The Time-Varying Gravitational Potential Field of a Massive, Deformable Body /

The internal as well as the external gravitational field of the Earth is computed under the assumption that (i) the mass distribution of the deformable body as well as (ii) the heights of the topographic surface and the depths of the interfaces (‘dynamic isostasy’) vary in time. In order to represen...

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Typ dokumentu: Článek
Jazyk: angličtina
ISSN: 0039-3169
Zdroj: Studia geophysica et geodaetica : a journal of geophysics, meteorology and climatology, geodesy: Roč. 44, č. 3 (2000), s. 364-373.
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