Array ( [0] => {{short description|Series of water waves caused by the displacement of a large volume of a body of water}} [1] => {{Other uses|Tsunami (disambiguation)|Tidal wave (disambiguation){{!}}Tidal wave}} [2] => {{Redirect|Sunami|the hardcore punk band|Sunami (band)}} [3] => {{pp-semi-indef}} [4] => {{pp-move-indef}} [5] => {{EngvarB|date=July 2019}} [6] => [[File:2004-tsunami.jpg|thumb|upright=1.4|The [[2004 Indian Ocean earthquake and tsunami|2004 Indian Ocean tsunami]] at [[Ao Nang]], [[Krabi Province]], [[Thailand]]]] [7] => [[File:NOAA Tsunami Animation-2016.webm|thumb|upright=1.4|3D tsunami animation]] [8] => A '''tsunami''' ({{IPAc-en|(|t|)|s|uː|ˈ|n|ɑː|m|i|,_|(|t|)|s|ʊ|ˈ|-}} {{respell|(t)soo|NAH|mee|,_|(t)suu|-}};{{cite book |title=Longman pronunciation dictionary |first=John C. |last= Wells |publisher=Longman |location=Harlow, England |date=1990 |isbn=978-0-582-05383-0 |page=736 }} Entry: "tsunami"{{cite web|url=https://www.macmillandictionary.com/pronunciation/british/tsunami|title=tsunami|work=[[Macmillan Dictionary]]|access-date=2018-11-23}}{{Cite Merriam-Webster|tsunami|access-date=19 August 2019}}{{cite web|url=https://www.ldoceonline.com/dictionary/tsunami|title=tsunami|work=[[Longman Dictionary of Contemporary English]]|publisher=[[Longman]]|access-date=19 August 2019}} from {{lang-ja|津波|lit=harbour wave}},{{cite web|url=http://nthmp-history.pmel.noaa.gov/terms.html|title=Tsunami Terminology|publisher=[[NOAA]]|access-date=2010-07-15|url-status=dead|archive-url=https://web.archive.org/web/20110225143835/http://nthmp-history.pmel.noaa.gov/terms.html|archive-date=2011-02-25}} {{IPA-ja|tsɯnami|pron}}) 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 [[tsunamis in lakes|large lake]]. [[Earthquake]]s, [[volcanic eruption]]s and other [[underwater explosion]]s (including detonations, [[landslide]]s, [[Ice calving|glacier calvings]], [[impact event|meteorite impacts]] and other disturbances) above or below water all have the potential to generate a tsunami.{{cite journal|title=When icebergs capsize, tsunamis may ensue|url=http://blogs.nature.com/barbaraferreira/2011/04/17/when-icebergs-capsize|author=Barbara Ferreira|date=April 17, 2011|journal=[[Nature (journal)|Nature]]|access-date=2011-04-27|archive-date=2011-11-04|archive-url=https://web.archive.org/web/20111104140755/http://blogs.nature.com/barbaraferreira/2011/04/17/when-icebergs-capsize|url-status=dead}} Unlike normal [[Wind wave|ocean waves, which are generated by wind]], or [[tide]]s, which are in turn generated by the [[gravitational pull]] of the [[Moon]] and the [[Sun]], a tsunami is generated by the displacement of water from a large event. [9] => [10] => Tsunami waves do not resemble normal undersea currents or [[Wind wave|sea waves]] because their [[Wind wave#Formation|wavelength]] is far longer.{{cite web|url=http://www.jpl.nasa.gov/news/news.php?release=2011-374|title=NASA Finds Japan Tsunami Waves Merged, Doubling Power|website=[[Jet Propulsion Laboratory]]|access-date=3 November 2016}} Rather than appearing as a [[breaking wave]], a tsunami may instead initially resemble a rapidly rising [[tide]].{{cite web|url=http://courses.washington.edu/larescue/Tsunami101/Tsunami101.htm|title= Tsunami 101|publisher= University of Washington |access-date= 1 December 2018}} For this reason, it is often referred to as a '''tidal wave''',{{Cite web | url=https://www.merriam-webster.com/dictionary/tidal%20wave | title=Definition of Tidal Wave}} 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.{{cite web|url= https://earthweb.ess.washington.edu/tsunami/general/physics/meaning.html |title= What does "tsunami" mean? | publisher = Earth and Space Sciences, University of Washington | access-date = 1 December 2018}} Tsunamis generally consist of a series of waves, with [[Period (physics)|period]]s ranging from minutes to hours, arriving in a so-called "[[wave packet|wave train]]".{{cite book |last=Fradin |first=Judith Bloom and Dennis Brindell |title=Witness to Disaster: Tsunamis |publisher=[[National Geographic Society]] |location=Washington, D.C. |date=2008 |pages=42–43 |url=http://shop.nationalgeographic.com/ngs/product/books/kids-books-and-atlases/animals-and-nature/witness-to-disaster%3A-tsunamis |url-status=dead |archive-url=https://web.archive.org/web/20120406091721/http://shop.nationalgeographic.com/ngs/product/books/kids-books-and-atlases/animals-and-nature/witness-to-disaster:-tsunamis |archive-date=2012-04-06 }} 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 earthquake and tsunami|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]]. [11] => [12] => The [[Ancient Greece|Ancient Greek]] historian [[Thucydides]] suggested in his 5th century BC ''[[History of the Peloponnesian War]]'' that tsunamis were related to [[submarine earthquake]]s, 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. [13] => [14] => ==Terminology== [15] => ===Tsunami=== [16] => {{infobox Chinese [17] => |pic=Tsunami (Chinese characters).svg [18] => |piccap="Tsunami" in ''[[kanji]]'' [19] => |picupright=0.35 [20] => |kanji=津波 [21] => |romaji=tsunami [22] => }} [23] => The term "tsunami" is a [[loan word|borrowing]] from the Japanese ''tsunami'' {{lang|ja|津波}}, meaning "harbour wave." For the plural, one can either follow ordinary English practice and add an ''s'', or use an invariable plural as in the Japanese.[a. Jap. tsunami, tunami, f. tsu harbour + nami waves.—''Oxford English Dictionary''] Some English speakers alter the word's initial {{IPAslink|ts}} to an {{IPAslink|s}} by dropping the "t," since English does not natively permit {{IPA|/ts/}} at the beginning of words, though the original Japanese pronunciation is {{IPA|/ts/}}. The term has become commonly accepted in English, although its literal Japanese meaning is not necessarily descriptive of the waves, which do not occur only in harbours. [24] => [25] => ===Tidal wave=== [26] => [[File:Tsunami 2004 aftermath. Aceh, Indonesia, 2005. Photo- AusAID (10730863873).jpg|thumb|upright=1.35|Tsunami aftermath in [[Aceh]], [[Indonesia]], December 2004]] [27] => [28] => Tsunamis are sometimes referred to as ''tidal waves''.