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As a tsunami leaves the deep water of the open ocean and travels into the shallower water near the coast, it transforms. The tsunamis energy flux, which is dependent on both its wave speed and wave height, remains nearly constant. because of this shaoling effect, a tsunami, imperceptible at sea, may grow to be several meters or more in height near the coast. When it finally reaches the coast, a tsunami may appear as a rapidly rising or falling tide or a series of breaking waves.

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13y ago

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