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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>11</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/hess-11-408-2007</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/11/408/2007/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/11/408/2007/hess-11-408-2007.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/11/408/2007/hess-11-408-2007.pdf</fulltext_pdf>
	<start_page>408</start_page>
	<end_page>414</end_page>
	<publication_date>2007-01-17</publication_date>
	<article_title content_type="html">Hydrological prediction in a non-stationary world</article_title>
	<authors>
		<author numeration="1" affiliations="">
			<name>R. T. Clarke</name>
		</author>
	</authors>
	<affiliations>
	</affiliations>
	<abstract content_type="html">The paper discusses evidence that common assumptions in the analysis of hydrological time series (homogeneous variability in random fluctuations about a constant mean value) may not be appropriate for some South American drainage basins. Relatively rapid changes have occurred, and are occurring, as a consequence of replacing mature forest by short crops and urban development. Some research claims to have detected non-linear trends in streamflow in rivers draining the south-eastern part of the sub-continent, together with decadal fluctuations and interannual peaks at ENSO timescales. The paper discusses the implications of such changes for hydrological practices now in widespread and largely unquestioned use.</abstract>
	<references>
	</references>
</article>

