<?xml version="1.0" encoding="UTF-8"?>
<xml>
  <records>
    <record>
      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
      <foreign-keys>
        <key app="Horizon" db-id="fdi:010066978">1</key>
      </foreign-keys>
      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Ibanhez, J. S. P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Araujo, M.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Lefèvre, Nathalie</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>The overlooked tropical oceanic CO2 sink</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>3804-3812</pages>
      <keywords>
        <keyword>ATLANTIQUE OUEST</keyword>
        <keyword>ZONE TROPICAL</keyword>
        <keyword>AMAZONE</keyword>
      </keywords>
      <dates>
        <year>2016</year>
      </dates>
      <call-num>fdi:010066978</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <accession-num>ISI:000378338800024</accession-num>
      <number>8</number>
      <electronic-resource-num>10.1002/2016gl068020</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010066978</url>
        </related-urls>
        <pdf-urls>
          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-03/010066978.pdf</url>
        </pdf-urls>
      </urls>
      <volume>43</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The intense rainfall in the tropical Atlantic spatially overlaps with the spread of the Amazon plume. Based on remote-sensed sea surface salinity and rainfall, we removed the contribution of rainfall to the apparent Amazon plume area, thus refining the quantification of its extension (0.84 +/- 0.06 x 10(6) km(2) to 0.89 +/- 0.06 x 10(6) km(2)). Despite the previous overestimation of the Amazon plume area due to the influence of rainfall (&gt;16%), our calculated annual CO2 flux based on rainfall-corrected sea surface CO2 fugacity confirms that the Amazon River plume is an atmospheric CO2 sink of global importance (-7.61 +/- 1.01 to -7.85 +/- 1.02 Tg C yr(-1)). Yet we show that current sea-air CO2 flux assessments for the tropical Atlantic could be overestimated in about 10% by neglecting the CO2 sink associated to the Amazon plume. Thus, including the Amazon plume, the sea-air CO2 exchange for the tropical Atlantic is estimated to be 81.1 +/- 1.1 to 81.5 +/- 1.1 Tg C yr(-1).</abstract>
      <custom6>032 ; 062</custom6>
      <custom1>UR182</custom1>
      <custom7>Brésil</custom7>
    </record>
  </records>
</xml>
