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...

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Autores: 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.
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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spelling 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)
instname_str Universidad Complutense de Madrid (UCM)
reponame_str Docta Complutense
collection Docta Complutense
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,300724