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http://117.252.14.250:8080/jspui/handle/123456789/6036
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DC Field | Value | Language |
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dc.contributor.author | Meetei, Prikash N. | - |
dc.contributor.author | Ahluwalia, Rajeev Saran | - |
dc.contributor.author | Rai, S. P. | - |
dc.contributor.author | Khobragade, S. D. | - |
dc.contributor.author | Sarangi, Shushanta | - |
dc.contributor.author | Goel, M. K. | - |
dc.contributor.author | Kumar, Sushil | - |
dc.date.accessioned | 2021-06-14T14:49:42Z | - |
dc.date.available | 2021-06-14T14:49:42Z | - |
dc.date.issued | 2020 | - |
dc.identifier.citation | Geocarto International | en_US |
dc.identifier.uri | http://117.252.14.250:8080/jspui/handle/123456789/6036 | - |
dc.description.abstract | Continuous monitoring of snow cover area (SCA) in space and time is a vital input to estimate the snow/glacier melt runoff, glacial mass balance and other hydrological studies. The present study aims to find out the spatio-temporal variation of SCA and inter-relationship between snow accumulation and topography in the Upper Ganga River Basin (UGRB) including Bhagirathi, Alaknanda, Mandakini and Pindar River sub-basins, central Himalaya using MODIS Terra (MOD10A2) data. SCA is found 32.33% to the total basin area of 18724km2 in UGRB. The Average of 12 year shows that Bhagirathi River Basin has maximum SCA 33.25%, whereas Pindar river basin has minimum SCA 17.50% among these four sub-basins. Maximum rate of change of SCA is found in the Mandakini River Basin. Slope class 20 –30 has more favorable conditions for snow accumulation. North and north-west aspect has higher snow accumulation with maximum positive attribution in January and minimum in July. | en_US |
dc.language.iso | en | en_US |
dc.publisher | Taylor & Francis | en_US |
dc.subject | Snow cover | en_US |
dc.subject | Elevation | en_US |
dc.subject | Slope | en_US |
dc.subject | Aspect | en_US |
dc.subject | MODIS | en_US |
dc.subject | Upper Ganga River Basin | en_US |
dc.title | Spatio-temporal analysis of snow cover and effect of terrain attributes in the Upper Ganga River Basin, central Himalaya | en_US |
dc.type | Article | en_US |
Appears in Collections: | Research papers in International Journals |
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