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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-21-21-2003</article-id>
<title-group>
<article-title>Variability of mesoscale features in the Mediterranean Sea from XBT data analysis</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fusco</surname>
<given-names>G.</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>Manzella</surname>
<given-names>G. M. R.</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>Cruzado</surname>
<given-names>A.</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>Gačić</surname>
<given-names>M.</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>Gasparini</surname>
<given-names>G. P.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kovačević</surname>
<given-names>V.</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>Millot</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tziavos</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Velasquez</surname>
<given-names>Z. 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>Walne</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zervakis</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zodiatis</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>ENEA, Progetto Speciale Clima Globale, La Spezia, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CSIC, Centre d’Estudis Avançats de Blanes, Blanes, Spain</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>OGS, Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Trieste, Italy</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>CNR, Istituto di Oceanografia Fisica, La Spezia, Italy</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>CNRS, Laboratoire de Biochimique, Toulon, France</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>National Centre for Marine Research, Athens, Greece</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Sir Alistair Hardy Foundation on Oceanographic Studies, Plymouth, UK</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Laboratory of Physical Oceanography, Department of Fisheries and Marine Research, Nicosia, Cyprus</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>01</month>
<year>2003</year>
</pub-date>
<volume>21</volume>
<issue>1</issue>
<fpage>21</fpage>
<lpage>32</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2003 G. Fusco et al.</copyright-statement>
<copyright-year>2003</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/21/21/2003/angeo-21-21-2003.html">This article is available from https://angeo.copernicus.org/articles/21/21/2003/angeo-21-21-2003.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/21/21/2003/angeo-21-21-2003.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/21/21/2003/angeo-21-21-2003.pdf</self-uri>
<abstract>
<p>During the period 1998–2000,
 the Mediterranean Forecasting System Pilot Project, aiming to build a
 forecasting system for the physical state of the sea, has been carried out. A
 ship-of-opportunity programme sampled the Mediterranean upper ocean thermal
 structure by means of eXpendable Bathy-Thermographs (XBTs), along seven tracks,
 from September 1999 to May 2000. The tracks were designed to detect some of the
 main circulation features, such as the stream of surface Atlantic water flowing
 from the Alboran Sea to the Eastern Levantine Basin. The cyclonic gyres in the
 Liguro-Provenal Basin, the southern Adriatic and Ionian Seas and the
 anticyclonic gyres in the Levantine Basin were also features to be detected.&lt;/p&gt;
 &lt;p  style=&quot;line-height: 20px;&quot;&gt;The monitoring system confirmed a long-term persistence of
 structures (at least during the entire observing period), which were previously
 thought to be transient features. In particular, in the Levantine Basin
 anticyclonic Shikmona and Ierapetra Gyres have been observed during the
 monitoring period.&lt;/p&gt;
 &lt;p  style=&quot;line-height: 20px;&quot;&gt;In order to identify the major changes in the thermal
 structures and the dynamical implications, the XBT data are compared with
 historical measurements collected in the 1980s and 1990s. The results indicate
 that some thermal features are being restored to the situation that existed in
 the 1980s, after the changes induced by the so-called &amp;quot;Eastern
 Mediterranean Transient&amp;quot;.&lt;br&gt;&lt;br&gt;
 &lt;b&gt;Key words. &lt;/b&gt;Oceanography: physical
 (eddies and mesoscale processes; general circulation; instruments and
 techniques)</p>
</abstract>
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