{{cite web|url=http://www.merriam-webster.com/dictionary/tidal%20wave|title=Definition of Tidal Wave|access-date=3 November 2016}} This once-popular term derives from the most common appearance of a tsunami, which is that of an extraordinarily high [[tidal bore]]. Tsunamis and tides both produce waves of water that move inland, but in the case of a tsunami, the inland movement of water may be much greater, giving the impression of an incredibly high and forceful tide. In recent years, the term "tidal wave" has fallen out of favour, especially in the scientific community, because the causes of tsunamis have nothing to do with those of [[tide]]s, which are produced by the gravitational pull of the moon and sun rather than the displacement of water. Although the meanings of "tidal" include "resembling""Tidal", The American Heritage Stedman's Medical Dictionary. [[Houghton Mifflin Harcourt|Houghton Mifflin Company]]. 11 November 2008.[http://dictionary.reference.com/browse/tidal Dictionary.reference.com] or "having the form or character of"-al. (n.d.). Dictionary.com Unabridged (v 1.1). Retrieved November 11, 2008, [http://dictionary.reference.com/browse/-al Dictionary.reference.com] tides, use of the term ''tidal wave'' is discouraged by geologists and oceanographers. [29] => [30] => A 1969 episode of the TV crime show ''[[Hawaii Five-O (1968 TV series)|Hawaii Five-O]]'' entitled "Forty Feet High and It Kills!" used the terms "tsunami" and "tidal wave" interchangeably."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. [31] => [32] => ===Seismic sea wave=== [33] => The term '''''seismic sea wave''''' is also used to refer to the phenomenon because the waves most often are generated by [[seismic]] activity such as earthquakes.{{cite web|url=http://weready.org/tsunami/index.php?option=com_glossary&letter=S&id=56|title=Seismic Sea Wave – Tsunami Glossary|access-date=3 November 2016}} Prior to the rise of the use of the term ''tsunami'' in English, scientists generally encouraged the use of the term ''seismic sea wave'' rather than ''tidal wave''. However, like ''tidal wave'', ''seismic sea wave'' is not a completely accurate term, as forces other than earthquakes—including underwater [[landslide]]s, volcanic eruptions, underwater explosions, land or ice [[Slump (geology)|slumping]] into the ocean, [[meteorite]] impacts, and the weather when the atmospheric pressure changes very rapidly—can generate such waves by displacing water.{{cite web|url=http://earthsci.org/education/teacher/basicgeol/tsumami/tsunami.html|title=tsunamis|access-date=3 November 2016}}{{cite web|url=http://www.bom.gov.au/tsunami/info/faq.shtml|title=Joint Australian Tsunami Warning Centre|first=corporateName=Bureau of Meteorology; address=GPO Box 1289, Melbourne, Victoria, Australia|last=postcode=3001|access-date=3 November 2016}} [34] => [35] => ===Other terms=== [36] => The use of the term ''tsunami'' for waves created by landslides entering bodies of water has become internationally widespread in both scientific and popular literature, although such waves are distinct in origin from large waves generated by earthquakes. This distinction sometimes leads to the use of other terms for landslide-generated waves, including '''''landslide-triggered tsunami''''', '''''displacement wave''''', '''''non-seismic wave''''', '''''impact wave''''', and, simply, '''''giant wave'''''.{{Cite journal|last1=Svennevig |first1=Kristian |last2=Hermanns |first2=Reginald L.|last3=Keiding |first3=Marie|last4=Binder |first4=Daniel|last5=Citterio |first5=Michelle |last6=Dahl-Jensen |first6=Trine|last7=Mertl |first7=Stefan|last8=Sørensen |first8=Erik Vest|last9=Voss |first9=Peter H. |date=23 July 2022|title=A large frozen debris avalanche entraining warming permafrost ground—the June 2021 Assapaat landslide, West Greenland|journal=Landslides|volume=19 |issue=11 |pages=2549–2567 |publisher=Springer Link|doi=10.1007/s10346-022-01922-7 |bibcode=2022Lands..19.2549S |doi-access=free }} [37] => [38] => ==History== [39] => {{see also|List of tsunamis}} [40] => [41] => [[File:1755 Lisbon earthquake.jpg|thumb|upright=1.35|[[1755 Lisbon earthquake|Lisbon earthquake and tsunami]] in November 1755]] [42] => [43] => While Japan may have the longest [[recorded history]] of tsunamis,{{Cite web |title=International Team Studies Tsunami Deposits in Japan to Improve Understanding and Mitigation of Tsunami Hazards {{!}} U.S. Geological Survey |url=https://www.usgs.gov/centers/pcmsc/news/international-team-studies-tsunami-deposits-japan-improve-understanding-and |access-date=2024-01-31 |website=www.usgs.gov}}{{Better citation|reason=The claim is only mentioned once without clarification ([[WP:NOTRS]]).|date=February 2024}} the sheer destruction caused by the [[2004 Indian Ocean earthquake and tsunami]] event mark it as the most devastating of its kind in modern times, killing around 230,000 people.[https://www.bbc.com/news/world-asia-30602159 Indian Ocean tsunami anniversary: Memorial events held] 26 December 2014, BBC News The [[Sumatra]]n region is also accustomed to tsunamis, with earthquakes of varying magnitudes regularly occurring off the coast of the island.