The near-bottom boundary layer in the black sea: Hydrological structure and modelling

The near-bottom boundary layer in the black sea: Hydrological structure and modelling The paper discusses the parameters derived through deep-sea precision CTD-probings, characteristic of the structure of the near-bottom boundaries layer, specifically, the depth of the layer's upper boundary and the mean vertical potential temperature/salinity gradients, as well as the density ratio over the layer of the near-bottom convection. The peculiarities of the parameters' spatial distribution have been identified. The conclusion derived from the analysis of the model implies that the near-bottom boundary layer occurs, aside from the presence of the bottom geothermal heat flux, due to the strong dependence of the Bosphorus salt flux on stratification. The dependence of the Black Sea buoyancy flux and vertical diffusion coefficient on depth has been estimated. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Physical Oceanography Springer Journals

The near-bottom boundary layer in the black sea: Hydrological structure and modelling

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Publisher
Kluwer Academic Publishers
Copyright
Copyright © 1998 by VSP
Subject
Earth Sciences; Oceanography; Remote Sensing/Photogrammetry; Atmospheric Sciences; Climate Change; Environmental Physics
ISSN
0928-5105
eISSN
0928-5105
D.O.I.
10.1007/BF02525515
Publisher site
See Article on Publisher Site

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