Influencia del intercambio térmico a través del fondo marino en el régimen de temperatura de Zonas Costeras
DOI:
https://doi.org/10.26640/22159045.78Keywords:
Thermical interaction, MECCA, hydrodynamicAbstract
The solution of the hydrodynamic problems with the MECA (Model For Estuarine and Coastal Circulation Assessment) model requires the determination of thermical boundary conditions al the bottom.
The authors have carried out an estimation of the possibilities of utilization of several boundary conditions at the bottom. In particular, formulation of coupled model for thermical interaction between the sediment and water column is discussed.
Results of mis work show a practical equivalence between the first type boundary condition and the coupled problem for the shallow water dynamics.
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References
Hess, K. W. (1989): MECC.A Programs Documentation. NOAA Technical Report NESDIS 46, Washington, D C.
Marchuk, G.I., and B. A. Kagán. (1991): Dynamics of Ocean Tidesd. Leningrad, Gidrometeoizdat, 472 p. (in Russsian)
Sukhorukov, V. A., N. V. Dmitriev, and S. M. Likhachov. (1986): Simulation of the Ocean Mixed Layer. Preprint 675, Computer Centre of the Academy of Sciences of the USSR, Novosibirsk, Russia, 24 p. (in Russian).
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