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<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>10</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/hess-10-861-2006</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/10/861/2006/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/10/861/2006/hess-10-861-2006.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/10/861/2006/hess-10-861-2006.pdf</fulltext_pdf>
	<start_page>861</start_page>
	<end_page>871</end_page>
	<publication_date>2006-11-16</publication_date>
	<article_title content_type="html">Simplified stochastic soil-moisture models: a look at infiltration</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. R. Rigby</name>
			<email>jrrigby@duke.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Porporato</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Civil and Environmental Engineering, Duke University, Durham NC, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A simplified, vertically-averaged model of soil moisture interpreted at the daily time scale and forced by a
stochastic process of instantaneous rainfall events is compared with a vertically-averaged model which uses a
non-overlapping rectangular pulse rainfall model and a more physically based description of infiltration. The
models are compared with respect to the importance of short time-scale (intra-storm) variable infiltration in
determining the probabilistic structure of soil-moisture dynamics at the daily time-scale. Differences in
approach to infiltration modelling show only minor effects on the probabilistic structure of soil-moisture
dynamics as simulated in the two models. The partitioning of losses during a single rainfall event are examined
closely and the conditions under which surface-controlled runoff is significant, as a proportion of total
losses, are delineated.</abstract>
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</article>

