Tsunami

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The 2004 Indian Ocean tsunami at Ao Nang, Krabi Province, Thailand 2004-tsunami.jpg
The 2004 Indian Ocean tsunami at Ao Nang, Krabi Province, Thailand
3D tsunami animation

A tsunami ( /(t)sˈnɑːmi,(t)sʊˈ-/ (t)soo-NAH-mee, (t)suu-; [1] [2] [3] [4] from Japanese : 津波, lit. 'harbour wave', [5] pronounced  [tsɯnami] ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. [6] Unlike normal ocean waves, which are generated by wind, or tides, which are generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water by a large event.

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Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer. [7] Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide. [8] For this reason, it is often referred to as a tidal wave, [9] although this usage is not favoured by the scientific community because it might give the false impression of a causal relationship between tides and tsunamis. [10] Tsunamis generally consist of a series of waves, with periods ranging from minutes to hours, arriving in a so-called "wave train." [11] Wave heights of tens of metres can be generated by large events. Although the impact of tsunamis is limited to coastal areas, their destructive power can be enormous, and they can affect entire ocean basins. The 2004 Indian Ocean tsunami was among the deadliest natural disasters in human history, with at least 230,000 people killed or missing in 14 countries bordering the Indian Ocean.

The Ancient Greek historian Thucydides suggested in his 5th century BC History of the Peloponnesian War that tsunamis were related to submarine earthquakes, [12] [13] but the understanding of tsunamis remained slim until the 20th century, and much remains unknown. Major areas of current research include determining why some large earthquakes do not generate tsunamis while other smaller ones do. This ongoing research is designed to help accurately forecast the passage of tsunamis across oceans as well as how tsunami waves interact with shorelines.

Terminology

Tsunami

Footnotes

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  4. "tsunami". Longman Dictionary of Contemporary English . Longman . Retrieved 19 August 2019.
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  12. 1 2 Thucydides: “A History of the Peloponnesian War”, 3.89.1–4
  13. 1 2 Smid, T. C. (April 1970). 'Tsunamis' in Greek Literature. Greece & Rome. 17 (2nd ed.). pp. 100–104.
  14. [a. Jap. tsunami, tunami, f. tsu harbour + nami waves.—Oxford English Dictionary]
  15. "Definition of Tidal Wave" . Retrieved 3 November 2016.
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  17. -al. (n.d.). Dictionary.com Unabridged (v 1.1). Retrieved November 11, 2008, Dictionary.reference.com
  18. "Forty Feet High and It Kills!" Hawaii Five-O. Writ. Robert C. Dennis and Edward J. Lakso. Dir. Michael O'Herlihy. CBS, 8 Oct. 1969. Television.
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  21. postcode=3001, corporateName=Bureau of Meteorology; address=GPO Box 1289, Melbourne, Victoria, Australia. "Joint Australian Tsunami Warning Centre" . Retrieved 3 November 2016.
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  24. Thucydides: “A History of the Peloponnesian War”, 3.89.5
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  40. Duff, Mark (2013-10-10). "Italy Vajont anniversary: Night of the 'tsunami'". BBC News. Bbc.co.uk. Retrieved 2014-02-27.
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References

Further reading

Tsunami
Tsunami (Chinese characters).svg
"Tsunami" in kanji