ENSO prediction one year in advance using western North Pacific sea surface temperatures

We present evidence that the de‐trended, boreal winter sea surface temperature anomalies (SSTA) in the western North Pacific (WNP) are a skillful predictor for the development of the El Niño‐Southern Oscillation (ENSO) by the following winter. The WNP shares some similarities with the Meridional Mod...

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Bibliographic Details
Published inGeophysical research letters Vol. 39; no. 5
Main Authors Wang, Shih-Yu, L'Heureux, Michelle, Chia, Hsin-Hsing
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.03.2012
American Geophysical Union
John Wiley & Sons, Inc
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Summary:We present evidence that the de‐trended, boreal winter sea surface temperature anomalies (SSTA) in the western North Pacific (WNP) are a skillful predictor for the development of the El Niño‐Southern Oscillation (ENSO) by the following winter. The WNP shares some similarities with the Meridional Mode (MM) located in the subtropical central and eastern North Pacific: both are linked to off‐equatorial SSTA and low‐level wind anomalies, and both appear to be strongly related to wintertime variability in the North Pacific Oscillation (NPO). However, in contrast with the MM, the WNP is associated with an opposite‐signed SSTA dipole located off southeastern Asia and in the western tropical Pacific, which is accompanied by equatorial winds that may influence the level of oceanic Kelvin wave activity that precedes ENSO events. Key Points Identification of the western North Pacific (WNP) region for SSTA Winter SSTA in WNP is a skillful predictor for ENSO development WNP SSTA initiates equatorial winds that influence oceanic Kelvin waves
Bibliography:istex:42D894027173387B1F8842A4D9184F6B125CDB85
ark:/67375/WNG-02N71RTT-B
ArticleID:2012GL050909
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2012GL050909