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M. L. ARGOTE ESPINOSA,M. F. LAVÍN,A. AMADOR
A vertically integrated, non-linear numerical model in finite differences is used to analyze two forcing mechanisms of the mean barotropic circulation in the Gulf of California: topographic rectification due to tidal currents (M2) and wind stress. Un...
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E. PALACIOS HERNÁNDEZ,M. L. ARGOTE ESPINOSA,A. AMADOR BUENROSTRO,M. MANCILLA PERAZA
A bidimensional numerical model is used to simulate and to establish the most important mechanism that controls Sebastian Vizcaino Bay B.C. barotropic circulation. The observed circulation patterns were reproduced by the model; in particular anticyclonic...
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M. L. ARGOTE ESPINOSA,F. J. GAVIDIA MEDINA,A. AMADOR BUENROSTRO
A hydrodynamical numerical model is used to predict the wind-induced circulation in Todos Santos Bay for wind conditions representative of summer, winter and the aperiodic westerly "Santana" winds. Maximum velocities along the coast and return flows ...
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