Mare Nostrum: geomed report - 2
GEOMED is a project for the determination of the geoid and of the Sea Surface Topography in the Mediterranean Sea. The existing set of data available on the Mediterranean in already quite significant and it is going to be improved in these years because of the new altimetric data coming from ERS1 an...
| Autores: | , , , , , , , , , , , , , , , , , , , , |
|---|---|
| Tipo de recurso: | libro |
| Fecha de publicación: | 1992 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | inglés |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/61191 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/61191 |
| Access Level: | acceso abierto |
| Palabra clave: | 528 Mareas Mediterráneo Geoide Geofísica Geodesia 2504 Geodesia |
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Mare Nostrum: geomed report - 2Sevilla De Lerma, Miguel JesúsBrovelli, M. A.Sanso, F.Arabelos, D.Spatalas, S. D.Tziavos, I. N.Rodríguez Caderot, GraciaGil, AlejandroVieira, RicardoToro Y Llaca, María Del CarmenFürst, W.Hausleitner, W.Höck, E.Schuh, W. D.Sünkel, H.Tscherning, C. C.Seierup, M. S.Knudsen, PerVermeer, MartinAndreu, M. A.Simó, C.528MareasMediterráneoGeoideGeofísicaGeodesia2504 GeodesiaGEOMED is a project for the determination of the geoid and of the Sea Surface Topography in the Mediterranean Sea. The existing set of data available on the Mediterranean in already quite significant and it is going to be improved in these years because of the new altimetric data coming from ERS1 and the TOPEX-POSEIDON missions. In the execution of the project we use, mainly, radar altimetric data (f rom SEASAT, GEOSAT and ESR1 missions) gravimetrie data, bathymetric models, as well as land gravi ty data set and DTMs of surrounding regions: these data sets are generally poor on the southern side of the Mediterranean. More geophysical data, like tidal and Moho depth models, will be user too. The partieularity of this projeet is in that the dynamics of the Mediterranean, as a elosed sea, eannot be easily modelled, so that the time dependent part of the altimetric signal has to be modelled empirically together wi th the radial orbi terror; on the other hand, sinee the satellite ares are very short, this choice is well justified. The separation between the stationary Sea Surface Topography and the geoid can be done in such an area using both data sets, the altimetric and the gravimetric one, whieh is available eontrary to the situation in open oceanic areas. This volume, the second of the MARE NOSTRUM Series, eolleet the works done by many groups involved in the GEOMED organization, in the last year, as informed in the GEOMED Meeting held in Madrid at october 1992, and will be followed by others with new contributions.Instituto de Astronomía y Geodesia (IAG-CSIC-UCM)Universidad Complutense de Madrid19921992-01-0119921992-01-01bookhttp://purl.org/coar/resource_type/c_2f33info:eu-repo/semantics/bookapplication/pdfhttps://hdl.handle.net/20.500.14352/61191reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/611912026-06-02T12:44:21Z |
| dc.title.none.fl_str_mv |
Mare Nostrum: geomed report - 2 |
| title |
Mare Nostrum: geomed report - 2 |
| spellingShingle |
Mare Nostrum: geomed report - 2 Sevilla De Lerma, Miguel Jesús 528 Mareas Mediterráneo Geoide Geofísica Geodesia 2504 Geodesia |
| title_short |
Mare Nostrum: geomed report - 2 |
| title_full |
Mare Nostrum: geomed report - 2 |
| title_fullStr |
Mare Nostrum: geomed report - 2 |
| title_full_unstemmed |
Mare Nostrum: geomed report - 2 |
| title_sort |
Mare Nostrum: geomed report - 2 |
| dc.creator.none.fl_str_mv |
Sevilla De Lerma, Miguel Jesús Brovelli, M. A. Sanso, F. Arabelos, D. Spatalas, S. D. Tziavos, I. N. Rodríguez Caderot, Gracia Gil, Alejandro Vieira, Ricardo Toro Y Llaca, María Del Carmen Fürst, W. Hausleitner, W. Höck, E. Schuh, W. D. Sünkel, H. Tscherning, C. C. Seierup, M. S. Knudsen, Per Vermeer, Martin Andreu, M. A. Simó, C. |
