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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-16-11-2008</doi>
	<article_url>http://www.adv-geosci.net/16/11/2008/</article_url>
	<abstract_html>http://www.adv-geosci.net/16/11/2008/adgeo-16-11-2008.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/16/11/2008/adgeo-16-11-2008.pdf</fulltext_pdf>
	<start_page>11</start_page>
	<end_page>17</end_page>
	<publication_date>2008-04-09</publication_date>
	<article_title content_type="html">Precipitation classification at mid-latitudes in terms of drop size distribution parameters</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Caracciolo</name>
			<email>caracciolo@fe.infn.it</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Porcù</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>F. Prodi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physics, University of Ferrara, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Atmospheric Sciences and Climate of the Italian National Research Council (ISAC-CNR), Bologna, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">The drop size distribution (DSD) is a fundamental property of rainfall
because the shape of the distribution reflects the physics of rain formation
processes. Given the lack of studies on the DSD at mid-latitudes, the
present work focuses on the microphysical characterization of precipitation
events occurring in Italy, using two different types of disdrometer. A large
number of different rain events was collected: they underwent microphysical
analysis by computing the Z-R relationships, observing the average DSDs and
DSD parameters, fitting the real distribution for different rainfall rate
categories and applying convective (C) &amp;ndash; stratiform (S) discrimination
algorithms. A general agreement with past works at mid-latitudes is found
both in the Z-R relationship and in DSD parameters. The rain distribution is
well described by a gamma DSD and only in some cases (especially the light
rain events) by an exponential DSD. Marked differences are observed in DSD
parameters and Z-R relationships between C and S episodes. The use of
disdrometers for areas covered by multiparametric radar is suggested and
will be performed in the near future.</abstract>
	<references>
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</article>

