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. The efficiency and numerical accuracy of three algorithms to compute tidal loading are reviewed. The interest extends to vertical deformations and the self-attraction and loading effect caused by ocean tides. Load calculations require evaluation of convolution integrals over the sphere. In order to assess the numerical accuracy of a load calculation procedure we recall that there exists an almost...
The response of the Earth’s crust to the direct effect of lunisolar gravitational forcing is known as the body tide. The body tide is superimposed by surface-loading forces due to the pressure of the periodically varying ocean tide acting on the Earth, called ocean tide loading (OTL). Both body tide and OTL can be decomposed into components of the same frequency known as tidal parameters. However,...
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