lmd_Dufresne2001.bib
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@article{2001GeoRL..28.1543F,
author = {{Friedlingstein}, P. and {Bopp}, L. and {Ciais}, P. and {Dufresne}, J.-L. and
{Fairhead}, L. and {LeTreut}, H. and {Monfray}, P. and {Orr}, J.
},
title = {{Positive feedback between future climate change and the carbon cycle}},
journal = {\grl},
keywords = {Atmospheric Composition and Structure: Biosphere/atmosphere interactions, Global Change, Oceanography: Biological and Chemical: Carbon cycling},
year = 2001,
volume = 28,
pages = {1543-1546},
abstract = {{Future climate change due to increased atmospheric CO$_{2}$ may
affect land and ocean efficiency to absorb atmospheric CO$_{2}$.
Here, using climate and carbon three-dimensional models forced by a 1\%
per year increase in atmospheric CO$_{2}$, we show that there is a
positive feedback between the climate system and the carbon cycle.
Climate change reduces land and ocean uptake of CO$_{2}$,
respectively by 54\% and 35\% at 4 {\times} CO$_{2}$. This negative
impact implies that for prescribed anthropogenic CO$_{2}$
emissions, the atmospheric CO$_{2}$ would be higher than the level
reached if climate change does not affect the carbon cycle. We estimate
the gain of this climate-carbon cycle feedback to be 10\% at 2 {\times}
CO$_{2}$ and 20\% at 4 {\times} CO$_{2}$. This translates into
a 15\% higher mean temperature increase.
}},
doi = {10.1029/2000GL012015},
adsurl = {http://adsabs.harvard.edu/abs/2001GeoRL..28.1543F},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
