Authors: Gopchenko E., Cheroy A.
Year: 2008
Issue: 06
Pages: 122-128
Abstract
The characteristics of temporal variability of current velocity and turbidity in Bystry branch has given. The quantitative estimation of short-term water runoff redistribution caused by wind denivellations has given for the first time. Recommendations concerning improvement of the received hydrological information has been developed.
Tags: Danube delta; flow velocity; turbidity; water runoff redistribution; wind denivellations
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