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1 расходоваться на
The greater part of its energy does not reach the surface of the Earth, it is expended in splitting the molecules and ionizing the upper layers of the atmosphere.Русско-английский словарь по космонавтике > расходоваться на
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2 расщепление молекул
The greater part of its energy does not reach the surface of the Earth, it is expended in splitting the molecules and ionizing the upper layers of the atmosphere.Русско-английский словарь по космонавтике > расщепление молекул
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3 слои атмосферы
[см. верхние слои земной атмосферы; входить в плотные слои атмосферы; нижние слои земной атмосферы; плотные слои атмосферы; после выхода ракеты из плотных слоев атмосферы; снижение в плотных слоях атмосферы]The greater part of its energy does not reach the surface of the Earth, it is expended in splitting the molecules and ionizing the upper layers of the atmosphere.…as the reentry compartment moves through dense atmosphere and induces the action of aerodynamic forces as a result of air resistance. -
4 днём и ночью
Русско-английский научно-технический словарь переводчика > днём и ночью
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5 днём и ночью
Русско-английский научно-технический словарь переводчика > днём и ночью
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6 верхние слои земной атмосферы
Русско-английский словарь по космонавтике > верхние слои земной атмосферы
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7 атмосферная инверсия
атмосферная инверсия
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric inversion
A temperature inversion in the atmosphere in which the temperature, instead of falling, increases with height above the ground. With the colder and heavier air below, there is no tendency to form upward currents and turbulence is suppressed. Inversions are often formed in the late afternoon when the radiation emitted from the ground exceeds that received from the sinking sun. Inversions are also caused by katabatic winds, that is cold winds flowing down the hillside into a valley, and by anticyclones. In inversion layers, both vertical and horizontal diffusion is inhibited and pollutants become trapped, sometimes for long periods. Low-level discharges of pollutants are more readily trapped by inversions than high level dischargers, hence the case for high stacks. Furthermore, high level discharges into an inversion tend to remain at a high level because of the absence of vertical mixing. (Source: GILP96)
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Русско-немецкий словарь нормативно-технической терминологии > атмосферная инверсия
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8 атмосферная инверсия
атмосферная инверсия
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric inversion
A temperature inversion in the atmosphere in which the temperature, instead of falling, increases with height above the ground. With the colder and heavier air below, there is no tendency to form upward currents and turbulence is suppressed. Inversions are often formed in the late afternoon when the radiation emitted from the ground exceeds that received from the sinking sun. Inversions are also caused by katabatic winds, that is cold winds flowing down the hillside into a valley, and by anticyclones. In inversion layers, both vertical and horizontal diffusion is inhibited and pollutants become trapped, sometimes for long periods. Low-level discharges of pollutants are more readily trapped by inversions than high level dischargers, hence the case for high stacks. Furthermore, high level discharges into an inversion tend to remain at a high level because of the absence of vertical mixing. (Source: GILP96)
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Русско-английский словарь нормативно-технической терминологии > атмосферная инверсия
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9 атмосферная инверсия
атмосферная инверсия
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric inversion
A temperature inversion in the atmosphere in which the temperature, instead of falling, increases with height above the ground. With the colder and heavier air below, there is no tendency to form upward currents and turbulence is suppressed. Inversions are often formed in the late afternoon when the radiation emitted from the ground exceeds that received from the sinking sun. Inversions are also caused by katabatic winds, that is cold winds flowing down the hillside into a valley, and by anticyclones. In inversion layers, both vertical and horizontal diffusion is inhibited and pollutants become trapped, sometimes for long periods. Low-level discharges of pollutants are more readily trapped by inversions than high level dischargers, hence the case for high stacks. Furthermore, high level discharges into an inversion tend to remain at a high level because of the absence of vertical mixing. (Source: GILP96)
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Русско-французский словарь нормативно-технической терминологии > атмосферная инверсия
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10 верхний
(в разн. знач.)upperверхние слои атмосферы — upper layers / strata of the atmosphere
верхнее течение Волги — the Upper Volga, the upper reaches of the Volga
верхнее платье — overcoat, outer clothing
верхний регистр муз. — highest register
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11 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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12 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. -
13 плотные слои атмосферы
[см. входить в плотные слои атмосферы; после выхода ракеты из плотных слоев атмосферы; снижение в плотных слоях атмосферы]…the aerodynamic loads decrease practically to zero when the rocket passes beyond the dense atmospheric layers.…as the reentry compartment moves through dense atmosphere…Русско-английский словарь по космонавтике > плотные слои атмосферы
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14 верхний
1) ( расположенный выше прочих) top; upperве́рхний эта́ж — upper / top floor
ве́рхний я́щик — top drawer
ве́рхние слои́ атмосфе́ры — upper layers / strata of the atmosphere
2) ( близкий к верховью реки) upper; up-riverве́рхнее тече́ние Во́лги — the Upper Volga, the upper reaches of the Volga
3) ( об одежде) outer; overве́рхняя оде́жда — overclothes, outer clothing
4) муз. highве́рхний реги́стр — highest register
••ве́рхняя пала́та (парламента) — upper chamber; ( в Великобритании) House of Lords
замо́к ве́рхнего реги́стра информ. — caps lock
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15 слои атмосферы
слои атмосферы
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric layering
Any one of a number of strata or layers of the earth's atmosphere; temperature distribution is the most common criterion used for denoting the various shell. Also known as atmospheric shell; atmospheric region. (Source: MGH)
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Русско-немецкий словарь нормативно-технической терминологии > слои атмосферы
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16 слои атмосферы
слои атмосферы
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric layering
Any one of a number of strata or layers of the earth's atmosphere; temperature distribution is the most common criterion used for denoting the various shell. Also known as atmospheric shell; atmospheric region. (Source: MGH)
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Русско-английский словарь нормативно-технической терминологии > слои атмосферы
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17 слои атмосферы
слои атмосферы
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric layering
Any one of a number of strata or layers of the earth's atmosphere; temperature distribution is the most common criterion used for denoting the various shell. Also known as atmospheric shell; atmospheric region. (Source: MGH)
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Русско-французский словарь нормативно-технической терминологии > слои атмосферы
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18 глубинные слои
Four Soviet automatic interplanetary stations entered the bottom layers of the Venusian atmosphere… -
19 опускаться
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