<?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>Extended winter Pacific North America oscillation as a precursor of the Indian summer monsoon rainfall</dc:title>
  <dc:creator>Peings, Y.</dc:creator>
  <dc:creator>Douville, H.</dc:creator>
  <dc:creator>/Terray, Pascal</dc:creator>
  <dc:description>In spite of considerable efforts, long-range forecasting of Indian summer monsoon rainfall (ISMR) is still a challenge for both statistical and dynamical tools. We highlight the winter-to-spring Pacific North America (PNA) oscillation as a predictor for the ISMR. A PNA-related index is proposed that is highly correlated with the following summer precipitation over India and is also a precursor of El Nino-Southern Oscillation (ENSO) events over recent decades. The PNA index compares well with other predictors used in operational statistical models for ISMR prediction. A multiple linear regression scheme is tested with a cross-validation hindcast approach and confirms the added value of our predictor, at least over the period 1958-2005. Nevertheless, the predictor shows less skill over the first half of the 20th century. Possible physical mechanisms of this teleconnection are also briefly discussed and could involve both a tropical Pacific sea surface temperature and Eurasian snow cover pathway. Citation: Peings, Y., H. Douville, and P. Terray (2009), Extended winter Pacific North America oscillation as a precursor of the Indian summer monsoon rainfall, Geophys. Res. Lett., 36, L11710, doi:10.1029/2009GL038453.</dc:description>
  <dc:date>2009</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/PAR00003585</dc:identifier>
  <dc:identifier>PAR00003585</dc:identifier>
  <dc:identifier>Peings Y., Douville H., Terray Pascal. Extended winter Pacific North America oscillation as a precursor of the Indian summer monsoon rainfall. 2009, 36, L11710</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
