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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ANGEO</journal-id>
<journal-title-group>
<journal-title>Annales Geophysicae</journal-title>
<abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ann. Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1432-0576</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/angeo-24-3-2006</article-id>
<title-group>
<article-title>Comparison of a NLOM data assimilation product to direct measurements in the Antarctic Polar Frontal Zone: a case study</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Losch</surname>
<given-names>M.</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>Schukay</surname>
<given-names>R.</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>Strass</surname>
<given-names>V.</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>Cisewski</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Alfred-Wegener-Institut für Polar- und Meeresforschung, Bremerhaven, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Universität Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>03</month>
<year>2006</year>
</pub-date>
<volume>24</volume>
<issue>1</issue>
<fpage>3</fpage>
<lpage>6</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2006 M. Losch et al.</copyright-statement>
<copyright-year>2006</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://angeo.copernicus.org/articles/24/3/2006/angeo-24-3-2006.html">This article is available from https://angeo.copernicus.org/articles/24/3/2006/angeo-24-3-2006.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/24/3/2006/angeo-24-3-2006.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/24/3/2006/angeo-24-3-2006.pdf</self-uri>
<abstract>
<p>A comparison of the Naval Research Lab Layered Ocean Model (NLOM)
  nowcast fields with independent in-situ observations from a cruise
  in the Polar Frontal Zone of the Atlantic Sector of the Southern
  Ocean is presented.
  NLOM sea surface temperature fields can be used to determine the
  position of fronts and individual eddies, whereas the analyzed sea
  surface height appears to be out of phase. It is suggested that this
  dynamical inconsistency is caused by a low data coverage for
  assimilation at the time of the cruise in combination with the data
  assimilation technique, that treats sea surface height and sea
  surface temperature data independently.</p>
</abstract>
<counts><page-count count="4"/></counts>
</article-meta>
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