Propagation of coupled Rayleigh-gravity waves on the ocean floor
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Abstract
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.
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Burlak, G. N., Koshevaya, S. V., Hayakawa, M., Sánchez-Mondragón, J., & Grimalsky, V. V. (1999). Propagation of coupled Rayleigh-gravity waves on the ocean floor. Geofisica Internacional, 38(4), 261–268. https://doi.org/10.22201/igeof.00167169p.1999.38.4.508
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