[http://www.australiangeographic.com.au/journal/the-10-biggest-tsunamis-in-history.htm/ The 10 most destructive tsunamis in history] {{Webarchive|url=https://web.archive.org/web/20131204022559/http://www.australiangeographic.com.au/journal/the-10-biggest-tsunamis-in-history.htm |date=2013-12-04 }}, Australian Geographic, March 16, 2011. [44] => [45] => Tsunamis are an often underestimated hazard in the [[Mediterranean Sea]] and parts of Europe. Of historical and current (with regard to risk assumptions) importance are the [[1755 Lisbon earthquake|1755 Lisbon earthquake and tsunami]] (which was caused by the [[Azores–Gibraltar Transform Fault]]), the [[1783 Calabrian earthquakes]], each causing several tens of thousands of deaths and the [[1908 Messina earthquake]] and tsunami. The tsunami claimed more than 123,000 lives in Sicily and Calabria and is among the deadliest natural disasters in modern Europe. The [[Storegga Slide]] in the Norwegian Sea and some examples of [[tsunamis affecting the British Isles]] refer to landslide and [[meteotsunami]]s, predominantly and less to earthquake-induced waves. [46] => [47] => [[426 BC Malian Gulf tsunami|As early as 426 BC]] the [[Ancient Greece|Greek]] historian [[Thucydides]] inquired in his book ''[[History of the Peloponnesian War]]'' about the causes of tsunami, and was the first to argue that ocean earthquakes must be the cause.[[Thucydides]]: [https://www.perseus.tufts.edu/cgi-bin/ptext?lookup=Thuc.+3.89.1 “A History of the Peloponnesian War”, 3.89.1–4]{{cite book|last=Smid|first=T. C.|title='Tsunamis' in Greek Literature|edition=2nd|volume=17|date=April 1970|pages=100–104|work=Greece & Rome|issue=1}} The oldest human record of a tsunami dates back to [[479 BC Potidaea earthquake|479 BC]], in the Greek colony of [[Potidaea]], thought to be triggered by an earthquake. The tsunami may have saved the colony from an invasion by the [[Achaemenid Empire]]. [48] => [49] =>
The cause, in my opinion, of this phenomenon must be sought in the earthquake. At the point where its shock has been the most violent the sea is driven back, and suddenly recoiling with redoubled force, causes the inundation. Without an earthquake I do not see how such an accident could happen.[[Thucydides]]: [https://www.perseus.tufts.edu/cgi-bin/ptext?lookup=Thuc.+3.89.1 “A History of the Peloponnesian War”, 3.89.5]
[50] => [51] => The [[Ancient Rome|Roman]] historian [[Ammianus Marcellinus]] (''Res Gestae'' 26.10.15–19) described the typical sequence of a tsunami, including an incipient earthquake, the sudden retreat of the sea and a following gigantic wave, after the [[365 Crete earthquake|365 AD tsunami]] devastated [[Alexandria]].{{cite journal|doi=10.2307/4135013|last=Kelly|first=Gavin|date=2004|title=Ammianus and the Great Tsunami|journal=The Journal of Roman Studies|volume=94|pages=141–167|issue=141|jstor=4135013|s2cid=160152988|url=https://www.research.ed.ac.uk/portal/en/publications/ammianus-and-the-great-tsunami(635a4807-14c9-4044-9caa-8f8e3005cb24).html|hdl=20.500.11820/635a4807-14c9-4044-9caa-8f8e3005cb24|hdl-access=free}}Stanley, Jean-Daniel & Jorstad, Thomas F. (2005), "[http://gsa.confex.com/gsa/2005AM/finalprogram/abstract_96386.htm The 365 A.D. Tsunami Destruction of Alexandria, Egypt: Erosion, Deformation of Strata and Introduction of Allochthonous Material] {{Webarchive|url=https://web.archive.org/web/20170525095324/https://gsa.confex.com/gsa/2005AM/finalprogram/abstract_96386.htm |date=2017-05-25 }}" [52] => [53] => ==Causes== [54] => The principal generation mechanism of a tsunami is the displacement of a substantial volume of water or perturbation of the sea.{{cite journal|doi=10.1016/j.marpetgeo.2004.10.016|last1=Haugen|first1=K|last2=Lovholt|first2=F|last3=Harbitz|first3=C|title=Fundamental mechanisms for tsunami generation by submarine mass flows in idealised geometries|journal=[[Marine and Petroleum Geology]]|date=2005|volume=22|issue=1–2|pages=209–217|bibcode=2005MarPG..22..209H }} This displacement of water is usually caused by earthquakes,{{cite web|title=Tsunami Locations & Occurrences|publisher=National Weather Service|url=https://www.weather.gov/jetstream/locations|access-date=16 January 2022}}{{cite news|first=Lisa M.|last=Krieger|title=Volcanic tsunamis: Why they are so difficult to predict|date=15 January 2022|newspaper=The Mercury News|url=https://www.mercurynews.com/2022/01/15/volcanic-tsunamis-why-they-are-so-difficult-to-predict/|access-date=16 January 2022}}{{cite news|title=Tsunamis|work=National Geographic|url=https://www.nationalgeographic.com/environment/article/tsunamis|archive-url=https://web.archive.org/web/20210412193722/https://www.nationalgeographic.com/environment/article/tsunamis|url-status=dead|archive-date=April 12, 2021|access-date=16 January 2022}} but can also be attributed to landslides, volcanic eruptions, glacier calvings or more rarely by meteorites and nuclear tests.{{cite journal|last=Margaritondo|first=G|title=Explaining the physics of tsunamis to undergraduate and non-physics students|journal=European Journal of Physics|date=2005|volume=26|issue=3|doi=10.1088/0143-0807/26/3/007|pages=401–407|bibcode = 2005EJPh...26..401M |s2cid=7512603|url=http://pdfs.semanticscholar.org/1b83/2dd51b201c4ee597b374780e359604e8b781.pdf|archive-url=https://web.archive.org/web/20190219220116/http://pdfs.semanticscholar.org/1b83/2dd51b201c4ee597b374780e359604e8b781.pdf|url-status=dead|archive-date=2019-02-19}}{{cite journal|doi=10.1146/annurev.fl.19.010187.001245|last=Voit|first=S.S|title=Tsunamis|journal=Annual Review of Fluid Mechanics|date=1987|volume=19|issue=1|pages=217–236|bibcode = 1987AnRFM..19..217V }} However, the possibility of a meteorite causing a tsunami is debated.{{cite news|title=Are Ocean Asteroid Impacts Really a Serious Threat?|author=Tia Ghose|date=2014|url=https://www.livescience.com/49298-asteroids-causing-tsunamis.html}} [55] => [56] => ===Seismicity=== [57] => Tsunamis can be generated when the sea floor abruptly deforms and vertically displaces the overlying water. Tectonic earthquakes are a particular kind of earthquake that are associated with the Earth's crustal deformation; when these earthquakes occur beneath the sea, the water above the deformed area is displaced from its equilibrium position.{{cite web|title=How do earthquakes generate tsunamis?