<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Extratropical forcing of ENSO</dc:title>
  <dc:creator>Boschat, G.</dc:creator>
  <dc:creator>/Terray, Pascal</dc:creator>
  <dc:creator>Masson, S.</dc:creator>
  <dc:subject>El Nino Southern Oscillation</dc:subject>
  <dc:subject>ENSO predictability</dc:subject>
  <dc:subject>singular value</dc:subject>
  <dc:subject>decomposition</dc:subject>
  <dc:description>We present evidence that sea surface temperatures in the North Pacific, South Atlantic, and South Indian Oceans during late boreal winter offer another important source of predictability for El Nino Southern Oscillation (ENSO). This new SST predictor may provide accurate prediction of the amplitude of ENSO events before their onset, for both El Nino and La Nina events which occurred during recent decades.</dc:description>
  <dc:date>2013</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010060369</dc:identifier>
  <dc:identifier>fdi:010060369</dc:identifier>
  <dc:identifier>Boschat G., Terray Pascal, Masson S.. Extratropical forcing of ENSO. 2013, 40 (8),  1605-1611</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>PACIFIQUE NORD</dc:coverage>
  <dc:coverage>ATLANTIQUE SUD</dc:coverage>
  <dc:coverage>OCEAN INDIEN</dc:coverage>
</oai_dc:dc>