| author |
Sevilla De Lerma, Miguel Jesús |
| author_facet |
Sevilla De Lerma, Miguel Jesús Brovelli, M. A. Sanso, F. Arabelos, D. Spatalas, S. D. Tziavos, I. N. Rodríguez Caderot, Gracia Gil, Alejandro Vieira, Ricardo Toro Y Llaca, María Del Carmen Fürst, W. Hausleitner, W. Höck, E. Schuh, W. D. Sünkel, H. Tscherning, C. C. Seierup, M. S. Knudsen, Per Vermeer, Martin Andreu, M. A. Simó, C. |
| author_role |
author |
| author2 |
Brovelli, M. A. Sanso, F. Arabelos, D. Spatalas, S. D. Tziavos, I. N. Rodríguez Caderot, Gracia Gil, Alejandro Vieira, Ricardo Toro Y Llaca, María Del Carmen Fürst, W. Hausleitner, W. Höck, E. Schuh, W. D. Sünkel, H. Tscherning, C. C. Seierup, M. S. Knudsen, Per Vermeer, Martin Andreu, M. A. Simó, C. |
| author2_role |
author author author author author author author author author author author author author author author author author author author author |
| dc.contributor.none.fl_str_mv |
Universidad Complutense de Madrid |
| dc.subject.none.fl_str_mv |
528 Mareas Mediterráneo Geoide Geofísica Geodesia 2504 Geodesia |
| topic |
528 Mareas Mediterráneo Geoide Geofísica Geodesia 2504 Geodesia |
| description |
GEOMED is a project for the determination of the geoid and of the Sea Surface Topography in the Mediterranean Sea. The existing set of data available on the Mediterranean in already quite significant and it is going to be improved in these years because of the new altimetric data coming from ERS1 and the TOPEX-POSEIDON missions. In the execution of the project we use, mainly, radar altimetric data (f rom SEASAT, GEOSAT and ESR1 missions) gravimetrie data, bathymetric models, as well as land gravi ty data set and DTMs of surrounding regions: these data sets are generally poor on the southern side of the Mediterranean. More geophysical data, like tidal and Moho depth models, will be user too. The partieularity of this projeet is in that the dynamics of the Mediterranean, as a elosed sea, eannot be easily modelled, so that the time dependent part of the altimetric signal has to be modelled empirically together wi th the radial orbi terror; on the other hand, sinee the satellite ares are very short, this choice is well justified. The separation between the stationary Sea Surface Topography and the geoid can be done in such an area using both data sets, the altimetric and the gravimetric one, whieh is available eontrary to the situation in open oceanic areas. This volume, the second of the MARE NOSTRUM Series, eolleet the works done by many groups involved in the GEOMED organization, in the last year, as informed in the GEOMED Meeting held in Madrid at october 1992, and will be followed by others with new contributions. |
| publishDate |
1992 |
| dc.date.none.fl_str_mv |
1992 1992-01-01 1992 1992-01-01 |
| dc.type.none.fl_str_mv |
book http://purl.org/coar/resource_type/c_2f33 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/book |
| format |
book |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/20.500.14352/61191 |
| url |
https://hdl.handle.net/20.500.14352/61191 |
| dc.language.none.fl_str_mv |
Inglés eng |
| language_invalid_str_mv |
Inglés |
| language |
eng |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Instituto de Astronomía y Geodesia (IAG-CSIC-UCM) |
| publisher.none.fl_str_mv |
Instituto de Astronomía y Geodesia (IAG-CSIC-UCM) |
| dc.source.none.fl_str_mv |
reponame:Docta Complutense instname:Universidad Complutense de Madrid (UCM) |
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Universidad Complutense de Madrid (UCM) |
| reponame_str |
Docta Complutense |
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Docta Complutense |
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1869419670697672704 |
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15,300724 |