Abstract
We have studied the response of normal modes to perturbations in inner-core shear velocity and attenuation, using fully coupled mode synthetics. Our results indicate that (i) mode pairs S-n(l)-S-n +/- 1(l) are strongly coupled by anelasticity, (ii) this coupling causes shear velocity perturbations to strongly affect the Q values of modes through exchange of inner-core characteristics, (iii) there is no evidence for a weakly attenuating inner core in shear, and (iv) the discrepancy between attenuation models returned from normal modes and body waves is small. These results suggest that inversions for inner-core attenuation and shear velocity should be performed simultaneously and should take account of the strong cross-coupling due to attenuation.
Original language | English |
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Pages (from-to) | 204-212 |
Number of pages | 9 |
Journal | Geophysical Journal International |
Volume | 167 |
Issue number | 1 |
DOIs | |
Publication status | Published - Oct 2006 |
Keywords
- attenuation
- inner core
- mode coupling
- normal modes
- FREE OSCILLATIONS
- EARTH
- ANISOTROPY
- CONSTRAINTS
- SPECTRA
- INVERSION