In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 126, No. 12 ( 2021-12)
Kurzfassung:
The transient climate response in two coupled models with the same atmosphere but different ocean components differs by 20% The upper (deeper) ocean heats faster (slower) in AWI‐CM compared to MPI‐ESM, independent of model resolution Vertical mixing in the northern North Atlantic and the Weddell and Ross Gyres appears to be key for these differences
Materialart:
Online-Ressource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2021JC017633
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
2016804-4
ZDB Id:
161667-5
ZDB Id:
3094219-6
SSG:
16,13