In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 45, No. 5 ( 2018-03-16), p. 2467-2475
Abstract:
Change in ENSO variability during the last 6,000 years is mainly induced by an orbital forcing only without invoking other climate forcing The zonal and meridional gradients of mean tropical SST were gradually reduced during the last 6,000 years ago The horizontal thermal advections associated with mean SST gradient are critical in modifying ENSO activity for the last 6,000 years
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1002/2017GL076250
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13
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