One of the most important transport mechanisms results from wave refraction.
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True tombolos are formed by wave refraction and diffraction.
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The direction of wave approach is often relatively perpendicular due to wave refraction.
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P-wave refraction evaluates the compression wave generated by the seismic source located at a known distance from the array.
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S-wave refraction evaluates the shear wave generated by the seismic source located at a known distance from the array.
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Wave refraction disperses wave energy through the bay, and along with the sheltering effect of the headlands this protects bays from storms.
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Wave refraction can occur at the end of a spit, carrying sediment around the end to form a hook or recurved spit.
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Thus, they most commonly occur across artificial bay and river entrances due to the loss of kinetic energy in the current after wave refraction.
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Wave refraction is the process by which wave normal to wave crests between which a fixed amount of energy flux is contained converge on local shallows and shoals.
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This usually occurs due to wave refraction, but can also be caused by isostatic change, a change in the level of the land ( e . g.
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