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Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/8039
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dc.contributor.authorHans, Darshan-
dc.contributor.authorUnder the Guidance of Arora, Manohar-
dc.date.accessioned2026-07-29T11:44:53Z-
dc.date.available2026-07-29T11:44:53Z-
dc.date.issued2017-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/8039-
dc.description.abstractA glacier is a persistent body of dense ice that is constantly moving under its own weight. It forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries (Cuffy and Paterson, 2010). Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, cirques, and other distinguishing features. The movement may be as little as few centimeters a day to much larger or faster.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectHydrological Modellingen_US
dc.subjectStreamflowen_US
dc.subjectGlacieren_US
dc.subjectCentral Himalayaen_US
dc.title61-A Dissertation Report on Hydrological Modelling of Streamflow in the Glacerized Catchment of Central Himalaya (Uttarakhand, India).en_US
dc.typeTechnical Reporten_US
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