61-A Dissertation Report on Hydrological Modelling of Streamflow in the Glacerized Catchment of Central Himalaya (Uttarakhand, India).

Hans, Darshan; Under the Guidance of Arora, Manohar

dc.contributor.author	Hans, Darshan
dc.contributor.author	Under the Guidance of Arora, Manohar
dc.date.accessioned	2026-07-29T11:44:53Z
dc.date.available	2026-07-29T11:44:53Z
dc.date.issued	2017
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/8039
dc.description.abstract	A 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.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Hydrological Modelling	en_US
dc.subject	Streamflow	en_US
dc.subject	Glacier	en_US
dc.subject	Central Himalaya	en_US
dc.title	61-A Dissertation Report on Hydrological Modelling of Streamflow in the Glacerized Catchment of Central Himalaya (Uttarakhand, India).	en_US
dc.type	Technical Report	en_US