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1 atmospheric diffusion measuring system
Engineering: ADMSУниверсальный русско-английский словарь > atmospheric diffusion measuring system
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2 Atmospheric Turbulence and Diffusion Division
Oceanography: ATDDУниверсальный русско-английский словарь > Atmospheric Turbulence and Diffusion Division
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3 атмосферная диффузия
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4 атмосферная диффузия
Русско-английский исловарь по машиностроению и автоматизации производства > атмосферная диффузия
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5 атмосферное рассеяние
Русско-английский авиационный словарь > атмосферное рассеяние
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6 атмосферное рассеяние
Русско-английский аэрокосмический словарь > атмосферное рассеяние
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7 атмосферное рассеяние
Авиация и космонавтика. Русско-английский словарь > атмосферное рассеяние
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8 атмосферная диффузия
атмосферная диффузия
Ндп. вихревая диффузия
Неупорядоченное перемещение воздуха с находящимися в нем примесями, обусловленное турбулентностью атмосферы
[ ГОСТ 17.2.1.04-77]Недопустимые, нерекомендуемые
Тематики
EN
DE
FR
Ндп. Вихревая диффузия
D. Atmospharische Diffusion
Е. Atmospheric diffusion
F. Diffusion atmospherique
Неупорядоченное перемещение воздуха с находящимися в нем примесями, обусловленное турбулентностью атмосферы
Источник: ГОСТ 17.2.1.04-77: Охрана природы. Атмосфера. Источники и метеорологические факторы загрязнения, промышленные выбросы. Термины и определения оригинал документа
Русско-французский словарь нормативно-технической терминологии > атмосферная диффузия
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9 атмосферная диффузия
атмосферная диффузия
Ндп. вихревая диффузия
Неупорядоченное перемещение воздуха с находящимися в нем примесями, обусловленное турбулентностью атмосферы
[ ГОСТ 17.2.1.04-77]Недопустимые, нерекомендуемые
Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > атмосферная диффузия
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10 коэффициент атмосферной диффузии
Русско-английский научный словарь > коэффициент атмосферной диффузии
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11 коэффициент атмосферного рассеяния
Русско-английский физический словарь > коэффициент атмосферного рассеяния
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12 атмосферная диффузия
атмосферная диффузия
Ндп. вихревая диффузия
Неупорядоченное перемещение воздуха с находящимися в нем примесями, обусловленное турбулентностью атмосферы
[ ГОСТ 17.2.1.04-77]Недопустимые, нерекомендуемые
Тематики
EN
DE
FR
Ндп. Вихревая диффузия
D. Atmospharische Diffusion
Е. Atmospheric diffusion
F. Diffusion atmospherique
Неупорядоченное перемещение воздуха с находящимися в нем примесями, обусловленное турбулентностью атмосферы
Источник: ГОСТ 17.2.1.04-77: Охрана природы. Атмосфера. Источники и метеорологические факторы загрязнения, промышленные выбросы. Термины и определения оригинал документа
Русско-немецкий словарь нормативно-технической терминологии > атмосферная диффузия
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13 атмосферная диффузия
Ecology: atmospheric diffusionУниверсальный русско-английский словарь > атмосферная диффузия
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14 диффузия в атмосфере
Makarov: atmospheric diffusionУниверсальный русско-английский словарь > диффузия в атмосфере
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15 коэффициент атмосферного рассеяния
Makarov: atmospheric diffusion coefficientУниверсальный русско-английский словарь > коэффициент атмосферного рассеяния
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16 коэффициент атмосферной диффузии
Makarov: atmospheric diffusion coefficientУниверсальный русско-английский словарь > коэффициент атмосферной диффузии
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17 система измерения атмосферной диффузии
Engineering: atmospheric diffusion measuring systemУниверсальный русско-английский словарь > система измерения атмосферной диффузии
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18 атмосферная инверсия
атмосферная инверсия
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > атмосферная инверсия
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19 атмосферная инверсия
атмосферная инверсия
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > атмосферная инверсия
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20 атмосферная инверсия
атмосферная инверсия
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > атмосферная инверсия
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