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A meteotsunami or meteorological tsunami [1] is a tsunami-like sea wave of meteorological origin. Meteotsunamis are generated when rapid changes in barometric pressure cause the displacement of a body of water.
Amplitude, Wave Height, or Tsunami Height: Refers to the height of a tsunami relative to the normal sea level at the time of the tsunami, which may be tidal High Water, or Low Water. It is different from the crest-to-trough height which is commonly used to measure other type of wave height.
A tsunami hitting a coastline. This article lists notable tsunamis, which are sorted by the date and location that they occurred.. Because of seismic and volcanic activity associated with tectonic plate boundaries along the Pacific Ring of Fire, tsunamis occur most frequently in the Pacific Ocean, [1] but are a worldwide natural phenomenon.
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Regular sea level at Kata Noi beach. Maximum recession of the sea at Kata Noi Beach at 10:25 a.m., prior to the third—and strongest—tsunami wave. The economic impact of the tsunami on Thailand was considerable, though not as great as in poorer countries such as Indonesia or Sri Lanka.