Policy intervention figure Atmospheric composition and climate: Difference between revisions
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|AltText=Greenhouse gas emissions, CO2 concentration levels, radiative forcing and temperature increase under a baseline and three climate policy scenarios | |AltText=Greenhouse gas emissions, CO2 concentration levels, radiative forcing and temperature increase under a baseline and three climate policy scenarios | ||
|Caption=Greenhouse gas emissions, CO2 concentration levels, radiative forcing, and temperature increase under a baseline and three climate policy scenarios (based on Van Vuuren et al. 2010). | |Caption=Greenhouse gas emissions, CO2 concentration levels, radiative forcing, and temperature increase under a baseline and three climate policy scenarios (based on Van Vuuren et al. 2010). | ||
Revision as of 18:29, 20 May 2014
Caption: Greenhouse gas emissions, CO2 concentration levels, radiative forcing, and temperature increase under a baseline and three climate policy scenarios (based on Van Vuuren et al. 2010). In the policy scenarios, emissions decrease strongly after 2020, while concentration levels only decrease or stabilise after 2050. Global mean temperature is, due to inertia in the global mean temperature, only stabilising at the end of the century in the most ambitious climate policy scenario (2.6 W/m2).
Figure is used on page(s): Atmospheric composition and climate
