Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds
Identifieur interne : 000829 ( Istex/Corpus ); précédent : 000828; suivant : 000830Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds
Auteurs : Dingbao Wang ; Ximing CaiSource :
- Geophysical Research Letters [ 0094-8276 ] ; 2010-03.
Abstract
This study explores the long‐term trends of low flow magnitude and the slopes and shapes of the recession curves during winter and summer seasons under climatic and human factors. Four watersheds in the American Midwest are selected for the analysis, including two urban watersheds (Salt Creek and Des Plaines) and two agricultural watersheds (Embarras and Kankakee). The results show that the long‐term baseflow recession slope trends in all the watersheds are primarily induced by human interferences. In the urban watersheds, the recession slopes decrease over time in both winter and summer due to effluent discharges. In the Kankakee watershed with irrigation, the recession slopes decrease in winter but increase in summer, and the opposite winter and summer trends are caused by the seasonal water use regime of irrigated agriculture. In the Embarras watershed with rainfed agriculture, the recession slopes decrease over time in winter but display no change in summer. Sources of water withdrawal (groundwater versus surface water) also have different impacts on the recession process. This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. Beyond the specific case studies, this paper documents how a scientific approach based on existing streamflow observation can be applied to improving our understanding of the impact of human and climatic influences on baseflow and low flow processes.
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DOI: 10.1029/2009GL041879
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title><author><name sortKey="Wang, Dingbao" sort="Wang, Dingbao" uniqKey="Wang D" first="Dingbao" last="Wang">Dingbao Wang</name><affiliation><mods:affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</mods:affiliation></affiliation></author><author><name sortKey="Cai, Ximing" sort="Cai, Ximing" uniqKey="Cai X" first="Ximing" last="Cai">Ximing Cai</name><affiliation><mods:affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: xmcai@illinois.edu</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934</idno><date when="2010" year="2010">2010</date><idno type="doi">10.1029/2009GL041879</idno><idno type="url">https://api.istex.fr/document/6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000829</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000829</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title><author><name sortKey="Wang, Dingbao" sort="Wang, Dingbao" uniqKey="Wang D" first="Dingbao" last="Wang">Dingbao Wang</name><affiliation><mods:affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</mods:affiliation></affiliation></author><author><name sortKey="Cai, Ximing" sort="Cai, Ximing" uniqKey="Cai X" first="Ximing" last="Cai">Ximing Cai</name><affiliation><mods:affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: xmcai@illinois.edu</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geophysical Research Letters</title><title level="j" type="abbrev">Geophys. Res. Lett.</title><idno type="ISSN">0094-8276</idno><idno type="eISSN">1944-8007</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2010-03">2010-03</date><biblScope unit="volume">37</biblScope><biblScope unit="issue">6</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">0094-8276</idno></series><idno type="istex">6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934</idno><idno type="DOI">10.1029/2009GL041879</idno><idno type="ArticleID">2009GL041879</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0094-8276</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">This study explores the long‐term trends of low flow magnitude and the slopes and shapes of the recession curves during winter and summer seasons under climatic and human factors. Four watersheds in the American Midwest are selected for the analysis, including two urban watersheds (Salt Creek and Des Plaines) and two agricultural watersheds (Embarras and Kankakee). The results show that the long‐term baseflow recession slope trends in all the watersheds are primarily induced by human interferences. In the urban watersheds, the recession slopes decrease over time in both winter and summer due to effluent discharges. In the Kankakee watershed with irrigation, the recession slopes decrease in winter but increase in summer, and the opposite winter and summer trends are caused by the seasonal water use regime of irrigated agriculture. In the Embarras watershed with rainfed agriculture, the recession slopes decrease over time in winter but display no change in summer. Sources of water withdrawal (groundwater versus surface water) also have different impacts on the recession process. This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. Beyond the specific case studies, this paper documents how a scientific approach based on existing streamflow observation can be applied to improving our understanding of the impact of human and climatic influences on baseflow and low flow processes.