## Abstract Backflow from the Yangtze River to Poyang Lake occurs frequently due to their different flood seasons. Based on the reasons for and time period of backflow, this study estimated the spatialβtemporal extent and the change of water clarity influenced by sediments within the backflow and n
β¦ LIBER β¦
Use of Water Clarity to Monitor the Effects of Climate Change and other Stressors on Oligotrophic Lakes
β Scribed by John M. Gunn; Ed Snucins; Norman D. Yan; Michael T. Arts
- Book ID
- 110235406
- Publisher
- Springer
- Year
- 2001
- Tongue
- English
- Weight
- 174 KB
- Volume
- 67
- Category
- Article
- ISSN
- 0167-6369
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