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<!DOCTYPE article SYSTEM "http://www.adv-geosci.net/inc/adgeo/copernicus.dtd">
<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>7</volume_number>
		<volume_title>7th Plinius Conference on Mediterranean Storms (2005)</volume_title>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/adgeo-7-15-2006</doi>
	<article_url>http://www.adv-geosci.net/7/15/2006/</article_url>
	<abstract_html>http://www.adv-geosci.net/7/15/2006/adgeo-7-15-2006.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/7/15/2006/adgeo-7-15-2006.pdf</fulltext_pdf>
	<start_page>15</start_page>
	<end_page>18</end_page>
	<publication_date>2006-01-13</publication_date>
	<article_title content_type="html">Warm season precipitation climatology: first European results</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. Levizzani</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Ginnetti</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. G. Laing</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>R. E. Carbone</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Research Council, Institute of Atmospheric Sciences and Climate, Bologna, Italy</affiliation>
		<affiliation numeration="2" content_type="html">National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">To date very low scores are associated to quantitative precipitation
forecasts (QPF) of warm season precipitation, a fact mostly due to the
little knowledge of the mechanisms driving these phenomena. The study aims
to produce a five-year climatology (1999–2003) of warm season precipitation
systems (MJJA) over Europe using Meteosat IR brightness temperatures as a
contribution to a global study launched by the World Weather Research
Programme (WWRP). Cold cloud persistence, span and duration of weather
systems were determined to derive the zonal propagation speed and daily
cycles.</abstract>
	<references>
	</references>
</article>

