## Abstract Replacement of water in a given hydrological component is one of the effects of the hydrological cycle. We introduce the concept of renewal time to express the rate of water replacement in a specific reach of a river. Based on streamβflow data from the 1990s, a simple formula is used to
Scheme of using the Middle Enisei and Lower Angara rivers
β Scribed by L. P. Mikhailov; T. P. Dotsenko; E. A. Smirnov; L. M. Shtaier
- Publisher
- Springer
- Year
- 1985
- Tongue
- English
- Weight
- 748 KB
- Volume
- 19
- Category
- Article
- ISSN
- 1570-1468
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