Project Completion Report Ionic Enrichment Dynamics of Glacial Sediment and Meltwater of Gangotri Glacier (DST-SERB No. SB/DGH-49/2013 dated 13.01.2014)

dc.contributor.author	Sharma, M. K.
dc.date.accessioned	2020-08-28T14:41:37Z
dc.date.available	2020-08-28T14:41:37Z
dc.date.issued	2017
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/4709
dc.description.abstract	One of the major findings of the study is that River Bhagirathi remains under closed system conditions from its origin at Gomukh to 14 km downstream at Gangotri, in which high p(CO2) closed system conditions dominates. The sediment concentration and subglacial activities play a major role in this process and influence of glacier system extend to downstream reaches as well.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Gangotri Glacier	en_US
dc.subject	Ganga plain catchments	en_US
dc.subject	Glacier meltwater	en_US
dc.title	Project Completion Report Ionic Enrichment Dynamics of Glacial Sediment and Meltwater of Gangotri Glacier (DST-SERB No. SB/DGH-49/2013 dated 13.01.2014)	en_US
dc.type	Technical Report	en_US