## Abstract During the snowmelt season, surface runoff into northern Canadian Shield lakes is governed by the distribution of snow and its ablation, storage in catchment slopes and valleys, and flow delivery from uplands, bottomlands and from upper lakes. For the lake studied, time lags exist betwe
โฆ LIBER โฆ
Slope runoff processes and flow generation in a subarctic, subalpine catchment
โ Scribed by Sean K. Carey; Ming-ko Woo
- Book ID
- 117138463
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 374 KB
- Volume
- 253
- Category
- Article
- ISSN
- 0022-1694
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