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Storm Surge Causes and Different Variations
Author(s) -
Park Mao
Publication year - 2017
Publication title -
international journal for empirical education and research
Language(s) - English
Resource type - Journals
eISSN - 2616-4833
pISSN - 2616-4817
DOI - 10.35935/edr/12.101
Subject(s) - storm surge , storm , tropical cyclone , flood myth , fetch , climatology , environmental science , surge , extratropical cyclone , geology , meteorology , oceanography , geography , archaeology
A storm surge, storm flood or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low pressure weather systems (such as tropical cyclones and strong extra-tropical cyclones), the severity of which is affected by the shallowness and orientation of the water body relative to storm path, as well as the timing of tides. Most casualties during tropical cyclones occur as the result of storm surges. It is a measure of the rise of water beyond what would be expected by the normal movement related to tides. The two main meteorological factors contributing to a storm surge are a long fetch of winds spiraling inward toward the storm, and a low-pressure-induced dome of water drawn up under and trailing the storm's center.

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