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Titlebook: Global Gravity Field and Its Temporal Variations; Symposium No. 116 Bo Richard H. Rapp,Anny A. Cazenave,R. Steven Nerem Conference proceedi

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Gravity Research Missions reviewed in light of the indirect ocean tide potential., We deliberately avoid a lengthy summary of all the different concepts. It is sufficient to mention that gravity gradiometry and tracking of the orbiter have been proposed for mapping the detailed structures of the Earth’s gravitational field. The current shortcomings in global gravity models are st
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High Degree and Order Spherical Harmonic Models for the Moon From Clementine and Historic S-Band Daubsatellites, and the Clementine spacecraft. The model combines 361,000 observations from Clementine with 347,000 historical observations. The model was developed using the method of . [1991] in order to derive a more realistic realization of the uncertainties associated with this model. An . power
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