## Abstract River flow from glacierized areas in the Himalaya is influenced both by intra‐annual variations in precipitation and energy availability, and by longer term changes in storage of water as glacier ice. High specific discharge from ice melt often dominates flow for considerable distances
Limits of warm and cold bioclimatic stress in different climatic regions
✍ Scribed by K. Zaninović
- Publisher
- Springer
- Year
- 1992
- Tongue
- English
- Weight
- 547 KB
- Volume
- 45
- Category
- Article
- ISSN
- 1434-4483
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