Tidal models of the Mediterranean sea
In order to evaluate the vertical displacement of the Sea Surface Topography due to the ocean tides, we have made the modeling of the four main constituents M2, 52, 01 and Kl for the whole Mediterranean Sea and the local model N2 corresponding to the western area. This paper concludes with a brief d...
| Autores: | , , |
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| Tipo de recurso: | capítulo de libro |
| Fecha de publicación: | 1994 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | inglés |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/60639 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/60639 |
| Access Level: | acceso abierto |
| Palabra clave: | 528 Geodesia Geomed Mediterráneo Mareas 2504 Geodesia |
| Sumario: | In order to evaluate the vertical displacement of the Sea Surface Topography due to the ocean tides, we have made the modeling of the four main constituents M2, 52, 01 and Kl for the whole Mediterranean Sea and the local model N2 corresponding to the western area. This paper concludes with a brief discussion of some results of the computed surface tide. |
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