In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 46, No. 21 ( 2019-11-16), p. 12165-12172
Kurzfassung:
A dipole structure of mixed layer salinity in the western‐central equatorial Pacific is a characteristic of El Niño‐La Niña asymmetry Nonlinear zonal advection plays a dominant role in generating the dipole salinity structure The dipole salinity structure has potential effects on the asymmetry of ENSO SST
Materialart:
Online-Ressource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2019GL084817
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2019
ZDB Id:
2021599-X
ZDB Id:
7403-2
SSG:
16,13
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