In:
Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 84, No. 21 ( 2003-05-27), p. 197-201
Kurzfassung:
Recent measurements and model studies have consistently identified a decreasing trend in the concentration of dissolved O 2 in the ocean over the last several decades. This trend has important implications for our understanding of anthropogenic climate change. First, the observed oceanic oxygen changes may be a signal of the beginning of a reorganization of large‐scale ocean circulation in response to anthropogenic radiative forcing. Second, the repartitioning of oxygen between the ocean and the atmosphere requires a revision of the current atmospheric carbon budget and the estimates of the terrestrial and oceanic carbon sinks as calculated by the Intergovernmental Panel on Climate Change (IPCC) from measurements of atmospheric O 2 /N 2 .
Materialart:
Online-Ressource
ISSN:
0096-3941
,
2324-9250
DOI:
10.1029/2003EO210001
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2003
ZDB Id:
24845-9
ZDB Id:
2118760-5
ZDB Id:
240154-X
SSG:
16,13
Permalink