Glacier Drainage Evolution and Control on Suspended Sediment Concentration in Meltwater, Dokriani Glacier, Garhwal Himalaya, India

Authors

  • Wadia Institute of Himalayan Geology, Dehra Dun - 248 001
  • Wadia Institute of Himalayan Geology, Dehra Dun - 248 001
  • Wadia Institute of Himalayan Geology, Dehra Dun - 248 001

Abstract

Discharge, electrical conductivity and suspended sediment concentrations of Dokriani glacial meltwater were observed from 8 May to 31 October 1994. The comprehensive database on hydrological parameters of an Indian Himalayan glacier so obtained suggests a close relationship between suspended sediment transfer characteristics and glacier drainage evolution during the 1994 ablation period.

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Short Communications

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Published

2003-08-01

How to Cite

Thayyen, R. J., Gergan, J. T., & Dobhal, D. P. (2003). Glacier Drainage Evolution and Control on Suspended Sediment Concentration in Meltwater, Dokriani Glacier, Garhwal Himalaya, India. Journal of Geological Society of India, 62(2), 237–242. Retrieved from http://www.geosocindia.com/index.php/jgsi/article/view/83223

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