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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>26</volume_number>
		<volume_title>11th EGU Plinius Conference on Mediterranean Storms (2009)</volume_title>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/adgeo-26-61-2010</doi>
	<article_url>http://www.adv-geosci.net/26/61/2010/</article_url>
	<abstract_html>http://www.adv-geosci.net/26/61/2010/adgeo-26-61-2010.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/26/61/2010/adgeo-26-61-2010.pdf</fulltext_pdf>
	<start_page>61</start_page>
	<end_page>64</end_page>
	<publication_date>2010-07-09</publication_date>
	<article_title content_type="html">The effect of observation timescales on the characterisation of extreme Mediterranean precipitation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. M. Camarasa Belmonte</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Soriano García</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. J. López-García</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geography, University of Valencia Avda. Blasco Ibáñez, 28, 46010 Valencia, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">This paper analyses the behaviour of five rainfall indicators (maximum
intensity, cumulative rainfall, irregularity, probability of rain and
persistence of rain) over different observation timescales ranging from
5 min to 24 h. It covers a large area on the Mediterranean side of the
Iberian Peninsula (River Júcar Water Authority, 43 000 km&lt;sup&gt;2&lt;/sup&gt;) on a
continuous basis over a period of 14 years (1994–2007). The results show
that the behaviour of extreme Mediterranean rainfall is heavily dependent on
the observation timescale. There are a number of turning points in the
indicator trends which occur on different timescales (1 and 6 h in
the case of rain intensity and irregularity, 6 h for cumulative rainfall
and between 15 and 30 min for the persistence of rain) and may be
relevant for the determination of thresholds used in water management.</abstract>
	<references>
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</article>

