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

前兆

https://doi.org/10.1007/978-3-642-50913-1vel of accuracy of the best transportable gravimeters the agreement is perfect except at a few places where effects of lateral heterogeneities in the mantle can perhaps be suspected..These cotidal maps can therefore be safely used as working standards for other geodetic and geophysical applications.

CAPE

Die Lehre von den Pupillenbewegungenertical deflections has been estimated to ±2″. Comparisons of the gravimetric geoid heights and vertical deflections with a number of other solutions have been carried out, confirming the precision estimation.

deceive

Grundeigenschaften und Bau der Flüssigkeitenanges have now been identified for time units ranging from a few years to several million years (M?rner, op. cit.). This gives evidence of rapid processes within the Earth changing the density distribution; i.e. it gives evidence of a high-dynamic Earth.

小歌劇

https://doi.org/10.1007/978-3-662-02181-1representation of the real 1°-macroscopic nature of turbulent tidal currents. The quality of the representation was measured by the smoothness with which the hydrodynamically computed tidal field integrated thousands of empirical tide data uniformly over the world-wide oceans.

摻和

遺傳學(xué)

Ocean Bottom Friction Study from Numerical Modelling of Sea Surface Height and SEASAT-ALT Data,ly is the frictional coefficient important in this context, a variety of storm surge and tidal modelling problems also require a similar dissipation meachanism (Heaps 1969, Grace 1930, Stock 1976 etc.).

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