Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Effects of Mantle Anelasticity on the Chandler Wobble

View through CrossRef
On the basis of the perturbation principles of the normal mode and Love numbers, the theoretical Q of the Chandler wobble is derived by assuming that the wobble energy is totally dissipated within the mantle and by using Zschau's mantle rheology model. The results show that mantle anelasticity is likely to be the most important dissipative source of the Chandler wobble energy, and the theoretical Chandler Q is 71. Finally, the parameter α of the absorption band model is calculated, and the applicability of the model is discussed as well.
Title: Effects of Mantle Anelasticity on the Chandler Wobble
Description:
On the basis of the perturbation principles of the normal mode and Love numbers, the theoretical Q of the Chandler wobble is derived by assuming that the wobble energy is totally dissipated within the mantle and by using Zschau's mantle rheology model.
The results show that mantle anelasticity is likely to be the most important dissipative source of the Chandler wobble energy, and the theoretical Chandler Q is 71.
Finally, the parameter α of the absorption band model is calculated, and the applicability of the model is discussed as well.

Related Results

Feedbacks between a non-Newtonian upper mantle, mantle viscosity structure and mantle dynamics
Feedbacks between a non-Newtonian upper mantle, mantle viscosity structure and mantle dynamics
SUMMARY Previous studies have shown that a low viscosity upper mantle can impact the wavelength of mantle flow and the balance of plate driving to resisting force...
Direct Confirmation of Chandler Wobble Source
Direct Confirmation of Chandler Wobble Source
Main nonsecular polar motion can be constructed from the current information of its excitation. Since early stages of Earth rotation study, several different sources were suggested...
Numerical modelling of mantle exhumation in inverted rift systems
Numerical modelling of mantle exhumation in inverted rift systems
The tectonic exhumation of mantle material is a well-known phenomenon and may occur during both rifting and subsequent (large-scale) basin inversion. However, the processes leading...
A study of the mantle flow field and lithospheric deformation beneath the Kuril-Kamchatka subduction zone using seismic anisotropy
A study of the mantle flow field and lithospheric deformation beneath the Kuril-Kamchatka subduction zone using seismic anisotropy
We investigate the flow field and deformation in the mantle wedge and subslab mantle beneath the Kuril-Kamchatka subduction zone using seismological data from a recently deployed s...
On the measurement of Sdiff splitting caused by lowermost mantle anisotropy
On the measurement of Sdiff splitting caused by lowermost mantle anisotropy
Seismic anisotropy has been detected at many depths of the Earth, including its upper layers, the lowermost mantle, and the inner core. While upper mantle seismic anisotropy is rel...
In-situ Measurement of Dislocation-induced Anelasticity by Using a Rock Analogue
In-situ Measurement of Dislocation-induced Anelasticity by Using a Rock Analogue
We developed a new experimental system with which anelasticity of a rock analogue sample (polycrystalline borneol) can be measured in situ during dislocation creep. We attached a p...
Connecting exoplanet mantle mineralogy to surface dynamic regime
Connecting exoplanet mantle mineralogy to surface dynamic regime
Based on stellar compositions, we know that rocky exoplanets show a diversity in interior compositions, and therefore mantle mineralogies. The mantle mineralogy controls physical p...

Back to Top