In:
Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 90, No. 16 ( 2009-04-21), p. 140-140
Abstract:
Climate‐induced changes in the terrestrial biosphere and the ocean modulate the release and uptake of carbon dioxide (CO 2 ), and this, in turn, alters atmospheric composition and climate in a process called climate/carbon cycle feedback. The Coupled Carbon Cycle Climate Model Intercomparison Project (C4MIP), using models of the terrestrial and ocean carbon cycles in ocean‐atmosphere general circulation models, has shown that although the feedback is positive, its magnitude is highly uncertain (P. Friedlingstein et al., J. Clim. , 19, 3337, 2006). It is important to quantify this feedback adequately because it affects the CO 2 emissions consistent with any atmospheric CO 2 stabilization.
Type of Medium:
Online Resource
ISSN:
0096-3941
,
2324-9250
DOI:
10.1029/2009EO160004
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2009
detail.hit.zdb_id:
24845-9
detail.hit.zdb_id:
2118760-5
detail.hit.zdb_id:
240154-X
SSG:
16,13
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