Annotation
Results are presented on bottom density flows under natural conditions; vertical distributions have been derived for the density, turbidity, mean velocity, scale of the fluctuations in the two flow-speed components, and the turbulent frictional stress. It is concluded that the mechanism of the flow near the bottom is similar to the mechanism for the liquid boundary of the bottom density flow. Although the results are in qualitative agreement with published data, there are substantial quantitative discrepancies over the major turbulent characteristics.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
A.A. Kuznetsov, Yu.G. Pyrkin, and L.V. Sokolov
Кафедра физики моря и вод суши
Кафедра физики моря и вод суши