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<front>
<journal-meta>
<journal-id journal-id-type="publisher">TC</journal-id>
<journal-title-group>
<journal-title>The Cryosphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">TC</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">The Cryosphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1994-0424</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/tc-6-985-2012</article-id>
<title-group>
<article-title>Limitations of a coupled regional climate model in the reproduction of the observed Arctic sea-ice retreat</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dorn</surname>
<given-names>W.</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>Dethloff</surname>
<given-names>K.</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>Rinke</surname>
<given-names>A.</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 Institute for Polar and Marine Research, Telegrafenberg A43, 14473 Potsdam, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>09</month>
<year>2012</year>
</pub-date>
<volume>6</volume>
<issue>5</issue>
<fpage>985</fpage>
<lpage>998</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 W. Dorn et al.</copyright-statement>
<copyright-year>2012</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://tc.copernicus.org/articles/6/985/2012/tc-6-985-2012.html">This article is available from https://tc.copernicus.org/articles/6/985/2012/tc-6-985-2012.html</self-uri>
<self-uri xlink:href="https://tc.copernicus.org/articles/6/985/2012/tc-6-985-2012.pdf">The full text article is available as a PDF file from https://tc.copernicus.org/articles/6/985/2012/tc-6-985-2012.pdf</self-uri>
<abstract>
<p>The effects of internal model variability on the simulation of
 Arctic sea-ice extent and volume have been examined with the aid of
 a seven-member ensemble with a coupled regional climate model for
 the period 1948–2008. Beyond general weaknesses related to
 insufficient representation of feedback processes, it is found that
 the model&apos;s ability to reproduce observed summer sea-ice retreat
 depends mainly on two factors: the correct simulation of the
 atmospheric circulation during the summer months and the sea-ice
 volume at the beginning of the melting period. Since internal model
 variability shows its maximum during the summer months, the ability
 to reproduce the observed atmospheric summer circulation is limited.
 In addition, the atmospheric circulation during summer also
 significantly affects the sea-ice volume over the years leading to
 a limited ability to start with reasonable sea-ice volume into the
 melting period. Furthermore, the sea-ice volume pathway shows
 notable decadal variability that varies in amplitude among the
 ensemble members. The scatter is particularly large in periods when
 the ice volume increases, indicating limited skill in reproducing
 high-ice years.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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