|url=http://www.geophys.washington.edu/tsunami/general/physics/earthquake.html|publisher=University of Washington|archive-url=https://web.archive.org/web/20070203154326/http://www.geophys.washington.edu/tsunami/general/physics/earthquake.html|archive-date=2007-02-03}} More specifically, a tsunami can be generated when [[thrust fault]]s associated with [[convergent boundary|convergent]] or destructive [[plate boundaries]] move abruptly, resulting in water displacement, owing to the vertical component of movement involved. Movement on [[Fault (geology)#Dip-slip faults|normal (extensional) faults]] can also cause displacement of the seabed, but only the largest of such events (typically related to flexure in the [[outer trench swell]]) cause enough displacement to give rise to a significant tsunami, such as the [[1977 Sumba earthquake|1977 Sumba]] and [[1933 Sanriku earthquake|1933 Sanriku]] events.{{citation|title=Source Process of the Great 1977 Sumba Earthquake|url=http://www.es.ucsc.edu/~thorne/TL.pdfs/LL_Sumba_JGR1988.pdf|first1=C. S.|last1=Lynnes|first2=T.|last2=Lay|year=1988|journal=Geophysical Research Letters|publisher=[[American Geophysical Union]]|volume=93|issue=B11|pages=13,407–13,420|doi=10.1029/JB093iB11p13407|bibcode = 1988JGR....9313407L }}{{cite journal | title=Seismological evidence for a lithospheric normal faulting – the Sanriku earthquake of 1933 | author=Kanamori H. | author-link=Hiroo Kanamori|journal=Physics of the Earth and Planetary Interiors | year=1971 | volume=4 | issue=4 | pages=298–300 | doi=10.1016/0031-9201(71)90013-6|bibcode = 1971PEPI....4..289K }} [58] => [59] => [60] => File:Eq-gen1.svg|Drawing of [[tectonic plate boundary]] before [[earthquake]] [61] => File:Eq-gen2.svg|Over-riding plate bulges under strain, causing [[tectonic uplift]]. [62] => File:Eq-gen3.svg|Plate slips, causing [[subsidence]] and releasing energy into water. [63] => File:Eq-gen4.svg|The energy released produces tsunami waves. [64] => [65] => [66] => Tsunamis have a small wave height offshore, and a very long [[wavelength]] (often hundreds of kilometres long, whereas normal ocean waves have a wavelength of only 30 or 40 metres),[http://www.australiangeographic.com.au/journal/facts-and-figures-how-tsunamis-form.htm/ Facts and figures: how tsunamis form] {{Webarchive|url=https://web.archive.org/web/20131105033906/http://www.australiangeographic.com.au/journal/facts-and-figures-how-tsunamis-form.htm/ |date=2013-11-05 }}, Australian Geographic, March 18, 2011. which is why they generally pass unnoticed at sea, forming only a slight swell usually about {{convert|300|mm|in}} above the normal sea surface. They grow in height when they reach shallower water, in a [[wave shoaling]] process described below. A tsunami can occur in any tidal state and even at low tide can still inundate coastal areas. [67] => [68] => On April 1, 1946, the 8.6 {{M|w}} [[1946 Aleutian Islands earthquake|Aleutian Islands earthquake]] occurred with a maximum [[Mercalli intensity scale|Mercalli intensity]] of VI (''Strong''). It generated a tsunami which inundated [[Hilo, Hawaii|Hilo]] on the island of Hawaii with a {{convert|14|m|ft|adj=mid|high}} surge. Between 165 and 173 were killed. The area where the earthquake occurred is where the [[Pacific Ocean]] floor is [[subducting]] (or being pushed downwards) under Alaska. [69] => [70] => Examples of tsunamis originating at locations away from convergent boundaries include [[Storegga]] about 8,000 years ago, [[Grand Banks]] in 1929, and [[Papua New Guinea]] in 1998 (Tappin, 2001). The Grand Banks and Papua New Guinea tsunamis came from earthquakes which destabilised sediments, causing them to flow into the ocean and generate a tsunami. They dissipated before travelling transoceanic distances. [71] => [72] => The cause of the Storegga sediment failure is unknown. Possibilities include an overloading of the sediments, an earthquake or a release of gas hydrates (methane etc.). [73] => [74] => The [[1960 Valdivia earthquake]] ([[Moment magnitude scale|''M''w]] 9.5), [[1964 Alaska earthquake]] (''M''w 9.2), [[2004 Indian Ocean earthquake]] (''M''w 9.2), and [[2011 Tōhoku earthquake and tsunami|2011 Tōhoku earthquake]] (''M''w9.0) are recent examples of powerful [[megathrust earthquake]]s that generated tsunamis (known as [[teletsunamis]]) that can cross entire oceans. Smaller (''M''w 4.2) earthquakes in Japan can trigger tsunamis (called local and regional tsunamis) that can devastate stretches of coastline, but can do so in only a few minutes at a time. [75] => [76] => ===Landslides=== [77] => The [[Tauredunum event]] was a large tsunami on [[Lake Geneva]] in 563 CE, caused by sedimentary deposits destabilized by a landslide. [78] => [79] => {{Anchor|Tsunami generated by landslides}} [80] => In the 1950s, it was discovered that tsunamis larger than had previously been believed possible can be caused by giant [[submarine landslides]]. These large volumes of rapidly displaced water transfer energy at a faster rate than the water can absorb. Their existence was confirmed in 1958, when a giant landslide in [[1958 Lituya Bay megatsunami|Lituya Bay]], Alaska, caused the highest wave ever recorded, which had a height of {{convert|524|m|ft|0}}.{{cite web |url=http://www.drgeorgepc.com/Tsunami1958LituyaB.html|title=The Mega-Tsunami of July 9, 1958 in Lituya Bay, Alaska|author=George Pararas-Carayannis|date=1999|access-date=2014-02-27}} The wave did not travel far as it struck land almost immediately. The wave struck three boats—each with two people aboard—anchored in the bay. One boat rode out the wave, but the wave sank the other two, killing both people aboard one of them.{{cite web| url = https://alaskashipwreck.com/shipwrecks-a-z/alaska-shipwrecks-b/| title = alaskashipwreck.com Alaska Shipwrecks (B)}}{{cite web| url = https://alaskashipwreck.com/shipwrecks-a-z/alaska-shipwrecks-s/| title = alaskashipwreck.com Alaska Shipwrecks (S)}}{{cite web| url = https://earthquake.alaska.edu/60-years-ago-1958-earthquake-and-lituya-bay-megatsunami| title = Dickson, Ian, "60 Years Ago: The 1958 Earthquake and Lituya Bay Megatsunami," University of Alaska Fairbanks Alaska Earthquake Center, July 13, 2018 Retrieved December 2, 2018.