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- W2025101074 abstract "Measurements of the amplitude at every crest of the higher mode wave trains give “dynamic dispersion curves” which show the higher modes having increases of amplitude at the velocities of the channel waves. These increases are not associated with maxima or minima of the corresponding group velocity dispersion curves. Most observations of higher modes at Uppsala are of the second Rayleigh mode which show channel waves in their dynamic dispersion, although when other modes are present they also show channel waves. The channel waves of the second Rayleigh mode have retrograde elliptic motion whereas previous observations of channel waves have found them to have predominantly transverse horizontal motion." @default.
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- W2025101074 date "1965-04-01" @default.
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- W2025101074 title "Higher Modes of Seismic Surface Waves--Relations to Channel Waves" @default.
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