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- W4249207924 abstract "Abstract. Seiches are often considered a transitory phenomenon wherein large amplitude water level oscillations are excited by a geophysical event, eventually dissipating some time after the event. However, continuous small-amplitude seiches have recently been recognized presenting a question as to the origin of continuous forcing. We examine 6 bays around the Pacific where continuous seiches are evident, and based on spectral, modal and kinematic analysis suggest that tidally-forced shelf-resonances are a primary driver of continuous seiches." @default.
- W4249207924 created "2022-05-12" @default.
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- W4249207924 date "2015-10-08" @default.
- W4249207924 modified "2023-10-16" @default.
- W4249207924 title "Continuous seiche in bays and harbors" @default.
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- W4249207924 doi "https://doi.org/10.5194/osd-12-2361-2015" @default.
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