
Русско-английский словарь по нефти и газу > абсорбированная вода
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3 абсорбированная вода
Русско-английский научно-технический словарь Масловского > абсорбированная вода
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4 абсорбированная вода
Русско-английский политехнический словарь > абсорбированная вода
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5 абсорбированная вода
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6 абсорбционная вода
Русско-английский словарь по нефти и газу > абсорбционная вода
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7 абсорбированная вода
Универсальный русско-английский словарь > абсорбированная вода
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8 абсорбционная вода
Универсальный русско-английский словарь > абсорбционная вода
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9 поглощённая вода
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10 почти или полностью неподвижная вода в снежном покрове, включающая адсорбированную и плёночную воду
Универсальный русско-английский словарь > почти или полностью неподвижная вода в снежном покрове, включающая адсорбированную и плёночную воду
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11 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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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-английский словарь нормативно-технической терминологии > циркуляция морской воды
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13 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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14 гигроскопическая влага
1) Engineering: absorbed moisture, molecular moisture2) Construction: hydroscopic moisture, hygroscopic moisture, hygroscopic water3) Cement: equilibrium moisture, equilibrium water contentУниверсальный русско-английский словарь > гигроскопическая влага
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15 излишний
Русско-английский научно-технический словарь переводчика > излишний
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16 излишний
Русско-английский научно-технический словарь переводчика > излишний
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17 как уже говорилось
Как уже говорилосьThe absorbed energy, as stated previously, is calculated from measurements of the pit volume.In equations (...) and (...), m too is a function of y, as stated earlier.As discussed earlier, higher quench front velocity is due to larger water subcoolings.Their effect, as already discussed, is to introduce scatter into frequency response plots.As mentioned, this method is questionable for this mode because of the possible errors in frequency.Русско-английский научно-технический словарь переводчика > как уже говорилось
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18 нижние слои земной атмосферы
[ант. верхние слои земной атмосферы]Radiation in the region between the optical and radio windows is absorbed by water vapour in the lower layers of the Earth's atmosphere.Русско-английский словарь по космонавтике > нижние слои земной атмосферы
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19 пары воды
Radiation in the region between the optical and radio windows is absorbed by water vapour in the lower layers of the Earth's atmosphere. -
20 поглощать
vt; св - поглоти́ть1) вбирать в себя to absorb, to take inпоглоща́ть во́ду — to absorb water
поглоща́ть конце́рн — to take over/to swallow up a concern
поглоща́ть кни́гу за кни́гой — to devour one book after another
во́лны поглоти́ли су́дно — the sea engulfed the boat
3) увлекать to absorb, to engrossфильм поглоти́л всё его́ внима́ние — he was absorbed/engrossed in the film
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