In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 126, No. 9 ( 2021-09)
Abstract:
Nino‐4W sea surface temperature (SST) variability, with high negative skewness, is a unique climate index in the western Pacific warm pool Zonal advective feedback, or advection due to anomalous zonal current, plays a key role in driving SST variability in Nino‐4W Strong negative feedback from air‐sea flux anomalies during the development of the warm events in Nino‐4W contributes to the SST skewness
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2021JC017591
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
SSG:
16,13
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