In:
Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 90, No. 16 ( 2009-04-21), p. 140-140
Kurzfassung:
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.
Materialart:
Online-Ressource
ISSN:
0096-3941
,
2324-9250
DOI:
10.1029/2009EO160004
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2009
ZDB Id:
24845-9
ZDB Id:
2118760-5
ZDB Id:
240154-X
SSG:
16,13
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