The dynamics of different regimes in an ice covered inland lake with through-flow are discussed. A new theory for selective withdrawal is tested with success. The mixing of the entering river with lake water is estimated and it is found that the net volume flux increases with about 60% through the mixing. The flow in the main part of the lake is discussed and some measurements are presented.
Research Article|June 01 1978
Anders Stigebrandt; Dynamics of an Ice Covered Lake with Through-Flow. Hydrology Research 1 June 1978; 9 (3-4): 219–244. doi: https://doi.org/10.2166/nh.1978.0023
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