Vous avez cherché: does rising temperature increase humidity (Espagnol - Anglais)

there was a temperature increase.
there was a temperature increase.

the result is a predicted temperature increase of 3 °c.
the result is a predicted temperature increase of 3 °c.

could that be a cause of the global temperature increase?
could that be a cause of the global temperature increase?

neglecting other forcings and considering the temperature increase to be an equilibrium increase would lead to a sensitivity of about 1.1 °c.
neglecting other forcings and considering the temperature increase to be an equilibrium increase would lead to a sensitivity of about 1.1 °c.

it is not easy to calculate these effects, but the general consensus is that, overall, they magnify the temperature increase by about a factor of 3."
it is not easy to calculate these effects, but the general consensus is that, overall, they magnify the temperature increase by about a factor of 3."

at high enough mach numbers the temperature increases so much over the shock that ionization and dissociation of gas molecules behind the shock wave begin.
at high enough mach numbers the temperature increases so much over the shock that ionization and dissociation of gas molecules behind the shock wave begin.

analysis of carbon isotopes in atmospheric co2 shows that the recent observed co2 increase cannot have come from the oceans, volcanoes, or the biosphere, and thus is not a response to rising temperatures as would be required if the same processes creating past lags were active now.
analysis of carbon isotopes in atmospheric shows that the recent observed increase cannot have come from the oceans, volcanoes, or the biosphere, and thus is not a response to rising temperatures as would be required if the same processes creating past lags were active now.

the global temperature increase since the beginning of the industrial period (taken as 1750) is about 0.8 °c, and the radiative forcing due to co2 and other long-lived greenhouse gases (mainly methane, nitrous oxide, and chlorofluorocarbons) emitted since that time is about 2.6 w/m2.
the global temperature increase since the beginning of the industrial period (taken as 1750) is about 0.8 °c, and the radiative forcing due to and other long-lived greenhouse gases (mainly methane, nitrous oxide, and chlorofluorocarbons) emitted since that time is about 2.6 w/m2.