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JOURNAL OF GEOPHYSICAL RESEARCH, VOL., C , doi.JC , Click Here for Full Article Infragravity waves in the deep ocean Generation, propagation, and seismic hum excitation Yusuke Uchiyama and James C.McWilliams Received September revised February accepted March published July.[] Oceanic infragravity waves are investigated as a possible source of seismic free oscillations, often referred to as the ‘‘hum of the Earth, using a numerical model of depth-independent, nondispersive, long-wave dynamics with a forcing from nonlinear interactions among the primary wind waves including swell.Because of near-resonant amplification, the structure of the primary-wave forcing field in shallow water, and an edge-trapping mechanism, infragravity waves are excited very effectively near the coasts.Deep-water
geophysical research, infragravity, propagation, excitation, cmcwilliams, september, oscillations, depth-independent nondispersive, interactions, near-resonant amplification, amplification structure, structure primary-wave, edge-trapping, coastsdeep-water, deep-water, ‘‘mesoscale,
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