step three.step 3. Complete Downwelling Anomaly Resolved from the Seismology
step three.step 3. Complete Downwelling Anomaly Resolved from the Seismology Seismic methods at the long wavelength limit detect the total seismic velocity anomaly Xoff ?c where ?c is the change of the velocity of the recorded wave. If seismic velocity varies linearly with temperature over this range, the total velocity anomaly is proportional to ?TdownXdown. […]