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GRACE gravity model: assssment in terms of deep ocean currents from hydrography and from the ECCO ocean model

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dc.contributor.author Zlotnicki, V. en_US
dc.contributor.author Stammer, D. en_US
dc.contributor.author Fukumori, I. en_US
dc.date.accessioned 2004-09-16T21:30:08Z
dc.date.available 2004-09-16T21:30:08Z
dc.date.issued 2003-04-06 en_US
dc.identifier.citation EGS-AGU-EUG Joint Assembly en_US
dc.identifier.citation Nice, France en_US
dc.identifier.clearanceno 03-0499 en_US
dc.identifier.uri http://hdl.handle.net/2014/6647
dc.description.abstract Here we assess the new generation of gravity models, derived from GRACE data. The differences between a global geoid model (one from GRACE data and one the well-known EGM-96), minus a Mean Sea Surface derived from over a decade of altimetric data are compared to hydrographic data from the Levitus compilation and to the ECCO numerical ocean model, which assimilates altimetry and other data. en_US
dc.format.extent 2332627 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other oceans ocean currents El Nino TOPEX Jason seawinds GRACE en_US
dc.title GRACE gravity model: assssment in terms of deep ocean currents from hydrography and from the ECCO ocean model en_US


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