AN ORGANIZED SIGNAL IN SNOWMELT RUNOFF OVER THE WESTERN UNITED STATES
Daily-to-weekly discharge during the snowmelt season is highly correlated among river basins in the upper elevations of the central and southern Sierra Nevada (Carson, Walker, Tuolumne, Merced, San Joaquin, Kings, and Kern Rivers). In many cases, the upper Sierra Nevada watershed operates in a singl...
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Veröffentlicht in: | Journal of the American Water Resources Association 2000-04, Vol.36 (2), p.421-432 |
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creator | Peterson, D. H. Smith, R. E. Dettinger, M. D. Cayan, D. R. Riddle, L. |
description | Daily-to-weekly discharge during the snowmelt season is highly correlated among river basins in the upper elevations of the central and southern Sierra Nevada (Carson, Walker, Tuolumne, Merced, San Joaquin, Kings, and Kern Rivers). In many cases, the upper Sierra Nevada watershed operates in a single mode (with varying catchment amplitudes). In some years, with appropriate lags, this mode extends to distant mountains. A reason for this coherence is the broad scale nature of synoptic features in atmospheric circulation, which provide anomalous insolation and temperature forcings that span a large region, sometimes the entire western U.S. These correlations may fall off dramatically, however, in dry years when the snowpack is spatially patchy. |
doi_str_mv | 10.1111/j.1752-1688.2000.tb04278.x |
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A reason for this coherence is the broad scale nature of synoptic features in atmospheric circulation, which provide anomalous insolation and temperature forcings that span a large region, sometimes the entire western U.S. These correlations may fall off dramatically, however, in dry years when the snowpack is spatially patchy.</description><identifier>ISSN: 1093-474X</identifier><identifier>EISSN: 1752-1688</identifier><identifier>DOI: 10.1111/j.1752-1688.2000.tb04278.x</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><subject>hydroclimatology ; snow hydrology ; snowmelt ; surface water hydrology ; USA ; USA, Western ; water management</subject><ispartof>Journal of the American Water Resources Association, 2000-04, Vol.36 (2), p.421-432</ispartof><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Peterson, D. 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A reason for this coherence is the broad scale nature of synoptic features in atmospheric circulation, which provide anomalous insolation and temperature forcings that span a large region, sometimes the entire western U.S. These correlations may fall off dramatically, however, in dry years when the snowpack is spatially patchy.</description><subject>hydroclimatology</subject><subject>snow hydrology</subject><subject>snowmelt</subject><subject>surface water hydrology</subject><subject>USA</subject><subject>USA, Western</subject><subject>water management</subject><issn>1093-474X</issn><issn>1752-1688</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNo9UN1KwzAYDaLgnL5D8MK71qRJmvSyzqwr1BTazIo3JVlT2NzcbDuYb29l4rk5H5wfPg4A9xj5eMTjxsecBR4OhfADhJA_WEQDLvzTBZj8S5fjjSLiUU7frsFN328QwgwLMgEyVjAvklil7_IZlmmi4gymCpYqr15kpmGxVPl8DvNXWUC9kLCSpZaFgkuV6t-EjrUsb8FVa7a9u_vjKVjOpZ4tvCxP0lmceSagbPAsWznTcNEy56xtWhvhSLTcmoYiukLjq44ELTO0bVDDGmIQ5W0UCmNtJKywZAoezr2Hbv91dP1Q79b9ym235tPtj32NeTiOQNBo9M7GdT-4U33o1jvTfdem-6hDTjirK5XUT1wtiK5wHZIfDJVa_w</recordid><startdate>20000401</startdate><enddate>20000401</enddate><creator>Peterson, D. 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R.</creatorcontrib><creatorcontrib>Riddle, L.</creatorcontrib><collection>Istex</collection><collection>Aqualine</collection><collection>Pollution Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Journal of the American Water Resources Association</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Peterson, D. H.</au><au>Smith, R. E.</au><au>Dettinger, M. D.</au><au>Cayan, D. 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A reason for this coherence is the broad scale nature of synoptic features in atmospheric circulation, which provide anomalous insolation and temperature forcings that span a large region, sometimes the entire western U.S. These correlations may fall off dramatically, however, in dry years when the snowpack is spatially patchy.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1752-1688.2000.tb04278.x</doi><tpages>12</tpages></addata></record> |
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subjects | hydroclimatology snow hydrology snowmelt surface water hydrology USA USA, Western water management |
title | AN ORGANIZED SIGNAL IN SNOWMELT RUNOFF OVER THE WESTERN UNITED STATES |
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