On the measurement of anelastic attenuation using amplitudes of low-frequency surface waves

Physics

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Scientific paper

A method is presented for the measurement of attenuation of long-period Rayleigh waves which minimizes two effects: that of biases owing to uncertainties in the source moment tensor and that of focusing owing to propagation in a laterally heterogeneous elastic Earth. In this manner, by measuring attenuation over minor arcs, odd terms of lateral heterogeneity in Q can be resolved. Global average Q estimates are in good agreement with the Preliminary Reference Earth Model (PREM) in the period range 180-285 s. At periods shorter than 180 s, our estimates of Q are lower than predicted by PREM. Maps of lateral variations in Q-1 show a general correspondence of high Q to high shear velocity and low Q to low shear velocity. In particular, the shift to the west, at increasing period, of the locus of the minimum in the Pacific Ocean is also observed in the Q-1 maps.

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