A new method for estimating the seasonal cycle of the heat balance at the ocean surface, with application to the Gulf of Mexico
The conservation of thermal energy applied to the upper layer of the ocean is used together with parameterizations of the heating and transport terms in order to simulate the sea surface temperature, the annual cycle of the radiation balance, the latent and sensible heat fluxes and the rate of ocean...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1993 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/1345 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1345 |
| Access Level: | acceso abierto |
| Palabra clave: | Golfo de México Simula Balance de radiación Calor latente Calor sensible Balance de calor océanico Gulf of Mexico Simulate Radiation balance Latent heat Sensible heat Oceanic heat storage |
| Sumario: | The conservation of thermal energy applied to the upper layer of the ocean is used together with parameterizations of the heating and transport terms in order to simulate the sea surface temperature, the annual cycle of the radiation balance, the latent and sensible heat fluxes and the rate of oceanic heat storage in the Gulf of Mexico. The results are compared with those obtained by other authors. |
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