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Assessment of runoff in Chandra river basin of Western Himalaya using Remote Sensing and GIS Techniques
The runoff of Chandra river basin in the Himalayan India was assessed using a hydrological model combined with satellite remote sensing observations. During a test period between 2000 and 2015, in situ measurements of runoff and meteorological parameters were conducted in the glacial catchment areas...
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Published in: | Environmental monitoring and assessment 2022-03, Vol.194 (3), p.145-145, Article 145 |
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description | The runoff of Chandra river basin in the Himalayan India was assessed using a hydrological model combined with satellite remote sensing observations. During a test period between 2000 and 2015, in situ measurements of runoff and meteorological parameters were conducted in the glacial catchment areas of Sutridhaka and Chhotashigri. A good agreement was found between the observed and predicted runoff (correlation
R
2
> 0.8). The hydrological model was then used to simulate the runoff of Chandra River for a period of 2000 to 2015. Almost 68% of the predicted runoff occurred during the ablation period (May to September). A sensitivity study of the Chandra basin hydrology to a predicted warming climate of 1 to 4 K, toward the end of the century suggests that increased production of glacial melt water would have more impact on runoff than potential increase in precipitation. During the monsoon months (of June to August), increased runoff is predicted due to enhanced glacial melting but the runoff in other months to be lower than present mean runoff, except for the summer months (March to July). |
doi_str_mv | 10.1007/s10661-022-09795-y |
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R
2
> 0.8). The hydrological model was then used to simulate the runoff of Chandra River for a period of 2000 to 2015. Almost 68% of the predicted runoff occurred during the ablation period (May to September). A sensitivity study of the Chandra basin hydrology to a predicted warming climate of 1 to 4 K, toward the end of the century suggests that increased production of glacial melt water would have more impact on runoff than potential increase in precipitation. During the monsoon months (of June to August), increased runoff is predicted due to enhanced glacial melting but the runoff in other months to be lower than present mean runoff, except for the summer months (March to July).</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-022-09795-y</identifier><identifier>PMID: 35122167</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Ablation ; Atmospheric Protection/Air Quality Control/Air Pollution ; Catchment area ; Catchment areas ; Climate Change ; Climate prediction ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Environment ; Environmental Management ; Environmental Monitoring ; Environmental science ; Geographic Information Systems ; Geographical information systems ; Glacial runoff ; Glacier melting ; Global warming ; Hydrologic models ; Hydrology ; In situ measurement ; Meltwater ; Meteorological parameters ; Monitoring/Environmental Analysis ; Monsoon precipitation ; Monsoons ; Remote sensing ; Remote Sensing Technology ; River basins ; Rivers ; Runoff ; Satellite observation ; Snow</subject><ispartof>Environmental monitoring and assessment, 2022-03, Vol.194 (3), p.145-145, Article 145</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2022</rights><rights>2022. The Author(s), under exclusive licence to Springer Nature Switzerland AG.</rights><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c375t-eba8abb0dd212ea972a2ea14fb9544ac21cbfc54bb8d5739a30c506ced924ecc3</citedby><cites>FETCH-LOGICAL-c375t-eba8abb0dd212ea972a2ea14fb9544ac21cbfc54bb8d5739a30c506ced924ecc3</cites><orcidid>0000-0002-9400-1893</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2625417068/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2625417068?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,11667,27901,27902,36037,36038,44339,74638</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/35122167$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Gaddam, Vinay Kumar</creatorcontrib><creatorcontrib>Myneni, Tanooj Kumar</creatorcontrib><creatorcontrib>Kulkarni, Anil V.</creatorcontrib><creatorcontrib>Zhang, Yongqiang</creatorcontrib><title>Assessment of runoff in Chandra river basin of Western Himalaya using Remote Sensing and GIS Techniques</title><title>Environmental monitoring and assessment</title><addtitle>Environ Monit Assess</addtitle><addtitle>Environ Monit Assess</addtitle><description>The runoff of Chandra river basin in the Himalayan India was assessed using a hydrological model combined with satellite remote sensing observations. During a test period between 2000 and 2015, in situ measurements of runoff and meteorological parameters were conducted in the glacial catchment areas of Sutridhaka and Chhotashigri. A good agreement was found between the observed and predicted runoff (correlation
R
2
