Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean

The spatial and time variations of the Southern Ocean sea level and its possible relationship with the Antartic sea ice changes and surface geostrophic currents in the area are investigated using altimeter data sets from ERS-1, ERS-2 and Topex-Poseidon between 1992 and 1999. Altimeter data are analy...

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Main Authors: P. Villares, P-U M. Catalán, J. Gómez-Enri, M. Bruno, A. Ruíz-Cañavate, Catalán P-u M, JJ. Alonso, R. Jiménez-Garay
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.20.5426
http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.20.5426 2023-05-15T14:15:46+02:00 Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean P. Villares P-U M. Catalán J. Gómez-Enri M. Bruno A. Ruíz-Cañavate Catalán P-u M JJ. Alonso R. Jiménez-Garay The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.20.5426 http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.20.5426 http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf text ftciteseerx 2016-01-07T17:21:32Z The spatial and time variations of the Southern Ocean sea level and its possible relationship with the Antartic sea ice changes and surface geostrophic currents in the area are investigated using altimeter data sets from ERS-1, ERS-2 and Topex-Poseidon between 1992 and 1999. Altimeter data are analysed following an Empirical Orthogonal Function Decomposition (EOFD) suggesting the following results: 1- The sea level variability is complex. Text antartic* Sea ice Southern Ocean Unknown Southern Ocean
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The spatial and time variations of the Southern Ocean sea level and its possible relationship with the Antartic sea ice changes and surface geostrophic currents in the area are investigated using altimeter data sets from ERS-1, ERS-2 and Topex-Poseidon between 1992 and 1999. Altimeter data are analysed following an Empirical Orthogonal Function Decomposition (EOFD) suggesting the following results: 1- The sea level variability is complex.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author P. Villares
P-U M. Catalán
J. Gómez-Enri
M. Bruno
A. Ruíz-Cañavate
Catalán P-u M
JJ. Alonso
R. Jiménez-Garay
spellingShingle P. Villares
P-U M. Catalán
J. Gómez-Enri
M. Bruno
A. Ruíz-Cañavate
Catalán P-u M
JJ. Alonso
R. Jiménez-Garay
Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
author_facet P. Villares
P-U M. Catalán
J. Gómez-Enri
M. Bruno
A. Ruíz-Cañavate
Catalán P-u M
JJ. Alonso
R. Jiménez-Garay
author_sort P. Villares
title Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
title_short Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
title_full Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
title_fullStr Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
title_full_unstemmed Satellite Altimeter Sea Level Variation Analysis Of The Southern Ocean
title_sort satellite altimeter sea level variation analysis of the southern ocean
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.20.5426
http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf
geographic Southern Ocean
geographic_facet Southern Ocean
genre antartic*
Sea ice
Southern Ocean
genre_facet antartic*
Sea ice
Southern Ocean
op_source http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.20.5426
http://earth.esa.int/pub/ESA_DOC/gothenburg/078gomez.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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