A Model of the Sevastopol'skaya Bay. Reproduction of the Vertical Structure of Temperature and Salinity Fields in 1997–1999

A Model of the Sevastopol'skaya Bay. Reproduction of the Vertical Structure of Temperature and... We discuss the results of a numerical experiment carried out within the framework of the most complete one-dimensional (integrated over the horizontal coordinates) version of the quasiisopycnic multilayer model taking into account the processes of diapycnic mass, heat, and salt exchange and the diffusion coefficients chosen according to the theory of double diffusion. The indicated experiment reproduces the vertical thermohaline structure of waters in the Sevastopol'skaya Bay and its variability in 1997–1999. For numerical computations, we use the actual data of meteorological observations and measurements of the discharge of the river Chernaya and the sea level. The comparison of the numerical results with the data of monthly hydrological surveys reveals their good agreement (not only qualitative but also quantitative). http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Physical Oceanography Springer Journals

A Model of the Sevastopol'skaya Bay. Reproduction of the Vertical Structure of Temperature and Salinity Fields in 1997–1999

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Publisher
Kluwer Academic Publishers-Plenum Publishers
Copyright
Copyright © 2003 by Plenum Publishing Corporation
Subject
Earth Sciences; Oceanography; Remote Sensing/Photogrammetry; Atmospheric Sciences; Climate Change; Environmental Physics
ISSN
0928-5105
eISSN
0928-5105
D.O.I.
10.1023/A:1025850016768
Publisher site
See Article on Publisher Site

Abstract

We discuss the results of a numerical experiment carried out within the framework of the most complete one-dimensional (integrated over the horizontal coordinates) version of the quasiisopycnic multilayer model taking into account the processes of diapycnic mass, heat, and salt exchange and the diffusion coefficients chosen according to the theory of double diffusion. The indicated experiment reproduces the vertical thermohaline structure of waters in the Sevastopol'skaya Bay and its variability in 1997–1999. For numerical computations, we use the actual data of meteorological observations and measurements of the discharge of the river Chernaya and the sea level. The comparison of the numerical results with the data of monthly hydrological surveys reveals their good agreement (not only qualitative but also quantitative).

Journal

Physical OceanographySpringer Journals

Published: Oct 20, 2004

References

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