Hydropower: Hydroelectric Power Generation from Alpine Glacier Melt
Reference work entry
First Online:
DOI: https://doi.org/10.1007/978-90-481-2642-2_624
Definition and introduction
Alpine glaciers act as natural reservoirs storing water in a frozen state instead of behind a dam. Glacier’s modify streamflow releasing the most runoff during the warmest, driest periods when all other sources of water for hydropower are at a minimum (Stenborg,
1970; Fountain and Tanborn,
1985). This seasonal variation characteristic mitigates low flow intervals and the dependability helps make glacier runoff a valuable water resource for hydropower (Fountain and Tangborn,
1985). Annual glacier runoff is highest in warm, dry summers and lowest during wet, cool summers, further providing a balance to alpine summer runoff, this is the glacier compensation effect (Lang,
1986). Dependable and consistent glacier runoff allows for run of river hydropower and smaller reservoir storage in glaciated basins. For long range planning minimum flows are greater and maximum flows less in glacier fed basins (Fountain and Tangborn,
1985). At the same time that glacier...
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