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    <titleInfo>
      <title>Ocean-atmosphere coupling in the monsoon intraseasonal oscillation : a simple model study</title>
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    <name type="personnal">
      <namePart type="family">Bellon</namePart>
      <namePart type="given">G.</namePart>
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    <name type="personnal">
      <namePart type="family">Sobel</namePart>
      <namePart type="given">A. H.</namePart>
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    <name type="personnal">
      <namePart type="family">Vialard</namePart>
      <namePart type="given">Jérôme</namePart>
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    <abstract>A simple coupled model is used in a zonally symmetric aquaplanet configuration to investigate the effect of ocean-atmosphere coupling on the Asian monsoon intraseasonal oscillation. The model consists of a linear atmospheric model of intermediate complexity based on quasi-equilibrium theory coupled to a simple, linear model of the upper ocean. This model has one unstable eigenmode with a period in the 30-60-day range and a structure similar to the observed northward-propagating intraseasonal oscillation in the Bay of Bengal/west Pacific sector. The ocean-atmosphere coupling is shown to have little impact on either the growth rate or latitudinal structure of the atmospheric oscillation, but it reduces the oscillation's period by a quarter. At latitudes corresponding to the north of the Indian Ocean, the sea surface temperature (SST) anomalies lead the precipitation anomalies by a quarter of a period, similarly to what has been observed in the Bay of Bengal. The mixed layer depth is in phase opposition to the SST: a monsoon break corresponds to both a warming and a shoaling of the mixed layer. This behavior results from the similarity between the patterns of the predominant processes: wind-induced surface heat flux and wind stirring. The instability of the seasonal monsoon flow is sensitive to the seasonal mixed layer depth: the oscillation is damped when the oceanic mixed layer is thin (about 10 m deep or thinner), as in previous experiments with several models aimed at addressing the boreal winter Madden-Julian oscillation. This suggests that the weak thermal inertia of land might explain the minima of intraseasonal variance observed over the Asian continent.</abstract>
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    <classification authority="local">032</classification>
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      <titleInfo>
        <title>Journal of Climate</title>
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      <part>
        <detail type="volume">
          <number>21</number>
        </detail>
        <detail type="volume">
          <number>20</number>
        </detail>
        <extent unit="pages">
          <list> 5254-5270</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2008</dateIssued>
      </originInfo>
      <identifier type="issn">0894-8755</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010044088</identifier>
    <identifier type="doi">10.1175/2008jcli2305.1</identifier>
    <identifier type="issn">0894-8755</identifier>
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      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/fdi:010044088</url>
      <url access="row object">https://www.documentation.ird.fr/intranet/publi/2008/11/010044088.pdf</url>
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      <recordCreationDate encoding="w3cdtf">2008-12-05</recordCreationDate>
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