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Depletion of the ozone layer
Destruction of the ozone layer
Deterioration of the ozone layer
Domestic economic equilibrium
Domestic equilibrium
Equilibrium concentration of ozone
Equilibrium cone of depression
Equilibrium cone of exhaustion
Equilibrium cone of influence
Equilibrium cone of pumping depression
Equilibrium ozone concentration
Internal economic equilibrium
Internal equilibrium
Steady-state concentration of ozone
Steady-state level of ozone
Steady-state ozone cocentration
Steady-state ozone level
Stratospheric pollution

Vertaling van "Ozone equilibrium " (Engels → Frans) :

TERMINOLOGIE
equilibrium concentration of ozone | equilibrium ozone concentration | steady-state concentration of ozone | steady-state level of ozone | steady-state ozone cocentration | steady-state ozone level

concentration de l'ozone à l'équilibre | concentration d'équilibre en ozone


equilibrium cone of depression | equilibrium cone of exhaustion | equilibrium cone of influence | equilibrium cone of pumping depression

cône d'appel d'équilibre


domestic economic equilibrium | domestic equilibrium | internal economic equilibrium | internal equilibrium

équilibre économique interne | équilibre interne


stratospheric pollution [ depletion of the ozone layer | destruction of the ozone layer | deterioration of the ozone layer ]

pollution stratosphérique [ dégradation de la couche d'ozone | destruction de la couche d'ozone | détérioration de la couche d'ozone | réduction de la couche d'ozone ]


Due to the observed increase in atmospheric CO2 (*), produced mainly by fossil-fuel burning, since the beginning of the industrial era, and due to the increase in the atmospheric concentration of other trace gases (methane, nitrous oxide, the chlorofluorocarbons, tropospheric ozone), the global equilibrium mean surface temperature is likely to increase by 1.5-5.5 C when the CO2 concentration has reached the double of its pre-industrial value (sometime in the course of the next century).

En raison de l'augmentation observee du C02(*) dans l'atmosphere, produit principalement par l'utilisation de combustibles fossiles, depuis le debut de l'ere industrielle, et en raison de l'augmentation de la concentration dans l'atmosphere d'autres gaz en traces (methane, oxyde d'azote, chlorofluorocarbones, ozone de la troposphere), la temperature moyenne d'equilibre a la surface du globe augmentera probablement de 1,5 a 5,5 C, lorsque la concentration de C02 aura atteint le double de sa valeur preindustrielle (au cours du siecle pr ...[+++]


Due to the observed increase in atmospheric CO2 (*), produced mainly by fossil-fuel burning, since the beginning of the industrial era, and due to the increase in the atmospheric concentration of other trace gases (methane, nitrous oxide, the chlorofluorocarbons, tropospheric ozone), the global equilibrium mean surface temperature is likely to increase by 1.5-5.5 C when the CO2 concentration has reached the double of its pre-industrial value (sometime in the course of the next century).

En raison de l'augmentation observee du C02(*) dans l'atmosphere, produit principalement par l'utilisation de combustibles fossiles, depuis le debut de l'ere industrielle, et en raison de l'augmentation de la concentration dans l'atmosphere d'autres gaz en traces (methane, oxyde d'azote, chlorofluorocarbones, ozone de la troposphere), la temperature moyenne d'equilibre a la surface du globe augmentera probablement de 1,5 a 5,5 C, lorsque la concentration de C02 aura atteint le double de sa valeur preindustrielle (au cours du siecle pr ...[+++]


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