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Titlebook: Geodetic Features of the Ocean Surface and their Implications; G. Seeber,J. R. Apel Book 1984 Springer Science+Business Media Dordrecht 19

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书目名称Geodetic Features of the Ocean Surface and their Implications
编辑G. Seeber,J. R. Apel
视频video
图书封面Titlebook: Geodetic Features of the Ocean Surface and their Implications;  G. Seeber,J. R. Apel Book 1984 Springer Science+Business Media Dordrecht 19
描述This volume contains most of the papers which were presented at the Interdisciplinary Symposium No. 4 "Geodetic Features of the Ocean Surface and their Implications" during the XVIII. General Assembly of the International Union of Geodesy and Geophysics (IUGG) in Hamburg, August 1983. The symposium was jointly sponsored by the International Associ­ ation of Geodesy (lAG) and the International Association for the Physi­ cal Sciences of the Ocean (IAPSO), and was as such one further step in animpQrtant line of international and interdisciplinary symposia, re­ lated to the field of Marine Geodesy. Originally the term "Marine Geodesy" was widely understood as "Geodesy in the Marine Environment" and dealt primarily with two as­ pects: precise position determination at sea and determination of a fine structured marine geoid. However, mainly with the impact of satel­ lite radar altimeter measurements, a new understanding began to develop: it became evident that the field of Marine Geodesy could not be treated adequately from geodesists alone but that it needed close cooperation with related disciplines such as oceanography and marine geophysics. Symposium No. 4 at Hamburg could demonstrat
出版日期Book 1984
关键词Gravimetrie; geophysics; lithosphere; modelling; satellite
版次1
doihttps://doi.org/10.1007/978-94-017-1673-4
isbn_softcover978-90-481-8405-7
isbn_ebook978-94-017-1673-4
copyrightSpringer Science+Business Media Dordrecht 1984
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Applications of Satellite Altimetry to Oceanography and Geophysics, surface height are equivalent to the geoid and are highly correlated with seafloor topography for wavelengths less than 1000 km. Using all available Geos-3 and Seasat altimeter data, mean sea surfaces and geoid gradient maps have been computed for the Bering Sea and the South Pacific. When enhanced
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Global Ocean Circulation Patterns Based on SEASAT Altimeter Data and the GEML2 Gravity Field,ve regional adjustments. This data was then used to create sea surface heights at 1° intersections in the ocean areas with respect to the GRS80 ellipsoid. These heights excluded the direct tidal effects but included the induced permanent deformation..A geoid corresponding to these sea surface height
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