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<article language="en">
	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>16</volume_number>
		<volume_title>Observation, Prediction and Verification of Precipitation (EGU Session 2007)</volume_title>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/adgeo-16-27-2008</doi>
	<article_url>http://www.adv-geosci.net/16/27/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/16/27/2008/adgeo-16-27-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/16/27/2008/adgeo-16-27-2008.pdf</fulltext_pdf>
	<start_page>27</start_page>
	<end_page>32</end_page>
	<publication_date>2008-04-09</publication_date>
	<article_title content_type="html">Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>F. Teschl</name>
			<email>franz.teschl@tugraz.at</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>W. L. Randeu</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. Schönhuber</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>R. Teschl</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Broadband Communications, Graz University of Technology, Graz, Austria</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Applied Systems Technology, Joanneum Research, Graz, Austria</affiliation>
	</affiliations>
	<abstract content_type="html">Polarimetric radar variables of rainfall events, like differential
reflectivity &lt;i&gt;Z&lt;/i&gt;&lt;sub&gt;DR&lt;/sub&gt;, or specific differential phase &lt;i&gt;K&lt;/i&gt;&lt;sub&gt;DP&lt;/sub&gt;, are better
suited for estimating rain rate &lt;i&gt;R&lt;/i&gt; than just the reflectivity factor for
horizontally polarized waves, &lt;i&gt;Z&lt;/i&gt;&lt;sub&gt;H&lt;/sub&gt;. A variety of physical and empirical
approaches exist to estimate the rain rate from polarimetric radar
observables. The relationships vary over a wide range with the location and
the weather conditions.

In this study, the polarimetric radar variables were simulated for S-, C-
and X-band wavelengths in order to establish radar rainfall estimators for
the alpine region of the form &lt;i&gt;R&lt;/i&gt;(&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;DP&lt;/sub&gt;), &lt;i&gt;R&lt;/i&gt;(&lt;i&gt;Z&lt;/i&gt;&lt;sub&gt;H&lt;/sub&gt;, &lt;i&gt;Z&lt;/i&gt;&lt;sub&gt;DR&lt;/sub&gt;), and
&lt;i&gt;R&lt;/i&gt;(&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;DP&lt;/sub&gt;), &lt;i&gt;Z&lt;/i&gt;&lt;sub&gt;DR&lt;/sub&gt;. For the simulation drop size distributions of hundreds
of 1-minute-rain episodes were obtained from 2D-Video-Distrometer
measurements in the mountains of Styria, Austria. The sensitivity of the
polarimetric variables to temperature is investigated, as well as the
influence of different rain drop shape models &amp;ndash; including recently
published ones &amp;ndash; on radar rainfall estimators. Finally it is shown how the
polarimetric radar variables change with the elevation angle of the
radar antenna.</abstract>
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</article>