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Dingbao Wang</name><affiliations><json:string>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</json:string></affiliations></json:item><json:item><name>Ximing Cai</name><affiliations><json:string>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</json:string><json:string>E-mail: xmcai@illinois.edu</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>baseflow recession slope</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>climate and human impacts</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>urban and agricultural watersheds</value></json:item></subject><articleId><json:string>2009GL041879</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>This study explores the long‐term trends of low flow magnitude and the slopes and shapes of the recession curves during winter and summer seasons under climatic and human factors. Four watersheds in the American Midwest are selected for the analysis, including two urban watersheds (Salt Creek and Des Plaines) and two agricultural watersheds (Embarras and Kankakee). The results show that the long‐term baseflow recession slope trends in all the watersheds are primarily induced by human interferences. In the urban watersheds, the recession slopes decrease over time in both winter and summer due to effluent discharges. In the Kankakee watershed with irrigation, the recession slopes decrease in winter but increase in summer, and the opposite winter and summer trends are caused by the seasonal water use regime of irrigated agriculture. In the Embarras watershed with rainfed agriculture, the recession slopes decrease over time in winter but display no change in summer. Sources of water withdrawal (groundwater versus surface water) also have different impacts on the recession process. This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. Beyond the specific case studies, this paper documents how a scientific approach based on existing streamflow observation can be applied to improving our understanding of the impact of human and climatic influences on baseflow and low flow processes.</abstract><qualityIndicators><score>7.02</score><pdfVersion>1.4</pdfVersion><pdfPageSize>612 x 792 pts (letter)</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1515</abstractCharCount><pdfWordCount>3784</pdfWordCount><pdfCharCount>23702</pdfCharCount><pdfPageCount>6</pdfPageCount><abstractWordCount>228</abstractWordCount></qualityIndicators><title>Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title><genre><json:string>article</json:string></genre><host><volume>37</volume><publisherId><json:string>GRL</json:string></publisherId><pages><total>6</total><last>n/a</last><first>n/a</first></pages><issn><json:string>0094-8276</json:string></issn><issue>6</issue><subject><json:item><value>HYDROLOGY</value></json:item><json:item><value>Human impacts</value></json:item><json:item><value>Streamflow</value></json:item><json:item><value>Catchment</value></json:item><json:item><value>Climate impacts</value></json:item><json:item><value>NATURAL HAZARDS</value></json:item><json:item><value>Human impact</value></json:item><json:item><value>Climate impact</value></json:item><json:item><value>Hydrology and Land Surface Studies</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1944-8007</json:string></eissn><title>Geophysical Research Letters</title><doi><json:string>10.1002/(ISSN)1944-8007</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>meteorology & atmospheric sciences</json:string></scienceMetrix></categories><publicationDate>2010</publicationDate><copyrightDate>2010</copyrightDate><doi><json:string>10.1029/2009GL041879</json:string></doi><id>6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934</id><score>0.04142177</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><availability><p>Copyright 2010 by the American Geophysical Union.</p></availability><date>2010</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title><author xml:id="author-1"><persName><forename type="first">Dingbao</forename><surname>Wang</surname></persName><affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</affiliation></author><author xml:id="author-2"><persName><forename type="first">Ximing</forename><surname>Cai</surname></persName><email>xmcai@illinois.edu</email><affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</affiliation></author></analytic><monogr><title level="j">Geophysical Research Letters</title><title level="j" type="abbrev">Geophys. 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This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. 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Res. Lett.</journalTitle>, <vol>37</vol>, L06406, doi:<accessionId ref="info:doi/10.1029/2009GL041879">10.1029/2009GL041879</accessionId>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:GRL.GRL26774.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="2"></count><count type="tableTotal" number="1"></count></countGroup><titleGroup><title type="main">Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title><title type="short">BASEFLOW RECESSION SLOPE TREND</title><title type="shortAuthors">Wang and Cai</title></titleGroup><creators><creator creatorRole="author" xml:id="grl26774-cr-0001" affiliationRef="#grl26774-aff-0001"><personName><givenNames>Dingbao</givenNames> <familyName>Wang</familyName></personName></creator><creator creatorRole="author" xml:id="grl26774-cr-0002" affiliationRef="#grl26774-aff-0001"><personName><givenNames>Ximing</givenNames> <familyName>Cai</familyName></personName><contactDetails><email normalForm="xmcai@illinois.edu">xmcai@illinois.edu</email></contactDetails></creator></creators><affiliationGroup><affiliation countryCode="US" type="organization" xml:id="grl26774-aff-0001"><orgDiv>Department of Civil and Environmental Engineering</orgDiv><orgName>University of Illinois at Urbana‐Champaign</orgName><address><city>Urbana</city><countryPart>Illinois</countryPart><country>USA</country></address></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="grl26774-kwd-0001">baseflow recession slope</keyword><keyword xml:id="grl26774-kwd-0002">climate and human impacts</keyword><keyword xml:id="grl26774-kwd-0003">urban and agricultural watersheds</keyword></keywordGroup><supportingInformation xml:id="grl26774-sup-0000"><p xml:id="grl26774-para-0001">Auxiliary material for this article contains includes 2 tables and 5 figures.