}} [81] => [82] => Another landslide-tsunami event occurred in 1963 when a massive landslide from [[Monte Toc]] entered the reservoir behind the [[Vajont Dam]] in Italy. The resulting wave surged over the {{convert|262|m|ft|0|adj=on}}-high dam by {{convert|250|m|ft|0}} and destroyed several towns. Around 2,000 people died.{{cite web |author=Petley, Dave (Professor) |url=http://www.landslideblog.org/2008/12/vaiont-vajont-landslide-of-1963.html |title=The Vaiont (Vajont) landslide of 1963 |publisher=The Landslide Blog |date=2008-12-11 |access-date=2014-02-26 |url-status=dead |archive-url=https://web.archive.org/web/20131206033431/http://www.landslideblog.org/2008/12/vaiont-vajont-landslide-of-1963.html |archive-date=2013-12-06 }}{{cite web|last=Duff |first=Mark |url=https://www.bbc.co.uk/news/world-europe-24464867 |title=Italy Vajont anniversary: Night of the 'tsunami' |work=BBC News |publisher=Bbc.co.uk |date=2013-10-10 |access-date=2014-02-27}} Scientists named these waves [[megatsunami]]s. [83] => [84] => Some geologists claim that large landslides from volcanic islands, e.g. [[Cumbre Vieja]] on [[La Palma]] ([[Cumbre Vieja tsunami hazard]]) in the [[Canary Islands]], may be able to generate megatsunamis that can cross oceans, but this is disputed by many others. [85] => [91] => [92] => In general, landslides generate displacements mainly in the shallower parts of the coastline, and there is conjecture about the nature of large landslides that enter the water. This has been shown to subsequently affect water in enclosed bays and lakes, but a landslide large enough to cause a transoceanic tsunami has not occurred within recorded history. Susceptible locations are believed to be the [[Hawaii (island)|Big Island]] of [[Hawaii]], [[Fogo, Cape Verde|Fogo]] in the [[Cape Verde Islands]], [[Réunion|La Reunion]] in the [[Indian Ocean]], and [[Cumbre Vieja]] on the island of [[La Palma]] in the [[Canary Islands]]; along with other volcanic ocean islands. This is because large masses of relatively unconsolidated volcanic material occurs on the flanks and in some cases detachment planes are believed to be developing. However, there is growing controversy about how dangerous these slopes actually are.{{cite journal| journal=Science of Tsunami Hazards| volume=20| number=5| pages=251–277| url=http://news.bbc.co.uk/2/hi/science/nature/3963563.stm| access-date=7 September 2014| title=Evaluation of the threat of mega tsunami generation from postulated massive slope failures of the island volcanoes on La Palma, Canary Islands, and on the island of Hawaii| first=George| last=Pararas-Carayannis| date=2002}} [93] => [94] => ===Volcanic eruptions=== [95] => {{main|Volcanic tsunami}} [96] => [97] => Other than by landslides or [[sector collapse]], volcanoes may be able to generate waves by [[pyroclastic flow]] submergence, caldera collapse, or underwater explosions.{{cite journal |last1=Paris |first1=R. |date=2015 |title=Source mechanisms of volcanic tsunamis |journal=Phil. Trans. R. Soc. |volume=373 |issue=2053 |doi=10.1098/rsta.2014.0380 |pmid=26392617 |bibcode=2015RSPTA.37340380P |s2cid=43187708 |doi-access=free }} Tsunamis have been triggered by a number of volcanic eruptions, including the [[1883 eruption of Krakatoa#Tsunamis and distant effects|1883 eruption of Krakatoa]], and the [[2022 Hunga Tonga–Hunga Ha'apai eruption and tsunami|2022 Hunga Tonga–Hunga Ha'apai eruption]]. Over 20% of all fatalities caused by volcanism during the past 250 years are estimated to have been caused by [[Volcanogenic tsunami|volcanogenic]] tsunamis.{{cite journal |last1=Latter |first1=J. H. |date=1981 |title=Tsunamis of volcanic origin: Summary of causes, with particular reference to Krakatoa, 1883 |url=https://link.springer.com/article/10.1007/BF02600578 |journal=Bulletin Volcanologique |volume=44 |issue=3 |pages=467–490|doi=10.1007/BF02600578 |bibcode=1981BVol...44..467L |s2cid=129637214 }} [98] => [99] => Debate has persisted over the origins and source mechanisms of these types of tsunamis, such as those generated by Krakatoa in 1883, and they remain lesser understood than their seismic relatives. This poses a large problem of awareness and preparedness, as exemplified by the eruption and collapse of [[2018 Sunda Strait tsunami|Anak Krakatoa in 2018]], which killed 426 and injured thousands when no warning was available. [100] => [101] => It is still regarded that lateral landslides and ocean-entering pyroclastic currents are most likely to generate the largest and most hazardous waves from volcanism;{{cite encyclopedia|last=Day|first=Simon J.|chapter-url=https://www.sciencedirect.com/science/article/pii/B9780123859389000584|title=The Encyclopedia of Volcanoes|chapter=Volcanic Tsunamis|publisher=[[Elsevier]]|year=2015|pages=993–1009 |doi=10.1016/B978-0-12-385938-9.00058-4 |isbn=9780123859389 |access-date=2022-03-21}} however, field investigation of the [[2022 Hunga Tonga–Hunga Ha'apai eruption and tsunami|Tongan event]], as well as developments in numerical modelling methods, currently aim to expand the understanding of the other source mechanisms.{{cite journal |last1=Hayward|first1=Matthew. W. |last2=Whittaker|first2=C. N. |last3=Lane|first3=E. M. |last4=Power|first4=W. L. |last5=Popinet|first5=S. |last6=White|first6=J.D.L. |date=2022 |title=Multilayer modelling of waves generated by explosive subaqueous volcanism |url=https://nhess.copernicus.org/articles/22/617/2022/ |journal=[[Natural Hazards and Earth System Sciences]] |volume=22 |issue=2|pages=617–637|doi=10.5194/nhess-22-617-2022 |bibcode=2022NHESS..22..617H |doi-access=free }}{{cite journal |last1=Battershill |first1=L. |date=2021 |title=Numerical Simulations of a Fluidized Granular Flow Entry Into Water: Insights Into Modeling Tsunami Generation by Pyroclastic Density Currents |url=https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021JB022855 |archive-url=https://web.archive.org/web/20230603121655/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021JB022855 |url-status=dead |archive-date=June 3, 2023 |journal=[[Journal of Geophysical Research: Solid