
Rotationally consistent Love numbers
Author(s) -
Dickman S. R.
Publication year - 2005
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.2005.02574.x
Subject(s) - speed wobble , solid earth , mantle (geology) , geology , geodesy , consistency (knowledge bases) , seismology , geophysics , mathematics , physics , geometry , classical mechanics
SUMMARY The Love number k 2 at a 14‐month period is used to characterize the deformation of the solid earth during the Chandler wobble. Traditionally, the value of k 2 (CW), ∼0.31, is inferred from observations of the Chandler wobble period, after the effects of the oceans have been subtracted. However, during wobble the core is almost completely decoupled from the mantle; consistency requires that we view that inference as a mantle‐only value of the Love number. This in turn implies that k 2 = 0.35 , almost 13 per cent higher than the traditionally accepted value. The use of rotationally consistent Love numbers leads to equations for predicting the effects of a given rotational excitation that are distinctly different from previous versions. Furthermore, formulations of the excitation itself—such as the ‘effective angular momentum functions’ of Barnes et al. —are seriously modified, with the excitation functions up to ∼14 per cent larger. Rotationally consistent Love numbers imply that the solid earth is much more anelastic at a 14‐month period than previously considered. Popular ‘constant Q’ and ‘power‐law Q’ models of anelasticity are unable to simultaneously fit observations of k 2 at seismic, nine‐day, and Chandler frequencies. Alternative anelastic relaxation models such as those proposed by Ivins hold much more promise.