</p><p xml:id="grl26774-para-0002">Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac).</p><p xml:id="grl26774-para-0003">See <url href="/pubs/plugins.html">Plugins</url> for a list of applications and supported file formats.</p><p xml:id="grl26774-para-0004">Additional file information is provided in the readme.txt.</p><supportingInfoItem><mediaResource alt="supplementary data" mimeType="text/plain" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0001-readme"></mediaResource><caption>readme.txt</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0002-ts01"></mediaResource><caption>Table S1. The Mann‐Kendall non‐parametric test for trends. Details of Mann‐Kendall test can be found from <link href="#grl26774-bib-0008"><i>Sahoo and Smith</i> [2009]</link>.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0003-ts02"></mediaResource><caption>Table S2. The Student's t‐test for three time periods.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" rendition="webOriginal" mimeType="image/tiff" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0004-fs01"></mediaResource><caption>Figure S1. Map of Salt Creek, Des Plaines River, Kankakee River, and Embarras River watersheds.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" rendition="webOriginal" mimeType="image/tiff" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0005-fs02"></mediaResource><caption>Figure S2. The mean winter temperature.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" rendition="webOriginal" mimeType="image/tiff" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0006-fs03"></mediaResource><caption>Figure S3. The mean summer temperature.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" rendition="webOriginal" mimeType="image/tiff" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0007-fs04"></mediaResource><caption>Figure S4. The annual precipitation, total precipitation in winter and summer season.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" rendition="webOriginal" mimeType="image/tiff" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0008-fs05"></mediaResource><caption>Figure S5. The surface water withdrawals vs. groundwater pumping in the part of the Kankakee watershed located in Indiana from 1985–2006.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="text/plain" href="urn-x:wiley:00948276:media:grl26774:grl26774-sup-0009-t01"></mediaResource><caption>Tab‐delimited Table 1.</caption></supportingInfoItem></supportingInformation><abstractGroup><abstract type="main"><p xml:id="grl26774-para-0005" label="1">This study explores the long‐term trends of low flow magnitude and the slopes and shapes of the recession curves during winter and summer seasons under climatic and human factors. Four watersheds in the American Midwest are selected for the analysis, including two urban watersheds (Salt Creek and Des Plaines) and two agricultural watersheds (Embarras and Kankakee). The results show that the long‐term baseflow recession slope trends in all the watersheds are primarily induced by human interferences. In the urban watersheds, the recession slopes decrease over time in both winter and summer due to effluent discharges. In the Kankakee watershed with irrigation, the recession slopes decrease in winter but increase in summer, and the opposite winter and summer trends are caused by the seasonal water use regime of irrigated agriculture. In the Embarras watershed with rainfed agriculture, the recession slopes decrease over time in winter but display no change in summer. Sources of water withdrawal (groundwater versus surface water) also have different impacts on the recession process. This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. Beyond the specific case studies, this paper documents how a scientific approach based on existing streamflow observation can be applied to improving our understanding of the impact of human and climatic influences on baseflow and low flow processes.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>BASEFLOW RECESSION SLOPE TREND</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds</title></titleInfo><name type="personal"><namePart type="given">Dingbao</namePart><namePart type="family">Wang</namePart><affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Ximing</namePart><namePart type="family">Cai</namePart><affiliation>Department of Civil and Environmental Engineering, University of Illinois at Urbana‐Champaign, Illinois, Urbana, USA</affiliation><affiliation>E-mail: xmcai@illinois.edu</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2010-03</dateIssued><dateCaptured encoding="w3cdtf">2009-11-23</dateCaptured><dateValid encoding="w3cdtf">2010-02-18</dateValid><edition>Wang, D., and X. Cai (2010), Comparative study of climate and human impacts on seasonal baseflow in urban and agricultural watersheds, Geophys. Res. Lett., 37, L06406, doi:10.1029/2009GL041879.