Abstract
The origin of microseisms has been ascribed by the author to the action of oriented winds on rough sea surfaces [Nanda, 1960]. Earlier, Longuet-Higgins [1950] had explained that the interference of opposite components in the twodimensional wave spectra of the sea surface might give the pressure on the sea bottom responsible for the generation of microseisms. For the following reasons the author was discouraged from putting too much reliance on the Longuet-Higgins theory for the incoherent sea.
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.
