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The Effect of Ocean Tide Loading on Tides of the Solid Earth Observed with the Superconducting Gravimeter

✍ Scribed by Richard J. Warburton; Christopher Beaumont; John M. Goodkind


Book ID
108735007
Publisher
John Wiley and Sons
Year
1975
Tongue
English
Weight
849 KB
Volume
43
Category
Article
ISSN
0956-540X

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## Abstract Periodic variations in the location of the center of mass of the solid Earth due to ocean tides are derived from the ocean tide model of Seiler (1991). The sum of nine partial tides leads to changes in the coordinates __X, Y, Z__ within a range of 1cm.