Simulación de la circulación en la Bahía de Campeche
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 con...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1990 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/1044 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1044 |
| Access Level: | acceso abierto |
| Palabra clave: | Bahía de Campeche Giros ciclónicos Modelos numéricos Bay of Campeche Cyclonic eddies Numerical modelling |
| Sumario: | 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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