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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-7-387-2006</article-id>
<title-group>
<article-title>On the potential of sub-mm passive MW observations from  geostationary satellites to retrieve heavy precipitation over the  Mediterranean Area</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pinori</surname>
<given-names>S.</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>Baordo</surname>
<given-names>F.</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>Medaglia</surname>
<given-names>C. M.</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>Mugnai</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>Bizzarri</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Consiglio Nazionale delle Ricerche &amp;ndash; Istituto di Fisica  dell&apos;Atmosfera e del Clima, Area di Ricerca di Tor Vergata, Via Fosso del  Cavaliere 100, 00133 Roma, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>11</month>
<year>2006</year>
</pub-date>
<volume>7</volume>
<fpage>387</fpage>
<lpage>394</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2006 S. Pinori et al.</copyright-statement>
<copyright-year>2006</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/7/387/2006/adgeo-7-387-2006.html">This article is available from https://adgeo.copernicus.org/articles/7/387/2006/adgeo-7-387-2006.html</self-uri>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/7/387/2006/adgeo-7-387-2006.pdf">The full text article is available as a PDF file from https://adgeo.copernicus.org/articles/7/387/2006/adgeo-7-387-2006.pdf</self-uri>
<abstract>
<p>The general interest in the potential use of the mm and sub-mm frequencies
up to 425 GHz resolution from geostationary orbit is increasing due to the
fact that the frequent time sampling and the comparable spatial resolution
relative to the &quot;classical&quot; (&amp;le;89 GHz) microwave frequencies would
allow the monitoring of precipitating intense events for the assimilation of
rain in now-casting weather prediction models.

&lt;br&gt;&lt;br&gt;
In this paper, we use the simulation of a heavy precipitating event in front
of the coast of Crete island (Greece) performed by the University of
Wisconsin - Non-hydrostatic Modeling System (UW-NMS) cloud resolving model
in conjunction with a 3D-adjusted plane parallel radiative transfer model to
simulate the upwelling brightness temperatures (TB&apos;s) at mm and sub-mm
frequencies. To study the potential use of high frequencies, we first
analyze the relationships of the simulated TB&apos;s with the microphysical
properties of the UW-NMS simulated precipitating clouds, and then explore
the capability of a Bayesian algorithm for the retrieval of surface rain
rate, rain and ice water paths at such frequencies.</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>