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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/hess-8-103-2004</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/8/103/2004/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/8/103/2004/hess-8-103-2004.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/8/103/2004/hess-8-103-2004.pdf</fulltext_pdf>
	<start_page>103</start_page>
	<end_page>107</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Estimating RUSLE’s rainfall factor in the part of Italy with a Mediterranean rainfall regime</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>N. Diodato</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Monte Pino Naturalistic Observatory, Contrada Monte Pino, 82100 Benevento, Italy</affiliation>
		<affiliation numeration="2" content_type="html">E-mail: nazdiod@tin.it</affiliation>
	</affiliations>
	<abstract content_type="html">The computation of the erosion index (&lt;i&gt;EI&lt;/i&gt;), which is basic to the 
     determination of the rainfall-runoff erosivity factor &lt;i&gt;R&lt;/i&gt; of the Revised Universal Soil 
     Loss Equation (RUSLE), is tedious and time-consuming and requires a continuous record of 
     rainfall intensity. In this study, a power equation(r&lt;sup&gt;2&lt;/sup&gt; &amp;#61; 0.867) involving annual 
     erosion index (&lt;i&gt;EI&lt;/i&gt;&lt;sub&gt;30-annual&lt;/sub&gt;) in the Mediterranean part of Italy is obtained. 
     Data from 12 raingauge stations are used to derive and then test a regional relationship for 
     estimating the erosion index from only three rainfall parameters. Erosivity rainfall data 
     derived from 5 additional stations are used for validation and critical examination. The 
     empirical procedures give results which compare satisfactorily with relationships calibrated 
     elsewhere.&lt;/p&gt;
&lt;p  style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;erosion index, rainfall, erosivity, Revised Universal Soil Loss Equation</abstract>
	<references>
	</references>
</article>

