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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>12</volume_number>
		<volume_title>Mediterranean storms and extreme events in an era of climate change</volume_title>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/adgeo-12-19-2007</doi>
	<article_url>http://www.adv-geosci.net/12/19/2007/</article_url>
	<abstract_html>http://www.adv-geosci.net/12/19/2007/adgeo-12-19-2007.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/12/19/2007/adgeo-12-19-2007.pdf</fulltext_pdf>
	<start_page>19</start_page>
	<end_page>26</end_page>
	<publication_date>2007-06-27</publication_date>
	<article_title content_type="html">Two case studies of severe storms in the Mediterranean using AMSU</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. M. Funatsu</name>
			<email>funatsu@lmd.polytechnique.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. Claud</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J.-P. Chaboureau</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Meteorologie Dynamique/IPSL, Ecole Polytechnique, 91128 Palaiseau CEDEX, France</affiliation>
		<affiliation numeration="2" content_type="html">Laboratoire d&apos;Aérologie, Observatoire Midi-Pyrénées, 14 avenue Belin, 31400 Toulouse, France</affiliation>
	</affiliations>
	<abstract content_type="html">Mediterranean storms and their associated upper level features are
diagnosed here using Advanced Microwave Sounding Unit (AMSU) observations.
AMSU-A channel 8 is used to identify upper-level intrusions of
stratospheric air, which are
often present upstream of heavy precipitating areas, while
a combination of AMSU-B channels 3 and 5 is chosen to discriminate moderate
to heavily precipitating areas. This precipitation detection
method provides results that are in good agreement with TRMM rainfall
product and independent ground-based precipitation
data. These tools allow us to follow the concomitant evolution
of two severe rainfall events in the Mediterranean region
and associated upper-level features.</abstract>
	<references>
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</article>

