Propagation of coupled Rayleigh-gravity waves on the ocean floor
It is shown that the Ocean-Earth crust interface can propagate gravity-sound Rayleigh waves. Dispersion properties of waves and flux of energy are derived. It is shown that the waves split into low and fast velocity branches. The fast branch has a multimode structure and has a cutoff in frequency an...
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Format: | Article |
Language: | English |
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Universidad Nacional Autónoma de México, Instituto de Geofísica
1999-09-01
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Series: | Geofísica Internacional |
Subjects: | |
Online Access: | http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1999/04/burlak.pdf |
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author | Vladimir V. Grimalsky J. Sánchez-Mondragón Masashi Hayakawa Svetlana V. Koshevaya Gennadiy N. Burlak |
author_facet | Vladimir V. Grimalsky J. Sánchez-Mondragón Masashi Hayakawa Svetlana V. Koshevaya Gennadiy N. Burlak |
author_sort | Vladimir V. Grimalsky |
collection | DOAJ |
description | It is shown that the Ocean-Earth crust interface can propagate gravity-sound Rayleigh waves. Dispersion properties of waves and flux of energy are derived. It is shown that the waves split into low and fast velocity branches. The fast branch has a multimode structure and has a cutoff in frequency and wave number. Numerical solutions are discussed. |
first_indexed | 2024-03-12T07:22:10Z |
format | Article |
id | doaj.art-56abd90cc96a46f9866d8cd89c9d0897 |
institution | Directory Open Access Journal |
issn | 0016-7169 |
language | English |
last_indexed | 2024-03-12T07:22:10Z |
publishDate | 1999-09-01 |
publisher | Universidad Nacional Autónoma de México, Instituto de Geofísica |
record_format | Article |
series | Geofísica Internacional |
spelling | doaj.art-56abd90cc96a46f9866d8cd89c9d08972023-09-02T22:18:06ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71691999-09-01384261268Propagation of coupled Rayleigh-gravity waves on the ocean floorVladimir V. GrimalskyJ. Sánchez-MondragónMasashi HayakawaSvetlana V. KoshevayaGennadiy N. BurlakIt is shown that the Ocean-Earth crust interface can propagate gravity-sound Rayleigh waves. Dispersion properties of waves and flux of energy are derived. It is shown that the waves split into low and fast velocity branches. The fast branch has a multimode structure and has a cutoff in frequency and wave number. Numerical solutions are discussed.http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1999/04/burlak.pdfEarthquakeRayleigh wavegravity-sound wave |
spellingShingle | Vladimir V. Grimalsky J. Sánchez-Mondragón Masashi Hayakawa Svetlana V. Koshevaya Gennadiy N. Burlak Propagation of coupled Rayleigh-gravity waves on the ocean floor Geofísica Internacional Earthquake Rayleigh wave gravity-sound wave |
title | Propagation of coupled Rayleigh-gravity waves on the ocean floor |
title_full | Propagation of coupled Rayleigh-gravity waves on the ocean floor |
title_fullStr | Propagation of coupled Rayleigh-gravity waves on the ocean floor |
title_full_unstemmed | Propagation of coupled Rayleigh-gravity waves on the ocean floor |
title_short | Propagation of coupled Rayleigh-gravity waves on the ocean floor |
title_sort | propagation of coupled rayleigh gravity waves on the ocean floor |
topic | Earthquake Rayleigh wave gravity-sound wave |
url | http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1999/04/burlak.pdf |
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