Abstract
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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
