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Cited by 342

The DOI matches its Crossref record; 40 of the 40 references it cites were found in a registry or an index.

Interactive Feedback between ENSO and the Indian Ocean

Kug, Jong-Seong, Kang, In-Sik·2006·Journal of Climate
DOI 10.1175/jcli3660.1
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Abstract

A feedback process of the Indian Ocean SST on ENSO is investigated by using observed data and atmospheric GCM. It is suggested that warming in the Indian Ocean produces an easterly wind stress anomaly over Indonesia and the western edge of the Pacific during the mature phase of El Niño. The anomalous easterly wind in the western Pacific during El Niño helps a rapid termination of El Niño and a fast transition to La Niña by generating upwelling Kelvin waves. Thus, warming in the Indian Ocean, which is a part of the El Niño signal, operates as a negative feedback mechanism to ENSO. This Indian Ocean feedback appears to operate mostly for relatively strong El Niños and results in a La Niña one year after the mature phase of the El Niño. This 1-yr period of phase transition implies a possible role of Indian Ocean–ENSO coupling in the biennial tendency of the ENSO. Atmospheric GCM experiments show that Indian Ocean SST forcing is mostly responsible for the easterly wind anomalies in the western Pacific.

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Metadata

Authors
Kug, J.-S., & Kang, I.-S.
Venue
Journal of Climate
Publisher
American Meteorological Society
Published
2006-05-01
Volume
19
Issue
9
Pages
1784-1801
ISSN
  • 0894-8755 (ISSN-L)
  • 1520-0442
DOI
10.1175/jcli3660.1
OpenAlex
W2003237794
Cited by
342
References
40
FWCI
10.95
Type
journal article
Language
en
Open access
closed

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