Earth]] |volume=126 |issue=11 |doi=10.1029/2021JB022855 |bibcode=2021JGRB..12622855B |s2cid=243837214 }} [102] => [103] => ===Meteorological=== [104] => {{main|Meteotsunami}} [105] => Some [[meteorological]] conditions, especially rapid changes in barometric pressure, as seen with the passing of a front, can displace bodies of water enough to cause trains of waves with wavelengths. These are comparable to seismic tsunamis, but usually with lower energies. Essentially, they are dynamically equivalent to seismic tsunamis, the only differences being 1) that meteotsunamis lack the transoceanic reach of significant seismic tsunamis, and 2) that the force that displaces the water is sustained over some length of time such that meteotsunamis cannot be modelled as having been caused instantaneously. In spite of their lower energies, on shorelines where they can be amplified by resonance, they are sometimes powerful enough to cause localised damage and potential for loss of life. They have been documented in many places, including the Great Lakes, the Aegean Sea, the English Channel, and the Balearic Islands, where they are common enough to have a local name, ''rissaga''. In Sicily they are called ''marubbio'' and in Nagasaki Bay, they are called ''abiki''. Some examples of destructive meteotsunamis include 31 March 1979 at Nagasaki and 15 June 2006 at Menorca, the latter causing damage in the tens of millions of euros.{{cite journal|last1=Monserrat|first1=S.|last2=Vilibíc|first2=I.|last3=Rabinovich|first3=A. B.|date=2006|title=Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band|journal=Natural Hazards and Earth System Sciences|volume=6|pages=1035–1051|doi=10.5194/nhess-6-1035-2006|bibcode=2006NHESS...6.1035M|issue=6|doi-access=free}} [106] => [107] => Meteotsunamis should not be confused with [[storm surges]], which are local increases in sea level associated with the low barometric pressure of passing tropical cyclones, nor should they be confused with setup, the temporary local raising of sea level caused by strong on-shore winds. Storm surges and setup are also dangerous causes of [[coastal flooding]] in severe weather but their dynamics are completely unrelated to tsunami waves. They are unable to propagate beyond their sources, as waves do. [108] => [109] => === Human-made or triggered tsunamis === [110] => {{see also|Tsunami bomb}} [111] => [112] => The accidental [[Halifax Explosion]] in 1917 triggered an 18-meter high tsunami in the harbour. [113] => [114] => There have been studies of the potential of the induction of and at least one actual attempt to create tsunami waves as a [[tectonic weapon]]. [115] => [116] => In World War II, the [[New Zealand Army|New Zealand Military Forces]] initiated [[Project Seal]], which attempted to create small tsunamis with explosives in the area of today's [[Shakespear Regional Park]]; the attempt failed.{{cite news|title=The Hauraki Gulf Marine Park, Part 2|date=3 March 2010|work=Inset to [[The New Zealand Herald]]|page=9}} [117] => [118] => There has been considerable speculation on the possibility of using [[nuclear weapon]]s to cause tsunamis near an enemy coastline. Even during [[World War II]] consideration of the idea using conventional explosives was explored. Nuclear testing in the [[Pacific Proving Ground]] by the United States seemed to generate poor results. ''Operation Crossroads'' fired two {{convert|20|ktTNT|abbr=on}} bombs, one in the air and one underwater, above and below the shallow ({{convert|50|m|abbr=on}}) waters of the [[Bikini Atoll]] lagoon. Fired about {{convert|6|km|abbr=on}} from the nearest island, the waves there were no higher than {{convert|3|–|4|m|abbr=on}} upon reaching the shoreline. Other underwater tests, mainly ''[[Operation Hardtack I|Hardtack I]]/Wahoo'' (deep water) and ''Hardtack I/Umbrella'' (shallow water) confirmed the results. Analysis of the effects of [[underwater explosion#shallow underwater explosions|shallow]] and [[underwater explosion#deep underwater explosions|deep underwater explosions]] indicate that the energy of the explosions does not easily generate the kind of deep, all-ocean waveforms which are tsunamis; most of the energy creates steam, causes vertical fountains above the water, and creates compressional waveforms.{{cite book| last1=Glasstone| first1=Samuel| last2=Dolan| first2=Philip| date=1977| title=Shock effects of surface and subsurface bursts – The effects of nuclear weapons| edition=third| place=Washington, DC| publisher=U.S. Department of Defense; Energy Research and Development Administration}} Tsunamis are hallmarked by permanent large vertical displacements of very large volumes of water which do not occur in explosions. [119] => [120] => ==Characteristics== [121] => [[File: Propagation du tsunami en profondeur variable.gif|thumb|When the wave enters shallow water, it slows down and its amplitude (height) increases.]] [122] => [[File:Tsunami2.JPG|thumb|The wave further slows and amplifies as it hits land. Only the largest waves crest.]] [123] => [124] => Tsunamis are caused by earthquakes, landslides, volcanic explosions, glacier calvings, and [[bolide]]s. They cause damage by two mechanisms: the smashing force of a wall of water travelling at high speed, and the destructive power of a large volume of water draining off the land and carrying a large amount of debris with it, even with waves that do not appear to be large. [125] => [126] => While everyday [[wind wave]]s have a [[wavelength]] (from crest to crest) of about {{convert|100|m|ft}} and a height of roughly {{convert|2|m|ft}}, a tsunami in the deep ocean has a much larger wavelength of up to {{convert|200|km|mi}}. Such a wave travels at well over {{convert|800|km/h|mph}}, but owing to the enormous wavelength the wave oscillation at any given point takes 20 or 30 minutes to complete a cycle and has an amplitude of only about {{convert|1|m|ft}}.