A new derivation of the ratio Q(wobble)/Qμ (mantle) |
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Authors: | Ari Ben-Menahem |
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Institution: | Department of Applied Mathematics, The Weizmann Institute of Science, Rehovot, Israel |
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Abstract: | Summary An extension of the Love-Larmor theory to a low-loss unelastic earth model, leads to the surprisingly simple approximation where τs= 447.4 sidereal day is the static wobble period, τR= 306 sidereal day is the rigid-earth wobble period and τw= 433 sidereal day is the observed Chandler period. Q W, Q μ are the respective average Q values of the wobble and the Earth's mantle at τW. The known numerical factor F is only slightly dependent on the Earth structure. |
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