In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 45, No. 22 ( 2018-11-28)
Kurzfassung:
The onset of Neoglaciation is regional and driven by nonlinear increases in regional cooling Model simulations suggest that cooling onsets are linked to Atlantic Meridional Overturning Circulation Observed and simulated rates of late Holocene cooling in the Arctic are remarkably similar
Materialart:
Online-Ressource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2018GL079773
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2018
ZDB Id:
2021599-X
ZDB Id:
7403-2
SSG:
16,13