> 0.8). The hydrological model was then used to simulate the runoff of Chandra River for a period of 2000 to 2015. Almost 68% of the predicted runoff occurred during the ablation period (May to September). A sensitivity study of the Chandra basin hydrology to a predicted warming climate of 1 to 4 K, toward the end of the century suggests that increased production of glacial melt water would have more impact on runoff than potential increase in precipitation. During the monsoon months (of June to August), increased runoff is predicted due to enhanced glacial melting but the runoff in other months to be lower than present mean runoff, except for the summer months (March to July).</description><subject>Ablation</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Catchment area</subject><subject>Catchment areas</subject><subject>Climate Change</subject><subject>Climate prediction</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental Monitoring</subject><subject>Environmental science</subject><subject>Geographic Information Systems</subject><subject>Geographical information systems</subject><subject>Glacial runoff</subject><subject>Glacier melting</subject><subject>Global warming</subject><subject>Hydrologic models</subject><subject>Hydrology</subject><subject>In situ measurement</subject><subject>Meltwater</subject><subject>Meteorological parameters</subject><subject>Monitoring/Environmental Analysis</subject><subject>Monsoon precipitation</subject><subject>Monsoons</subject><subject>Remote sensing</subject><subject>Remote Sensing Technology</subject><subject>River basins</subject><subject>Rivers</subject><subject>Runoff</subject><subject>Satellite observation</subject><subject>Snow</subject><issn>0167-6369</issn><issn>1573-2959</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>M0C</sourceid><recordid>eNp9kUtLxDAUhYMozvj4Ay4k4MZNNUmbdLKUQccBQdARlyFJb8cObapJK_Tfm7E-wIWrS3K-c29uDkInlFxQQvLLQIkQNCGMJUTmkifDDppSnqcJk1zuoimhIk9EKuQEHYSwISRimdxHk5RTxqI4ReurECCEBlyH2xL73rVliSuH5y_aFV5jX72Dx0aHeBeBZwgdeIdvq0bXetC4j8IaP0DTdoAfwX0eoxUvlo94BfbFVW89hCO0V-o6wPFXPURPN9er-W1yd79Yzq_uEpvmvEvA6Jk2hhQFowy0zJmOhWalkTzLtGXUmtLyzJhZEReVOiWWE2GhkCwDa9NDdD72ffXtdm6nmipYqGvtoO2DYoIJQjiXWUTP_qCbtvcuvm5L8YzmRMwixUbK-jYED6V69XF3PyhK1DYGNcagYgzqMwY1RNPpV-veNFD8WL7_PQLpCIQouTX439n_tP0ARnWUNw</recordid><startdate>20220301</startdate><enddate>20220301</enddate><creator>Gaddam, Vinay Kumar</creator><creator>Myneni, Tanooj Kumar</creator><creator>Kulkarni, Anil V.</creator><creator>Zhang, Yongqiang</creator><general>Springer International Publishing</general><general>Springer 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of runoff in Chandra river basin of Western Himalaya using Remote Sensing and GIS Techniques</title><author>Gaddam, Vinay Kumar ; Myneni, Tanooj Kumar ; Kulkarni, Anil V. ; Zhang, Yongqiang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c375t-eba8abb0dd212ea972a2ea14fb9544ac21cbfc54bb8d5739a30c506ced924ecc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Ablation</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Catchment area</topic><topic>Catchment areas</topic><topic>Climate Change</topic><topic>Climate prediction</topic><topic>Earth and Environmental Science</topic><topic>Ecology</topic><topic>Ecotoxicology</topic><topic>Environment</topic><topic>Environmental Management</topic><topic>Environmental Monitoring</topic><topic>Environmental science</topic><topic>Geographic Information Systems</topic><topic>Geographical information 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Academic</collection><jtitle>Environmental monitoring and assessment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gaddam, Vinay Kumar</au><au>Myneni, Tanooj Kumar</au><au>Kulkarni, Anil V.</au><au>Zhang, Yongqiang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Assessment of runoff in Chandra river basin of Western Himalaya using Remote Sensing and GIS Techniques</atitle><jtitle>Environmental monitoring and assessment</jtitle><stitle>Environ Monit Assess</stitle><addtitle>Environ Monit Assess</addtitle><date>2022-03-01</date><risdate>2022</risdate><volume>194</volume><issue>3</issue><spage>145</spage><epage>145</epage><pages>145-145</pages><artnum>145</artnum><issn>0167-6369</issn><eissn>1573-2959</eissn><abstract>The runoff of Chandra river basin in the Himalayan India was assessed using a hydrological model combined with satellite remote sensing observations. During a test period between 2000 and 2015, in situ measurements of runoff and meteorological parameters were conducted in the glacial catchment areas of Sutridhaka and Chhotashigri. A good agreement was found between the observed and predicted runoff (correlation
R
2
> 0.8). The hydrological model was then used to simulate the runoff of Chandra River for a period of 2000 to 2015. Almost 68% of the predicted runoff occurred during the ablation period (May to September). A sensitivity study of the Chandra basin hydrology to a predicted warming climate of 1 to 4 K, toward the end of the century suggests that increased production of glacial melt water would have more impact on runoff than potential increase in precipitation. During the monsoon months (of June to August), increased runoff is predicted due to enhanced glacial melting but the runoff in other months to be lower than present mean runoff, except for the summer months (March to July).</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>35122167</pmid><doi>10.1007/s10661-022-09795-y</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-9400-1893</orcidid></addata></record> |
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subjects | Ablation Atmospheric Protection/Air Quality Control/Air Pollution Catchment area Catchment areas Climate Change Climate prediction Earth and Environmental Science Ecology Ecotoxicology Environment Environmental Management Environmental Monitoring Environmental science Geographic Information Systems Geographical information systems Glacial runoff Glacier melting Global warming Hydrologic models Hydrology In situ measurement Meltwater Meteorological parameters Monitoring/Environmental Analysis Monsoon precipitation Monsoons Remote sensing Remote Sensing Technology River basins Rivers Runoff Satellite observation Snow |
title | Assessment of runoff in Chandra river basin of Western Himalaya using Remote Sensing and GIS Techniques |
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