Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/1283
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dc.contributor.authorSingh, Pratap-
dc.date.accessioned2019-04-09T11:10:25Z-
dc.date.available2019-04-09T11:10:25Z-
dc.date.issued1992-
dc.identifier.urihttp://117.252.14.250:8080/xmlui/handle/123456789/1283-
dc.description.abstractAll 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.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.relation.ispartofseries;TR-170-
dc.subjectDokriani glacieren_US
dc.subjectDokriani glacier - Hydrological studiesen_US
dc.titleTR-170 : Hydrological studies on Dokriani glacier in Garhwal Himalayasen_US
dc.typeTechnical Reporten_US
Appears in Collections:Technical Reports

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