Baseline figure Atmospheric composition and climate: Difference between revisions

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{{FigureTemplate
{{FigureTemplate
|Figure=047x img13.png
|Figure=091x img13.png
|AltText=Global agricultural production and areas per region
|AltText=Greenhouse gas emissions, CO<sub>2</sub> concentration, temperature increase and radiative forcing under baseline and climate policy scenarios
|Caption=Production of animal and crop products (top) and cropland and grassland areas (bottom) in 2000 and in 2030 according to an implementation of FAO projections (Bruinsma 2003) in IMAGE, and according to IMPACT and MAGNET projections (Stehfest et al. 2013).
|Caption=In the policy scenarios, emissions decrease strongly after 2020, while concentration levels only decrease or stabilise after 2050. Global mean temperature, due to inertia in the climate system, will not stabilise until the end of this century under the most ambitious climate policy scenario (2.6 W/m<sup>2</sup>).
|FigureType=Baseline figure
|FigureType=Baseline figure
|OptimalSize=500
|OptimalSize=600
|Component=Agricultural economy and forestry;
|Component=Atmospheric composition and climate;
}}
}}

Latest revision as of 09:41, 1 July 2014


Greenhouse gas emissions, CO2 concentration, temperature increase and radiative forcing under baseline and climate policy scenarios

Caption: In the policy scenarios, emissions decrease strongly after 2020, while concentration levels only decrease or stabilise after 2050. Global mean temperature, due to inertia in the climate system, will not stabilise until the end of this century under the most ambitious climate policy scenario (2.6 W/m2).

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