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We used a full wave-theory method to construct synthetic seismograms (75) for general forms of D″ anisotropy in the D″ layer. This is a convenient method for modeling waves diffracted along a spherical boundary.
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Additional figures are available as supporting material on Science Online.
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We thank M. Bostock for assistance in accessing some of the Canadian National Seismic Network waveform data, S. Ford and D. Wiens for data from the South Pacific, and the Incorporated Research Institutions for Seismology Data Management Center for all other waveform data. This work was supported by the U.S. National Science Foundation. V.M. was on leave to Institut de Physique du Globe de Paris while part of this work was done.
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