Degree–day factors for snow and ice for Dokriani Glacier, Garhwal Himalayas
- 22 August 2000
- journal article
- Published by Elsevier BV in Journal of Hydrology
- Vol. 235 (1-2), 1-11
- https://doi.org/10.1016/s0022-1694(00)00249-3
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Effect of orography on precipitation in the western Himalayan regionJournal of Hydrology, 1997
- Impact assessment of climate change on the hydrological response of a snow and glacier melt runoff dominated Himalayan riverJournal of Hydrology, 1997
- Estimation of Snow and Glacier-Melt Contribution to the Chenab River, Western HimalayaMountain Research and Development, 1997
- Determination of snowmelt factor in the Himalayan regionHydrological Sciences Journal, 1996
- Hydrological characteristics of the Dokriani Glacier in the Garhwal HimalayasHydrological Sciences Journal, 1995
- Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modellingJournal of Glaciology, 1995
- Sensitivity to climate change of the mass balance of glaciers in southern NorwayJournal of Glaciology, 1993
- Reconstruction of Mass Balance Variations for Franz Josef Glacier, New Zealand, 1913 to 1989Arctic and Alpine Research, 1992
- On Glacier Energy Balance, Ablation, and Air TemperatureJournal of Glaciology, 1981
- Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, NepalJournal of Glaciology, 1979