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1 inversion thermique
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Франко-русский словарь нормативно-технической терминологии > inversion thermique
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2 inversion thermique
inversion of temperature; temperature inversionDictionnaire français-anglais de géographie > inversion thermique
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3 inversion thermique
инверсия температуры; температурная инверсияDictionnaire français-russe de géographie > inversion thermique
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4 inversion thermique
Dictionnaire français-allemand de géographie > inversion thermique
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5 inversión de temperatura
inversion de température; inversion thermiqueDictionnaire anglais-français de géographie > inversión de temperatura
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6 inversion of temperature
inversion de température; inversion thermiqueEnglish-French dictionary of Geography > inversion of temperature
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7 thermique
massive vein ice; massive wedge ice* -
8 thermique
повторножильный лед; полигонально-жильный лед* -
9 thermique
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10 temperature inversion
inversion de température; inversion thermiqueEnglish-French dictionary of Geography > temperature inversion
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11 atmosphärische Inversion
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Немецко-русский словарь нормативно-технической терминологии > atmosphärische Inversion
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12 atmospheric inversion
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Англо-русский словарь нормативно-технической терминологии > atmospheric inversion
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13 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)
[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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14 Temperaturinversion
inversion de température; inversion thermiqueDeutsch-Französisch Wörterbuch für Geographie > Temperaturinversion
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15 инверсия температуры
inversion de température; inversion thermiqueРусско-французский географический словарь > инверсия температуры
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16 температурная инверсия
inversion de température; inversion thermiqueРусско-французский географический словарь > температурная инверсия
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17 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)
[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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18 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)
[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 sol
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20 sol
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См. также в других словарях:
Inversion de température ou inversion thermique — ● Inversion de température ou inversion thermique température plus élevée en altitude qu au sol, phénomène relativement fréquent au dessus d un sol très froid, en hiver, notamment dans les vallées de montagne … Encyclopédie Universelle
Inversion thermique — Couche d inversion Nuages piégés sous une couche d inversion, dans le Puy de Dôme Une couche d inversion est une couche d air dont le gradient de température est positif, c est à dire que celle ci croît avec l altitude. En effet, dans la… … Wikipédia en Français
inversion — [ ɛ̃vɛrsjɔ̃ ] n. f. • 1529; lat. inversio, de invertere « retourner » I ♦ A ♦ Sens spéciaux 1 ♦ Déplacement (d un mot ou d un groupe de mots) par rapport à l ordre normal ou habituel de la construction. Inversion du sujet dans l interrogation (ex … Encyclopédie Universelle
THERMIQUE — La thermique est la branche de la physique qui traite des échanges de chaleur accompagnés ou non d’échange de masse et de changement de phases. Elle peut donc être considérée comme partie intégrante de la thermodynamique des phénomènes… … Encyclopédie Universelle
Inversion de température — Couche d inversion Nuages piégés sous une couche d inversion, dans le Puy de Dôme Une couche d inversion est une couche d air dont le gradient de température est positif, c est à dire que celle ci croît avec l altitude. En effet, dans la… … Wikipédia en Français
Couche d'inversion — Une couche d inversion est une couche d air dont le gradient de température est positif, c est à dire que celle ci croît avec l altitude. En effet, dans la troposphère la température de l air diminue normalement avec l altitude, d environ… … Wikipédia en Français
Gradient Thermique Adiabatique — Le gradient thermique adiabatique est, dans l atmosphère terrestre, la variation de température de l air avec l altitude (autrement dit le gradient de la température de l air), qui ne dépend que de la pression atmosphérique, c est à dire :… … Wikipédia en Français
Gradient thermique adiabatique — Le gradient thermique adiabatique est, dans l atmosphère terrestre, la variation de température de l air avec l altitude (autrement dit le gradient de la température de l air), qui ne dépend que de la pression atmosphérique, c est à dire :… … Wikipédia en Français
Couche D'inversion — Nuages piégés sous une couche d inversion, dans le Puy de Dôme Une couche d inversion est une couche d air dont le gradient de température est positif, c est à dire que celle ci croît avec l altitude. En effet, dans la troposphère la température… … Wikipédia en Français
Amplitude Thermique — On appelle amplitude thermique l écart entre la température minimale et maximale en un même lieu pendant une durée de temps déterminé. Le record mondial d amplitude thermique annuelle est de 104,4 °C, mesuré à Verkhoïansk, en Sibérie… … Wikipédia en Français
Amplitude thermique — On appelle amplitude thermique l écart entre la température minimale et maximale en un même lieu pendant une durée de temps déterminée. Le record mondial d amplitude thermique annuelle est de 104,4 °C, mesuré à Verkhoïansk, en Sibérie… … Wikipédia en Français