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Traveling Waves in Shallow Seas of Variable Depths
The problem of the existence of traveling waves in inhomogeneous fluid is very important
for enabling an explanation of long-distance wave propagations such as tsunamis and storm waves.
The present paper discusses new solutions to the variable-coefficient wave equations describing
traveling waves in fluid layers of variable depths (1D shallow-water theory). Such solutions are
obtained by using the transformation methods when variable-coefficient equations can be reduced
to the constant coefficient equation when the existence of traveling waves is evident. It is shown
that there is a wide class of monotonic bottom profiles (discrete set) that allow the existence of
traveling waves that are not reflected in a strongly inhomogeneous water medium. Their temporal
shape changes with distance, mainly near the water–land boundary (shoreline). Traveling waves can
transfer the wave energy over a long distance that is often observed at the transoceanic propagation
of tsunami waves