D-waves and nonuniformity of the rotation of the earth

Details D-waves and nonuniformity of the rotation of the earth D-waves and nonuniformity of the rotation of the earth

Oct 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976dossr.230..811g&link_type=abstract

Akademiia Nauk SSSR, Doklady, vol. 230, Oct. 1, 1976, p. 811-814. In Russian.

Physics

Geophysics

1

Cross Correlation, Earth Rotation, Earthquakes, Seismic Waves, Angular Velocity, Geophysics, Statistical Analysis, Tables (Data)

Scientific paper

An attempt is made to find a correlation between seismic D-waves responsible for earthquakes of a certain magnitude and the nonuniformity of earth rotation. The procedure used is to determine whether the position of T sub i, the time of occurrence of the i-th earthquake, coincides with one of the minima of the earth's rotation velocity. A coincidence would signify that the i-th earthquake occurs at the moment of the passage of one of the D-waves, induced at the pole by nonuniformity of earth rotation, through the epicenter. The analysis is based on data on the nonuniformity of earth rotation for the period 1815-1967. The example of earthquakes in the Arctic (1904-1975) tends to confirm the correlation.

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