By studying long-period precursors to SS and PP phases, it is possible to map global variations in the topography of the seismic discontinuities in the upper mantle.
Current results are available in the following papers:
SS precursor results (Flanagan and Shearer, 1998a), including figures, tables of the spherical harmonic coefficients for the smoothed topography maps (410, 520, 660, TZ), and a table of the individual depth estimates and travel-times are available by anonymous ftp at: mahi.ucsd.edu/pub/TOPOTZ.
PP precursor results (Flanagan and Shearer, 1999) including a model of 410 topography are available by anonymous ftp at: mahi.ucsd.edu/pub/TOPOPP.
Near-source 410 topography results (Flanagan and Shearer, 1998b) are available by anonymous ftp at: mahi.ucsd.edu/pub/THE410.
Click here to see maps of discontinuity topography derived from SS precursors (Plate 2 from Flanagan and Shearer, 1998a).