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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESS</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1684-9981</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/nhess-13-1567-2013</article-id>
<title-group>
<article-title>Coupled atmosphere ocean climate model simulations in the Mediterranean region: effect of a high-resolution marine model on cyclones and precipitation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sanna</surname>
<given-names>A.</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>Lionello</surname>
<given-names>P.</given-names>
<ext-link>https://orcid.org/0000-0002-0779-5681</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gualdi</surname>
<given-names>S.</given-names>
<ext-link>https://orcid.org/0000-0001-7777-8935</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CMCC, viale Aldo Moro 44, 40127 Bologna, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Unisalento, S.P. 6, Monteroni, 73100 Lecce, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>INGV, via Donato Creti 12, 40128 Bologna, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>06</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>6</issue>
<fpage>1567</fpage>
<lpage>1577</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 A. Sanna et al.</copyright-statement>
<copyright-year>2013</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://nhess.copernicus.org/articles/13/1567/2013/nhess-13-1567-2013.html">This article is available from https://nhess.copernicus.org/articles/13/1567/2013/nhess-13-1567-2013.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/13/1567/2013/nhess-13-1567-2013.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/13/1567/2013/nhess-13-1567-2013.pdf</self-uri>
<abstract>
<p>In this study we investigate the importance of an eddy-permitting
Mediterranean Sea circulation model on the simulation of atmospheric
cyclones and precipitation in a climate model. This is done by analyzing
results of two fully coupled GCM (general circulation models) simulations, differing only for the
presence/absence of an interactive marine module, at very
high-resolution (~ 1/16°), for the simulation of the 3-D
circulation of the Mediterranean Sea. Cyclones are tracked by applying an
objective Lagrangian algorithm to the MSLP (mean sea level pressure) field. On annual basis, we find a
statistically significant difference in vast cyclogenesis regions (northern
Adriatic, Sirte Gulf, Aegean Sea and southern Turkey) and in lifetime,
giving evidence of the effect of both land–sea contrast and surface heat
flux intensity and spatial distribution on cyclone characteristics.
Moreover, annual mean convective precipitation changes significantly in the
two model climatologies as a consequence of differences in both air–sea
interaction strength and frequency of cyclogenesis in the two analyzed
simulations.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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