In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 45, No. 1 ( 2018-01-16), p. 354-362
Kurzfassung:
The recent decrease in WNP TCs was driven by an intensification of vertical wind shear in the southeastern/eastern WNP The intensified vertical wind shear in the southeastern/eastern WNP arose primarily from the enhanced SST warming in the North Atlantic The SST anomalies in the tropical Pacific associated with the negative PDO and the anthropogenic forcing play only secondary roles
Materialart:
Online-Ressource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1002/2017GL076397
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2018
ZDB Id:
2021599-X
ZDB Id:
7403-2
SSG:
16,13
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