Physics – Space Physics
Scientific paper
Feb 1984
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984rvgsp..22...73p&link_type=abstract
Reviews of Geophysics and Space Physics (ISSN 0034-6853), vol. 22, Feb. 1984, p. 73-84.
Physics
Space Physics
18
Earth Tides, Energy Budgets, Energy Dissipation, Atmospheric Tides, Integral Equations
Scientific paper
When developed in constituent form, the sphere-surface integral which presently expresses the dissipation of tidal energy depends linearly on the secondary potential that arises from the tidal disturbance, and can therefore be expressed as the sum of one part that is due to the body tide and another that is due to the fluid tides. While the former part solely depends on the anelastic part of the earth to the primary potential, the latter primarily depends on the elastic solid earth response to tidal loading and on the sum of the ocean tide and atmospheric tide mass disturbances. The + or - 15 percent uncertainty of recent ocean tide models' dissipation values can be accounted for by modeling difficulties.
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