<?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>Sea surface temperature and salinity seasonal changes in the western Solomon and Bismarck Seas</dc:title>
  <dc:creator>/Delcroix, Thierry</dc:creator>
  <dc:creator>/Radenac, Marie-H&#xE9;l&#xE8;ne</dc:creator>
  <dc:creator>/Cravatte, Sophie</dc:creator>
  <dc:creator>Alory, G.</dc:creator>
  <dc:creator>Gourdeau, L.</dc:creator>
  <dc:creator>L&#xE9;ger, F.</dc:creator>
  <dc:creator>Singh, A.</dc:creator>
  <dc:creator>/Varillon, David</dc:creator>
  <dc:subject>INTERACTION OCEAN ATMOSPHERE</dc:subject>
  <dc:subject>TEMPERATURE DE SURFACE</dc:subject>
  <dc:subject>SALINITE</dc:subject>
  <dc:subject>COURANT GEOSTROPHIQUE</dc:subject>
  <dc:subject>ADVECTION MARINE</dc:subject>
  <dc:subject>UPWELLING</dc:subject>
  <dc:subject>EL NINO</dc:subject>
  <dc:subject>PRECIPITATION</dc:subject>
  <dc:subject>VENT</dc:subject>
  <dc:subject>ESTUAIRE</dc:subject>
  <dc:subject>VARIATION MENSUELLE</dc:subject>
  <dc:subject>VARIATION SAISONNIERE</dc:subject>
  <dc:subject>VARIATION ANNUELLE</dc:subject>
  <dc:description>We analyze mean and seasonal change of Sea Surface Temperature (SST) and Salinity (SSS) in the Solomon and Bismarck Seas, using 1977-2009 in situ data collected from Voluntary Observing Ships. Covariability of these two variables with surface wind, altimeter-derived and model-derived horizontal currents, precipitation, and Sepik River discharge are examined. SST and SSS show large annual oscillations in the Solomon Sea, with the coldest and saltiest waters occurring in July/August mainly due to horizontal advection. In contrast, they show large semiannual oscillations in the Bismarck Sea. There, the coldest and saltiest waters happen in January/February, when the northwest monsoon winds drive coastal upwelling, and in July/August, when the New Guinea Coastal Current advects cold and high-salinity waters from the Solomon Sea through Vitiaz Strait. The low SSS values observed in April/May, stuck between the January/February and July/August SSS maxima, are further enhanced by the Sepik River discharge annual maximum. A high-resolution model strengthens the conclusions we derive from observations. The impacts of ENSO on SST and SSS are also discussed with, for instance, saltier-than-average and fresher-than-average waters during the 2002-2003 El Nino and 2007-2008 La Nina, respectively.</dc:description>
  <dc:date>2014</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010062177</dc:identifier>
  <dc:identifier>fdi:010062177</dc:identifier>
  <dc:identifier>Delcroix Thierry, Radenac Marie-H&#xE9;l&#xE8;ne, Cravatte Sophie, Alory G., Gourdeau L., L&#xE9;ger F., Singh A., Varillon David. Sea surface temperature and salinity seasonal changes in the western Solomon and Bismarck Seas. 2014, 119 (4),  2642-2657</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>PACIFIQUE</dc:coverage>
  <dc:coverage>SALOMON</dc:coverage>
  <dc:coverage>BISMARCK</dc:coverage>
  <dc:coverage>PAPOUASIE NOUVELLE GUINEE</dc:coverage>
</oai_dc:dc>
