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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-8-47-2004</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/8/47/2004/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/8/47/2004/hess-8-47-2004.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/8/47/2004/hess-8-47-2004.pdf</fulltext_pdf>
	<start_page>47</start_page>
	<end_page>61</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Spatial and temporal variations in precipitation in the Upper Indus Basin, global teleconnections and hydrological implications</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>D.R. Archer</name>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>H.J. Fowler</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">JBAConsulting, South Barn, Broughton Hall, Scripton, North Yorkshire, BD23 3AE, UK</affiliation>
		<affiliation numeration="2" content_type="html">Water Resource Systems Research Laboratory, School of Civil Engineering and Geosciences, University of Newcastle, Newcastle upon Tyne NE1 7RU, UK</affiliation>
		<affiliation numeration="3" content_type="html">Email for corresponding author: davearcher@yahoo.com</affiliation>
	</affiliations>
	<abstract content_type="html">Most of the flow in the River Indus from its upper mountain basin is derived 
        from melting snow and glaciers. Climatic variability and change of both precipitation and 
        energy inputs will, therefore, affect rural livelihoods at both a local and a regional 
        scale through effects on summer runoff in the River Indus. Spatial variation in 
        precipitation has been investigated by correlation and regression analysis of long-period 
        records. There is a strong positive correlation between winter precipitation at stations 
        over the entire region, so that, for practical forecasting of summer runoff in some basins, 
        a single valley-floor precipitation station can be used In contrast, spatial relationships 
        in seasonal precipitation are weaker in summer and sometimes significantly negative between 
        stations north and south of the Himalayan divide. Although analysis of long datasets of 
        precipitation from 1895 shows no significant trend, from 1961–1999 there are statistically 
        significant increases in winter, in summer and in the annual precipitation at several 
        stations. Preliminary analysis has identified a significant positive correlation between 
        the winter North Atlantic Oscillation (NAO) and winter precipitation in the Karakoram and 
        a negative correlation between NAO and summer rainfall at some stations.&lt;/p&gt;
&lt;p  style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;upper Indus basin, climate change, time series analysis, spatial correlation, 
        teleconnections</abstract>
	<references>
	</references>
</article>

