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The series computation of the gravitational perturbation due to an ocean tide

✍ Scribed by J.B. Merriam


Book ID
116043713
Publisher
Elsevier Science
Year
1980
Tongue
English
Weight
458 KB
Volume
23
Category
Article
ISSN
0031-9201

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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.