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- W2159087174 abstract "Description of seiches which occurred along the Gulf Coast of the United States and in Norway at the times of the Alaskan earthquake of 1964 and the Assam earthquake of 1950 are reviewed. An analytical expression is derived for the effect of seismic surface waves on a water channel of width L and depth H. The expression is used to explain many of the observations of Norwegian seiches and also to compute a theoretical marigram which is compared with an actual marigram recorded in a channel at Freeport, Texas. The horizontal components of seismic surface waves are shown to be the dominant cause of seiches due to teleseisms. The maximum seiche amplitudes vary as (1) the seismic wave amplitude, (2) (H)1/2 where H is the channel depth, and (3) the degree of resonance between the seismic waves and the natural periods of oscillation of standing water waves in the channel. The seismic surface waves from the Alaskan earthquake provided enough energy to produce all of the observed seiches in the Gulf Coast area. The seiche observations were limited to the Gulf Coast region because the thick sediments unique to this area are necessary to provide sufficient seismic wave amplification for the production of seiches." @default.
- W2159087174 created "2016-06-24" @default.
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- W2159087174 date "1965-02-15" @default.
- W2159087174 modified "2023-10-02" @default.
- W2159087174 title "Excitation of seiches in channels by seismic waves" @default.
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- W2159087174 doi "https://doi.org/10.1029/jz070i004p00847" @default.
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