Simulación de la circulación en la Bahía de Campeche
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Abstract
A non-linear reduce gravity model is used for the study of the circulation in the Bay of Campeche. The equations of the model are solved numerically on a staggered uniform grid of 30 km resolution. Data on the inflow-outflow through the Yucatan Channel and Florida Strait were imposed as boundary conditions. Results indicated the presence of cyclonic eddies in the Bay of Campeche with a westward propagation.
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Monreal Gómez, M. A., & Salas de León, D. A. (1990). Simulación de la circulación en la Bahía de Campeche. Geofisica Internacional, 29(2), 101–111. https://doi.org/10.22201/igeof.00167169p.1990.29.2.791
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