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<front>
<journal-meta>
<journal-id journal-id-type="publisher">OS</journal-id>
<journal-title-group>
<journal-title>Ocean Science</journal-title>
<abbrev-journal-title abbrev-type="publisher">OS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ocean Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1812-0792</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/os-7-755-2011</article-id>
<title-group>
<article-title>An empirical stochastic model of sea-surface temperatures and surface winds over the Southern Ocean</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kravtsov</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kondrashov</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kamenkovich</surname>
<given-names>I.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ghil</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Wisconsin-Milwaukee, Dept. of Mathematical Sciences, Atmospheric Science group, P.O. Box 413, Milwaukee, WI 53201, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of California at Los Angeles, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Miami, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Ecole Normale Supérieure, Paris, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>11</month>
<year>2011</year>
</pub-date>
<volume>7</volume>
<issue>6</issue>
<fpage>755</fpage>
<lpage>770</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 S. Kravtsov et al.</copyright-statement>
<copyright-year>2011</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://os.copernicus.org/articles/7/755/2011/os-7-755-2011.html">This article is available from https://os.copernicus.org/articles/7/755/2011/os-7-755-2011.html</self-uri>
<self-uri xlink:href="https://os.copernicus.org/articles/7/755/2011/os-7-755-2011.pdf">The full text article is available as a PDF file from https://os.copernicus.org/articles/7/755/2011/os-7-755-2011.pdf</self-uri>
<abstract>
<p>This study employs NASA&apos;s recent satellite measurements of sea-surface
temperatures (SSTs) and sea-level winds (SLWs) with missing data filled-in
by Singular Spectrum Analysis (SSA), to construct empirical models that
capture both intrinsic and SST-dependent aspects of SLW variability. The
model construction methodology uses a number of algorithmic innovations that
are essential in providing stable estimates of the model&apos;s propagator. The
best model tested herein is able to faithfully represent the time scales and
spatial patterns of anomalies associated with a number of distinct
processes. These processes range from the daily synoptic variability to
interannual signals presumably associated with oceanic or coupled dynamics.
Comparing the simulations of an SLW model forced by the observed SST
anomalies with the simulations of an SLW-only model provides preliminary
evidence for the ocean driving the atmosphere in the Southern Ocean region.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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