</edition><copyrightDate encoding="w3cdtf">2010</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">2</extent><extent unit="tables">1</extent></physicalDescription><abstract>This study explores the long‐term trends of low flow magnitude and the slopes and shapes of the recession curves during winter and summer seasons under climatic and human factors. Four watersheds in the American Midwest are selected for the analysis, including two urban watersheds (Salt Creek and Des Plaines) and two agricultural watersheds (Embarras and Kankakee). The results show that the long‐term baseflow recession slope trends in all the watersheds are primarily induced by human interferences. In the urban watersheds, the recession slopes decrease over time in both winter and summer due to effluent discharges. In the Kankakee watershed with irrigation, the recession slopes decrease in winter but increase in summer, and the opposite winter and summer trends are caused by the seasonal water use regime of irrigated agriculture. In the Embarras watershed with rainfed agriculture, the recession slopes decrease over time in winter but display no change in summer. Sources of water withdrawal (groundwater versus surface water) also have different impacts on the recession process. This long‐term analysis of recession rates, in conjunction with the changes in low flow magnitude, offers valuable insight on human interferences to hydrologic processes. Beyond the specific case studies, this paper documents how a scientific approach based on existing streamflow observation can be applied to improving our understanding of the impact of human and climatic influences on baseflow and low flow processes.</abstract><subject><genre>keywords</genre><topic>baseflow recession slope</topic><topic>climate and human impacts</topic><topic>urban and agricultural watersheds</topic></subject><relatedItem type="host"><titleInfo><title>Geophysical Research Letters</title></titleInfo><titleInfo type="abbreviated"><title>Geophys. Res. Lett.</title></titleInfo><genre type="journal">journal</genre><note type="content"> Auxiliary material for this article contains includes 2 tables and 5 figures. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). See Plugins for a list of applications and supported file formats. Additional file information is provided in the readme.txt. Auxiliary material for this article contains includes 2 tables and 5 figures. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). See Plugins for a list of applications and supported file formats. Additional file information is provided in the readme.txt. Auxiliary material for this article contains includes 2 tables and 5 figures. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). See Plugins for a list of applications and supported file formats. Additional file information is provided in the readme.txt. Auxiliary material for this article contains includes 2 tables and 5 figures. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). See Plugins for a list of applications and supported file formats. Additional file information is provided in the readme.txt.Supporting Info Item: readme.txt - Table S1. The Mann‐Kendall non‐parametric test for trends. Details of Mann‐Kendall test can be found from . - Table S2. The Student's t‐test for three time periods. - Figure S1. Map of Salt Creek, Des Plaines River, Kankakee River, and Embarras River watersheds. - Figure S2. The mean winter temperature. - Figure S3. The mean summer temperature. - Figure S4. The annual precipitation, total precipitation in winter and summer season. - Figure S5. The surface water withdrawals vs. groundwater pumping in the part of the Kankakee watershed located in Indiana from 1985–2006. - Tab‐delimited Table 1. - </note><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/taxonomy5/1800">HYDROLOGY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1834">Human impacts</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1860">Streamflow</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1804">Catchment</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1807">Climate impacts</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4300">NATURAL HAZARDS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4323">Human impact</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4321">Climate impact</topic></subject><subject><genre>article-category</genre><topic>Hydrology and Land Surface Studies</topic></subject><identifier type="ISSN">0094-8276</identifier><identifier type="eISSN">1944-8007</identifier><identifier type="DOI">10.1002/(ISSN)1944-8007</identifier><identifier type="CODEN">GPRLAJ</identifier><identifier type="PublisherID">GRL</identifier><part><date>2010</date><detail type="volume"><caption>vol.</caption><number>37</number></detail><detail type="issue"><caption>no.</caption><number>6</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>6</total></extent></part></relatedItem><identifier type="istex">6FF25F8D163C9EEE9FCDED5C0989BA1F3B1E4934</identifier><identifier type="DOI">10.1029/2009GL041879</identifier><identifier type="ArticleID">2009GL041879</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2010 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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