Open AccessOscillation, Nutation and Wobble of an Elliptical Rotating Earth with Liquid Outer Core
Author(s) -
Shen PoYu,
Mansinha L.
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.tb04167.x
Subject(s) - nutation , speed wobble , outer core , inner core , oscillation (cell signaling) , physics , rotation (mathematics) , earth's rotation , sidereal time , amplitude , core (optical fiber) , geophysics , mechanics , geodesy , classical mechanics , geology , geometry , chemistry , optics , astrophysics , mathematics , biochemistry , astronomy
We have constructed a general first‐order theory describing those small oscillations of a rotating elliptical earth that are affected by the presence of a liquid outer core. The theory is applicable to free core oscillations and earth tides. Care has been taken to include the effects of the wobble or nutation due to the rotation of the outer core relative to the solid earth. On the basis of the theory the free spheroidal modes of degree 2 and order 1 have been investigated. We have searched for and listed undertones with periods less than 28 hr. No upper limit to the eigenperiods has been detected. It is shown that stable, unstable and neutral polytropic cores are capable of free oscillation. At a period close to the sidereal day the spheroidal mode is accompanied by rigid rotation of the liquid outer core with respect to the solid earth. This is the well‐known diurnal wobble of the Earth. It appears probable that the diurnal wobble is one of a class of similar wobbles that involve large toroidal motions in the outer core. Finally, the amplitudes of the 18·6‐yr principal nutations has been computed. Excellent agreement is found with observed values.