[http://earthsci.org/education/teacher/basicgeol/tsumami/tsunami.html Earthsci.org], Tsunamis This makes tsunamis difficult to detect over deep water, where ships are unable to feel their passage. [127] => [128] => The velocity of a tsunami can be calculated by obtaining the square root of the depth of the water in metres multiplied by the acceleration due to gravity (approximated to 10 m/s2). For example, if the Pacific Ocean is considered to have a depth of 5000 metres, the velocity of a tsunami would be {{sqrt|5000 × 10}} = {{sqrt|50000}} ≈ {{convert|224|m/s|ft/s}}, which equates to a speed of about {{convert|806|km/h|mi/h}}. This is the formula used for calculating the velocity of [[Shallow water equations#Wave modelling by shallow water equations|shallow-water]] waves. Even the deep ocean is shallow in this sense because a tsunami wave is so long (horizontally from crest to crest) by comparison. [129] => [130] => The reason for the Japanese name "harbour wave" is that sometimes a village's [[fishermen]] would sail out, and encounter no unusual waves while out at sea fishing, and come back to land to find their village devastated by a huge wave. [131] => [132] => As the tsunami approaches the coast and the waters become shallow, [[wave shoaling]] compresses the wave and its speed decreases below {{convert|80|km/h|mph}}. Its wavelength diminishes to less than {{convert|20|km|mi}} and its amplitude grows enormously—in accord with [[Green's law]]. Since the wave still has the same very long [[frequency|period]], the tsunami may take minutes to reach full height. Except for the very largest tsunamis, the approaching wave does not [[Breaking wave|break]], but rather appears like a fast-moving [[tidal bore]].{{cite web|url=http://walrus.wr.usgs.gov/tsunami/basics.html|title=Life of a Tsunami|date=22 October 2008|work=Western Coastal & Marine Geology|publisher=United States Geographical Survey|access-date=2009-09-09}} Open bays and coastlines adjacent to very deep water may shape the tsunami further into a step-like wave with a steep-breaking front. [133] => [134] => When the tsunami's wave peak reaches the shore, the resulting temporary rise in sea level is termed ''run up''. Run up is measured in metres above a reference sea level. A large tsunami may feature multiple waves arriving over a period of hours, with significant time between the wave crests. The first wave to reach the shore may not have the highest run-up.{{cite web|url=http://www.tulane.edu/~sanelson/geol204/tsunami.htm|title=Tsunami|author=Prof. Stephen A. Nelson|date=28 January 2009|publisher=Tulane University|access-date=2009-09-09}} [135] => [136] => About 80% of tsunamis occur in the Pacific Ocean, but they are possible wherever there are large bodies of water, including lakes. However, tsunami interactions with shorelines and the seafloor topography are extremely complex, which leaves some countries more vulnerable than others. For example, the Pacific coasts of the United States and Mexico lie adjacent to each other, but the United States has recorded ten tsunamis in the region since 1788, while Mexico has recorded twenty-five since 1732.{{cite web |url=https://www.worlddata.info/america/usa/tsunamis.php |website=WorldData|title=Tsunamis in the United States }}{{cite web |url=https://www.worlddata.info/america/mexico/tsunamis.php |website=WorldData|title=Tsunamis in Mexico }} Similarly, Japan has had more than a hundred tsunamis in recorded history, while the neighboring island of Taiwan has registered only two, in 1781 and 1867.{{Cite web|url=https://www.worlddata.info/asia/japan/tsunamis.php|title=Tsunamis in Japan|website=Worlddata.info}}{{Cite web|url=https://www.worlddata.info/asia/taiwan/tsunamis.php|title=Tsunamis in Taiwan|website=Worlddata.info}} [137] => [138] => {{clear}} [139] => [140] => ==Drawback== [141] => [[File: Shallow water wave.gif|upright=2|thumb|right|An illustration of the rhythmic "drawback" of surface water associated with a wave. It follows that a very large drawback may herald the arrival of a very large wave.]] [142] => [143] => All [[wave]]s have a positive and negative peak; that is, a ridge and a trough. In the case of a propagating wave like a tsunami, either may be the first to arrive. If the first part to arrive at the shore is the ridge, a massive breaking wave or sudden flooding will be the first effect noticed on land. However, if the first part to arrive is a trough, a drawback will occur as the shoreline recedes dramatically, exposing normally submerged areas. The drawback can exceed hundreds of metres, and people unaware of the danger sometimes remain near the shore to satisfy their curiosity or to collect fish from the exposed seabed. [144] => [145] => A typical wave period for a damaging tsunami is about twelve minutes. Thus, the sea recedes in the drawback phase, with areas well below sea level exposed after three minutes. For the next six minutes, the wave trough builds into a ridge which may flood the coast, and destruction ensues. During the next six minutes, the wave changes from a ridge to a trough, and the flood waters recede in a second drawback. Victims and debris may be swept into the ocean. The process repeats with succeeding waves. [146] => [147] => ==Scales of intensity and magnitude== [148] => As with earthquakes, several attempts have been made to set up scales of tsunami intensity or magnitude to allow comparison between different events.{{cite web|author=Gusiakov V.|title=Tsunami Quantification: how we measure the overall size of tsunami (Review of tsunami intensity and magnitude scales)|url=http://www.ngdc.noaa.gov/hazard/data/presentations/jtc/gusiakov.pdf|access-date=2009-10-18}} [149] => [150] => ===Intensity scales=== [151] => The first scales used routinely to measure the intensity of tsunamis were the ''[[August Heinrich Sieberg|Sieberg]]-[[Nicholas Ambraseys|Ambraseys]] scale'' (1962), used in the [[Mediterranean Sea]] and the ''Imamura-Iida intensity scale'' (1963), used in the Pacific Ocean. The latter scale was modified by Soloviev (1972), who calculated the tsunami intensity "''I''" according to the formula: [152] => [153] => :\mathit{I} = \frac{1}{2} + \log_{2} \mathit{H}_{av} [154] => [155] => where \mathit{H}_{av} is the "tsunami height" in meters, averaged along the nearest coastline, with the tsunami height defined as the rise of the water level above the normal tidal level at the time of occurrence of the tsunami.Soloviev, S., & Go, N., 1974 (English transl. 