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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Die Lehre von der Einzelwirtschafts of short wavelength geoidal undulation and those of free-air anomalies in the western Pacific look alike with each other. The gravity anomalies of shorter wavelengths can be explained by tectonics related with thickness of the lithosphere. Positive free-air anomalies of longer wavelengths may be e

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E. Blanck,F. Giesecke,H. Stremmegree meshsize) that is refined in three steps to half-degree mesh-size in most of the shelf areas. The technique of combining coarse and fine grid cells has been generalized. Thus the model is not restricted to a specific arrangement of the numerical grid.

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Umwandlungen der strahlenden Energie,n of orbit corrections, on exact geoid representation and on our ability to separate independent oceanic processes affecting sea surface elevations. The barotropic tide — namely the oceanic response to gravitational driving which maintains its phase lock with gravitational forces and which is always

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scotoma

Die Kapitalbeschaffung (Finanzierung) values of convenient small block size. Remaining gaps have been interpolated by means of least squares prediction filtering. The precision of the compiled mean free air gravity anomalies is estimated to ± 7 mgal, verified by a comparison of independent gravity anomaly sets.

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,6′× 10′ Free Air Gravity Anomalies of Europe Including Marine Areas, values of convenient small block size. Remaining gaps have been interpolated by means of least squares prediction filtering. The precision of the compiled mean free air gravity anomalies is estimated to ± 7 mgal, verified by a comparison of independent gravity anomaly sets.

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Book 1984r 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 (

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