Abstract
GEOPHYSICAL RESEARCH LETTERS,
VOL. 29,
1405,
4 PP., 2002
doi:10.1029/2001GL013777
On the magnitude of positive feedback between future climate change and the carbon cycle
IPSL/LMD, Paris, France
IPSL/LMD, Paris, France
IPSL/LMD, Paris, France
IPSL/LSCE, Gif sur Yvette, France
IPSL/LSCE, Gif sur Yvette, France
IPSL/LSCE, Gif sur Yvette, France
IPSL/LSCE, Gif sur Yvette, France
IPSL/LSCE, Gif sur Yvette, France
We use an ocean-atmosphere general circulation model coupled to land and ocean carbon models to simulate the evolution of
climate and atmospheric CO2 from 1860 to 2100. Our model reproduces the observed global mean temperature changes and the growth rate of atmospheric CO2 for the period 1860–2000. For the future, we simulate that the climate change due to CO2 increase will reduce the land carbon uptake, leaving a larger fraction of anthropogenic CO2 in the atmosphere. By 2100, we estimate that atmospheric CO2 will be 18% higher due to the climate change impact on the carbon cycle. Such a positive feedback has also been found by
Published 23 May 2002.
Citation: (2002), On the magnitude of positive feedback between future climate change and the carbon cycle, Geophys. Res. Lett., 29(10), 1405, doi:10.1029/2001GL013777.
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