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      <rec-number>1</rec-number>
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        <key app="Horizon" db-id="fdi:010080903">1</key>
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      <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%">Auger, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Morrow, R.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Kestenare, Elodie</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Sallee, J. B.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Cowley, R.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Southern Ocean in-situ temperature trends over 25 years emerge from interannual variability</title>
        <secondary-title>Nature Communications</secondary-title>
      </titles>
      <pages>514 [9 p.]</pages>
      <keywords>
        <keyword>OCEAN AUSTRAL</keyword>
      </keywords>
      <dates>
        <year>2021</year>
      </dates>
      <call-num>fdi:010080903</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Nature Communications</full-title>
      </periodical>
      <isbn>2041-1723</isbn>
      <accession-num>ISI:000613043600008</accession-num>
      <number>1</number>
      <electronic-resource-num>10.1038/s41467-020-20781-1</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010080903</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers21-02/010080903.pdf</url>
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      </urls>
      <volume>12</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Despite playing a major role in global ocean heat storage, the Southern Ocean remains the most sparsely measured region of the global ocean. Here, a unique 25-year temperature time-series of the upper 800m, repeated several times a year across the Southern Ocean, allows us to document the long-term change within water-masses and how it compares to the interannual variability. Three regions stand out as having strong trends that dominate over interannual variability: warming of the subantarctic waters (0.290.09 degrees C per decade); cooling of the near-surface subpolar waters (-0.07 +/- 0.04 degrees C per decade); and warming of the subsurface subpolar deep waters (0.04 +/- 0.01 degrees C per decade). Although this subsurface warming of subpolar deep waters is small, it is the most robust long-term trend of our section, being in a region with weak interannual variability. This robust warming is associated with a large shoaling of the maximum temperature core in the subpolar deep water (39 +/- 09m per decade), which has been significantly underestimated by a factor of 3 to 10 in past studies. We find temperature changes of comparable magnitude to those reported in Amundsen-Bellingshausen Seas, which calls for a reconsideration of current ocean changes with important consequences for our understanding of future Antarctic ice-sheet mass loss. The Southern Ocean takes up the most heat and carbon, yet because of its remote and harsh location, it remains relatively sparsely measured. Here the authors use a 25 year temperature series which shows a clear, long term trend in subsurface warming that emerges from interannual variability.</abstract>
      <custom6>032</custom6>
      <custom1>UR182 / UR065</custom1>
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