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<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>10</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/npg-10-261-2003</doi>
	<article_url>http://www.nonlin-processes-geophys.net/10/261/2003/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/10/261/2003/npg-10-261-2003.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/10/261/2003/npg-10-261-2003.pdf</fulltext_pdf>
	<start_page>261</start_page>
	<end_page>274</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">The Soverato flood in Southern Italy: performance of global and limited-area ensemble forecasts</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Montani</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>C. Marsigli</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. Nerozzi</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>T. Paccagnella</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>S. Tibaldi</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>R. Buizza</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Regional Meteorological Service ARPA-SMR, Bologna, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Department of Earth Sciences, University of Bologna, Bologna, Italy</affiliation>
		<affiliation numeration="3" content_type="html">European Centre for Medium-Range Weather Forecasts, Reading, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The predictability
      of the flood event affecting Soverato (Southern Italy) in September 2000
      is investigated by considering three different configurations of ECMWF
      ensemble: the operational Ensemble Prediction System (EPS), the targeted
      EPS and a high-resolution version of EPS. For each configuration, three
      successive runs of ECMWF ensemble with the same verification time are
      grouped together so as to generate a highly-populated
      &amp;quot;super-ensemble&amp;quot;. Then, five members are selected from the
      super-ensemble and used to provide initial and boundary conditions for the
      integrations with a limited-area model, whose runs generate a Limited-area
      Ensemble Prediction System (LEPS). The relative impact of targeting the
      initial perturbations against increasing the horizontal resolution is
      assessed for the global ensembles as well as for the properties
      transferred to LEPS integrations, the attention being focussed on the
      probabilistic prediction of rainfall over a localised area. At the 108, 84
      and 60- hour forecast ranges, the overall performance of the global
      ensembles is not particularly accurate and the best results are obtained
      by the high-resolution version of EPS. The LEPS performance is very
      satisfactory in all configurations and the rainfall maps show probability
      peaks in the correct regions. LEPS products would have been of great
      assistance to issue flood risk alerts on the basis of limited-area
      ensemble forecasts. For the 60-hour forecast range, the sensitivity of the
      results to the LEPS ensemble size is discussed by comparing a 5-member
      against a 51-member LEPS, where the limited-area model is nested on all
      EPS members. Little sensitivity is found as concerns the detection of the
      regions most likely affected by heavy precipitation, the probability peaks
      being approximately the same in both configurations.</abstract>
	<references>
	</references>
</article>

