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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%">Roxy, M. K.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ritika, K.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Terray, Pascal</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Murtugudde, R.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ashok, K.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Goswami, B. N.</style>
          </author>
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      <titles>
        <title>Drying of Indian subcontinent by rapid Indian Ocean warming and a weakening land-sea thermal gradient</title>
        <secondary-title>Nature Communications</secondary-title>
      </titles>
      <pages>art. 7423 [10 ]</pages>
      <keywords>
        <keyword>INDE</keyword>
        <keyword>OCEAN INDIEN</keyword>
      </keywords>
      <dates>
        <year>2015</year>
      </dates>
      <call-num>fdi:010065146</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Nature Communications</full-title>
      </periodical>
      <isbn>2041-1723</isbn>
      <accession-num>ISI:000357176400003</accession-num>
      <electronic-resource-num>10.1038/ncomms8423</electronic-resource-num>
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      <volume>6</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>There are large uncertainties looming over the status and fate of the South Asian summer monsoon, with several studies debating whether the monsoon is weakening or strengthening in a changing climate. Our analysis using multiple observed datasets demonstrates a significant weakening trend in summer rainfall during 1901-2012 over the central-east and northern regions of India, along the Ganges-Brahmaputra-Meghna basins and the Himalayan foothills, where agriculture is still largely rain-fed. Earlier studies have suggested an increase in moisture availability and land-sea thermal gradient in the tropics due to anthropogenic warming, favouring an increase in tropical rainfall. Here we show that the land-sea thermal gradient over South Asia has been decreasing, due to rapid warming in the Indian Ocean and a relatively subdued warming over the subcontinent. Using long-term observations and coupled model experiments, we provide compelling evidence that the enhanced Indian Ocean warming potentially weakens the land-sea thermal contrast, dampens the summer monsoon Hadley circulation, and thereby reduces the rainfall over parts of South Asia.</abstract>
      <custom6>032 ; 021</custom6>
      <custom1>UR182</custom1>
      <custom7>Inde</custom7>
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