<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-5-2355-2005</article-id>
<title-group>
<article-title>Comparison of raingauge observations with modeled precipitation over Cyprus using Contiguous Rain Area analysis</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tartaglione</surname>
<given-names>N.</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>Mariani</surname>
<given-names>S.</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>Accadia</surname>
<given-names>C.</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>Speranza</surname>
<given-names>A.</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>Casaioli</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, University of Camerino, Camerino, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Agenzia per la Protezione dell’Ambiente e per i Servizi Tecnici, Rome, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Mathematics and Informatics, University of Camerino, Camerino, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>04</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>2355</fpage>
<lpage>2376</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/5/2355/2005/acpd-5-2355-2005.html">This article is available from http://www.atmos-chem-phys-discuss.net/5/2355/2005/acpd-5-2355-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/5/2355/2005/acpd-5-2355-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/5/2355/2005/acpd-5-2355-2005.pdf</self-uri>
<abstract>
<p>Verification of modeled rainfall with precipitation observed by a rain gauge network has been performed in a case study over the Cyprus Island.
Cyprus has a relatively dense rain gauge network. The applied verification method is the Contiguous Rain Area (CRA) analysis.
 In this work some drawbacks are pointed out when CRA method is applied in such a case study. Impact on CRA results, when considering different
 dimensions of the compared model domain and different types of indicators (correlation and mean square error) used in the comparison, are discussed.
  Results indicate that care has to be taken when verification of modeled rainfall is performed over some of islands or hydrological basins.</p>
</abstract>
<counts><page-count count="22"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>