<?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>Revisiting atmospheric dust export to the Southern Hemisphere ocean : biogeochemical implications - art. no. GB2006</dc:title>
  <dc:creator>Wagener, T.</dc:creator>
  <dc:creator>Guieu, C.</dc:creator>
  <dc:creator>Losno, R.</dc:creator>
  <dc:creator>/Bonnet, Sophie</dc:creator>
  <dc:creator>/Mahowald, Nathalie</dc:creator>
  <dc:description>Aerosol concentrations in the Southern Hemisphere are largely undersampled. This study presents a chemical and physical description of dust particles collected on board research vessels in the southeast Pacific (SEPS) and the Southern Ocean (SOKS). Concentrations of dust were 6.1 +/- 2.4 ng m(-3) for SEPS and 13.0 +/- 6.3 ng m(-3) for SOKS. Dust fluxes, derived from those concentrations, were 9.9 +/- 3.7 mg m(-2) d(-1) for SEPS and 38 +/- 14 mg m(-2) d(-1) for SOKS and are shown to be representative of actual fluxes in those areas. Dust and iron deposition are up to 2 orders of magnitude lower than former predictions. A map of dust deposition on the Southern Hemisphere is proposed by incorporating those in situ measurements into a dust model. This study confirms that dust deposition is not the dominant source of iron to the large high-nutrient low-chlorophyll Southern Ocean.</dc:description>
  <dc:date>2008</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/PAR00002400</dc:identifier>
  <dc:identifier>PAR00002400</dc:identifier>
  <dc:identifier>Wagener T., Guieu C., Losno R., Bonnet Sophie, Mahowald Nathalie. Revisiting atmospheric dust export to the Southern Hemisphere ocean : biogeochemical implications - art. no. GB2006. 2008, 22 (2),  NIL_1-NIL_13</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
