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

Evacuate

High Resolution Gravimetric Geoid Heights and Gravimetric Vertical Deflections of Europe Including ea, Baltic Sea and parts of the North Atlantic Ocean in a 12′ × 20′ grid. The computation has been carried out by least squares spectral combination using closed integral formulas, combining 104 000 mean free air gravity anomalies in 6′ × 10′ blocks, 12 000 mean free air gravity anomalies in 1° × 1°

整理

conservative

Geophysical Interpretation of Features in the Marine Geoid of Fennoscandia,tween current models of crustal depth and the geoid for marine areas of Scandinavia. The Fennoscandian land uplift together with its corresponding resultant change of geoid were also found to be highly correlated with crustal depth structure..Results of these correlations compare favorably with theo

amnesia

Geoidal Topography: Origin and Time Consistency,the internal structures and conditions. Deformations of the geoid — i.e. the mean sea level — with time, therefore, give evidence of density changes within the Earth. Past sea level changes that can be shown not to originate from tectonic processes, changes in the oceans’ water volume, changes in th

Panther

Free-Air Anomalies in the Western Pacific from the Viewpoint of Wave Number Spectrum,s 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

Daily-Value

性學(xué)院

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.

磨坊

Semidiurnal Amphidrome of the North East Pacific: Where?,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

多產(chǎn)魚

宣傳