Open AccessThe Passive Influence of the Oceans upon the Rotation of the Earth
Author(s) -
Dahlen F. A.
Publication year - 1976
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1976.tb04163.x
Subject(s) - speed wobble , gravitational potential , eigenfunction , polar motion , earth's rotation , physics , rotation (mathematics) , classical mechanics , gravitation , geology , mechanics , geodesy , geometry , quantum mechanics , mathematics , eigenvalues and eigenvectors
A general theory is developed which allows the exact numerical computation of the static equilibrium response of a non‐rotating spherically symmetric Earth model covered by thin oceans with geometrically irregular coastlines to the action of an imposed static tidal or centrifugal potential. The theory is self‐consistent, and takes into account the gravitational self‐attraction of the oceans and the elastic‐gravitational response of the Earth model to both the applied potential and the equilibrium oceanic tidal load on the surface. The results are used to determine the influence of an equilibrium pole tide on the free period and the associated rotational eigenfunction of the Chandler wobble. If the pole is globally well represented by this equilibrium approximation, its effect is to increase the Chandler wobble period by 27·6 days. It is shown that a fully self‐consistent theory of the rotation of an Earth model with oceans predicts that changes in spin and wobble will be coupled, and that the Chandler wobble should, as a result, be accompanied by an associated periodic change in the length of day. The consequences of spin‐wobble coupling are explored quantitatively, and found to be slight.