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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ADGEO</journal-id>
<journal-title-group>
<journal-title>Advances in Geosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">ADGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Adv. Geosci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7359</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/adgeo-16-33-2008</article-id>
<title-group>
<article-title>Process-oriented statistical-dynamical evaluation of LM precipitation forecasts</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Claußnitzer</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>Langer</surname>
<given-names>I.</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>Névir</surname>
<given-names>P.</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>Reimer</surname>
<given-names>E.</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>Cubasch</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institut f¨ur Meteorologie, Freie Universität Berlin Carl-Heinrich-Becker-Weg 6-10, D-12165 Berlin, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>04</month>
<year>2008</year>
</pub-date>
<volume>16</volume>
<fpage>33</fpage>
<lpage>41</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 A. Claußnitzer et al.</copyright-statement>
<copyright-year>2008</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://adgeo.copernicus.org/articles/16/33/2008/adgeo-16-33-2008.html">This article is available from https://adgeo.copernicus.org/articles/16/33/2008/adgeo-16-33-2008.html</self-uri>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/16/33/2008/adgeo-16-33-2008.pdf">The full text article is available as a PDF file from https://adgeo.copernicus.org/articles/16/33/2008/adgeo-16-33-2008.pdf</self-uri>
<abstract>
<p>The objective of this study is the scale dependent evaluation of precipitation forecasts of the Lokal-Modell (LM) from the German Weather Service in relation to dynamical and cloud parameters. For this purpose the newly designed Dynamic State Index (&lt;i&gt;DSI&lt;/i&gt;) is correlated with clouds and precipitation. The &lt;i&gt;DSI&lt;/i&gt; quantitatively describes the deviation and relative distance from a
stationary and adiabatic solution of the primitive
equations.
A case study and statistical analysis of clouds and precipitation demonstrates the availability of the &lt;i&gt;DSI&lt;/i&gt; as a dynamical threshold parameter. This confirms the importance of imbalances of the atmospheric flow field, which dynamically induce the generation of rainfall.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</article>