The above shows the result of topography measurements for the 660 km
discontinuity; the average of all 470 cap values is 654 km. Each symbol represents the measured depth perturbation
from the average at the corresponding cap
location. Using the least squares method with damping, we fit the values of
spherical harmonics up to degree 12 (169 coefficients). The color contours
show the values obtained by the synthesis of the spherical harmonic
expansion. The most notable features are the large depression of the discontinuity boundary
in the western Pacific,
Tonga and South America. With the most dense data coverage included in this study, the depression under
the western Pacific extending from Kamchatka to the
Philippines is the most
robust of the long wavelength features. The depth perturbations are as large as
25 km from the global mean; this result is consistent with earlier works, and its cause has been associated
with the effect of subduction. No significant features
are evident near the East Pacific Rise.
THE POWER SPECTRUM
of the 660 km topography reveals a strong degree 2 and a relatively small degree 1.
There is an excellent correlation between the
velocity perturbations and 660 topography. In regions
where large positive velocity anomalies are found, such as
subduction zones in the western Pacific and South America,
we also find significant depression of the 660 km boundary. This feature
may be related to the negatively sloping phase boundary
or the negative buoyancy of the cold slab material.