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<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/nhess-10-379-2010</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/10/379/2010/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/10/379/2010/nhess-10-379-2010.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/10/379/2010/nhess-10-379-2010.pdf</fulltext_pdf>
	<start_page>379</start_page>
	<end_page>382</end_page>
	<publication_date>2010-02-23</publication_date>
	<article_title content_type="html">&lt;i&gt;Brief communication&lt;/i&gt; &quot;Does climatic change in precipitation drive erosion in Naxos Island, Greece?&quot;</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. T. Nastos</name>
			<email>nastos@geol.uoa.gr</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>N. Evelpidou</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Vassilopoulos</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory of Climatology and Atmospheric Environment, Faculty of Geology and Geoenvironment, University of Athens, Panepistimiopolis, 157 84 Athens, Greece</affiliation>
		<affiliation numeration="2" content_type="html">Department of Geography-Climatology, Faculty of Geology and Geoenvironment, University of Athens, Panepistimiopolis, 157 84 Athens, Greece</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper we examined whether the recorded precipitation changes cause
erosion in Naxos Island, Greece using precipitation indices derived from
daily precipitation totals, during the period 1955–2007, in order to develop
an erosion risk model. Although the mean annual precipitation appear to be
low (~360.0 mm), the erosion processes of the area are very intense,
because of the intensive character of precipitation, the high slope relief,
the differential lithology and the absence of important land cover The
results of the analysis showed that the climatic changes in precipitation and
the changes in land cover and land use are the main drivers for the erosion.
This is why the 2nd (1971–1985) and 3rd (1986–2007) studied sub-periods may
be called of high erosion risk, and especially the second one mainly because
of the increased frequency of extreme precipitation events.</abstract>
	<references>
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</article>

