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TR-170 : Hydrological studies on Dokriani glacier in Garhwal Himalayas

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dc.contributor.author Singh, Pratap
dc.date.accessioned 2019-04-09T11:10:25Z
dc.date.available 2019-04-09T11:10:25Z
dc.date.issued 1992
dc.identifier.uri http://117.252.14.250:8080/xmlui/handle/123456789/1283
dc.description.abstract All the northern rivers of India are perennial due to regulation by snowmelt and glacier melt runoff. It may set new hydroelectric generators supplying cheap an plentiful electricity. An assessment of the water equivalent of the melting snow pack and the determination of drainage characteristics of various glaciers in the high mountains have importance for regulating the Himalayan river systems for greater hydroelectric power generation, irrigation and other benefits. In the present report hydrological studies carried out at Dokriani glacier has been presented. The data on flow, suspended sediment and computed time lag between melting and its appearance in the melt stream is reported. It also includes the general characteristics of the Dokriani glacier. en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.relation.ispartofseries ;TR-170
dc.subject Dokriani glacier en_US
dc.subject Dokriani glacier - Hydrological studies en_US
dc.title TR-170 : Hydrological studies on Dokriani glacier in Garhwal Himalayas en_US
dc.type Technical Report en_US


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