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On the Application of Relaxation Methods to Oceanic Tides

✍ Scribed by Rossiter, J. R.


Book ID
120144986
Publisher
The Royal Society
Year
1958
Tongue
English
Weight
729 KB
Volume
248
Category
Article
ISSN
0962-8444

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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.