On correlation of the energies of primary and secondary storm microseisms

Details On correlation of the energies of primary and secondary storm microseisms On correlation of the energies of primary and secondary storm microseisms

Oct 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990pepi...63..196o&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 63, Issue 3-4, p. 196-200.

Physics

1

Scientific paper

The estimations made by Ostrovsky (1979) have revealed that the energy correlation of primary and secondary storm microseisms should substantially increase with increasing period of the oceanic waves generating them. Comparison with experimental data (Korhonen, 1971; Korhonen and Pirhonen, 1976; Bossolasco et al., 1973) showed that these conclusions are confirmed in many cases. This permitted a new interpretation of some of the results. The dependence of the intensity of primary and secondary microseisms on the period of oceanic waves is suggested as an additional criterion for the detection of the generation zones of microseisms.

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