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- W4312708045 abstract "The meltwater runoff characteristics of the glacierized basins are different from those of purely rain-fed basins. Understanding the hydrological response of Himalayan glaciers, where significant rainfall occurs in addition to snow and glaciers, becomes very complex. Large variability has been observed in the meteorological conditions over glacierized regions, with rainfall being the most variable. Meltwater runoff from snow and glaciers is the most important source of runoff for mountain streams during the early ablation season (May and June). The discharge from the glacierized basins is highly regulated by the drainage and meltwater storage characteristics of the glacier. The interannual variability in the discharge for the glaciers is low as compared to the diurnal variability. The availability of dependable flows and suitable heads provides excellent conditions for hydropower generation and has resulted in extensive development of hydropower projects in the Himalaya. However, still, a large potential is yet to be harnessed in Uttarakhand (~ 70%) and other Himalayan states. To develop this potential under the threat of frequent disasters in the state and the absence of hydrometeorological data in glacierized basins, integrated continuous long-term monitoring of glaciers is essential." @default.
- W4312708045 created "2023-01-05" @default.
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- W4312708045 date "2022-01-01" @default.
- W4312708045 modified "2023-10-11" @default.
- W4312708045 title "Hydrological importance of Himalayan glaciers: A perspective from Garhwal Himalaya" @default.
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- W4312708045 doi "https://doi.org/10.1016/b978-0-323-85378-1.00028-3" @default.
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