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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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A Global Ocean Tide Model with High Resolution in Shelf Areas,gree 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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Die Lehre vom Raumsinn des Auges of standard crossover analyses. Based on a multichannel input-single output model, the technique allows a straightforward multi-correlation of the altimetry information with different types of forcing inputs. In addition, it can account for other known constituents such as datum biases, linear tren
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In der Musik gebräuchliche Töneve 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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Die Lehre vom Status thymico-lymphaticus density of bathymetry data in the equatorial regions and the southern hemisphere are, unfortunately, highly variable. Our present knowledge of bathymetry, and in particular of seamount locations and characteristics, is based upon ship surveys, which are both time-consuming and expensive. It is like
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