1984), [http://www.dfo-mpo.gc.ca/Library/69881.pdf “Catalogue of tsunamis on the western shore of the Pacific Ocean”], Canadian Translation of Fisheries and Aquatic Sciences, No. 5077, (310 p). This scale, known as the ''Soloviev-Imamura tsunami intensity scale'', is used in the global tsunami catalogues compiled by the NGDC/NOAA{{cite web|url=http://ngdc.noaa.gov/hazard/tsu_db.shtml|title=NGDC/WDS Global Historical Tsunami Database – NCEI|first=National Geophysical Data|last=Center|access-date=3 November 2016}} and the Novosibirsk Tsunami Laboratory as the main parameter for the size of the tsunami. [156] => [157] => This formula yields: [158] => * ''I'' = 2 for \mathit{H}_{av} = 2.8 metres [159] => * ''I'' = 3 for \mathit{H}_{av} = 5.5 metres [160] => * ''I'' = 4 for \mathit{H}_{av} = 11 metres [161] => * ''I'' = 5 for \mathit{H}_{av} = 22.5 metres [162] => * etc. [163] => [164] => In 2013, following the intensively studied tsunamis in 2004 and 2011, a new 12-point scale was proposed, the Integrated Tsunami Intensity Scale (ITIS-2012), intended to match as closely as possible to the modified [[Environmental Seismic Intensity scale|ESI2007]] and [[European Macroseismic Scale|EMS]] earthquake intensity scales.{{cite journal | title=A Proposal for a New Integrated Tsunami Intensity Scale (ITIS-2012) | author=Lekkas E. | author2=Andreadakis E. | author3=Kostaki I. | author4=Kapourani E. | name-list-style=amp | journal=Bulletin of the Seismological Society of America | date=2013 | volume=103 | issue=2B | pages=1493–1502 | doi=10.1785/0120120099|bibcode = 2013BuSSA.103.1493L }}Katsetsiadou, K.N., Andreadakis, E. and Lekkas, E., 2016. [http://www.pagepress.org/journals/index.php/rg/article/view/5857 Tsunami intensity mapping: applying the integrated Tsunami Intensity Scale (ITIS2012) on Ishinomaki Bay Coast after the mega-tsunami of Tohoku, March 11, 2011]. ''Research in Geophysics'', ''5''(1). [165] => [166] => ===Magnitude scales=== [167] => The first scale that genuinely calculated a magnitude for a tsunami, rather than an intensity at a particular location was the ML scale proposed by Murty & Loomis based on the potential energy. Difficulties in calculating the potential energy of the tsunami mean that this scale is rarely used. Abe introduced the ''tsunami magnitude scale \mathit{M}_{t}'', calculated from, [168] => [169] => :\mathit{M}_{t} = {a} \log h + {b} \log R + \mathit{D} [170] => [171] => where ''h'' is the maximum tsunami-wave amplitude (in m) measured by a tide gauge at a distance ''R'' from the epicentre, ''a'', ''b'' and ''D'' are constants used to make the Mt scale match as closely as possible with the moment magnitude scale.{{Cite book|author=Abe K.|date =1995|title=Estimate of Tsunami Run-up Heights from Earthquake Magnitudes|work=Tsunami: progress in prediction, disaster prevention, and warning|publisher =Springer|access-date=2009-10-18|url=https://books.google.com/books?id=5YjaGdQOJIwC&pg=PA21 |isbn=978-0-7923-3483-5}} [172] => [173] => ==Tsunami heights== [174] => [[File:Tsunami run-up, height, and inundation.png|thumb|Diagram showing several measures to describe a tsunami size, including height, inundation and run-up]] [175] => Several terms are used to describe the different characteristics of tsunami in terms of their height:{{cite web| url = http://itic.ioc-unesco.org/index.php?option=com_content&view=category&layout=blog&id=1142&Itemid=1142| title = Tsunami Glossary}}{{cite web| url = https://walrus.wr.usgs.gov/news/tsu-terms.html| title = Tsunami Terms}}{{cite web| url = http://www.jma.go.jp/jma/kishou/know/faq/faq26.html| title = 津波について}}{{Cite web |url=http://www.coastal.jp/ttjt/index.php?%E6%B4%A5%E6%B3%A2 |title=津波の高さの定義 |access-date=2012-02-19 }}{{dead link|date=April 2021|bot=medic}}{{cbignore|bot=medic}} [176] => * 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.{{cite web| url = http://weready.org/tsunami/index.php?option=com_glossary&letter=T&id=73| title = Tsunami Amplitude}} [177] => * Run-up Height, or Inundation Height: The height reached by a tsunami on the ground above sea level, Maximum run-up height refers to the maximum height reached by water above sea level, which is sometimes reported as the maximum height reached by a tsunami. [178] => * Flow Depth: Refers to the height of tsunami above ground, regardless of the height of the location or sea level. [179] => * (Maximum) Water Level: Maximum height above sea level as seen from trace or water mark. Different from maximum run-up height in the sense that they are not necessarily water marks at inundation line/limit. [180] => [181] => ==Warnings and predictions== [182] => {{See also|Tsunami warning system}}{{Verification|Section|date=July 2023}}[[File:Calculated Travel Time Map for 1964 Alaska Tsunami.jpg|thumb|300 px|Calculated travel time map for the 1964 Alaska tsunami (in hours)]] [183] => [184] => Drawbacks can serve as a brief warning. People who observe drawback (many survivors report an accompanying sucking sound) can survive only if they immediately run for high ground or seek the upper floors of nearby buildings. [185] => [186] => In 2004, ten-year-old [[Tilly Smith]] of [[Surrey]], England, was on [[Maikhao beach]] in [[Phuket Province|Phuket]], Thailand with her parents and sister, and having learned about tsunamis recently in school, told her family that a tsunami might be imminent. Her parents warned others minutes before the wave arrived, saving dozens of lives. She credited her geography teacher, Andrew Kearney. [187] => [188] => In the [[2004 Indian Ocean earthquake|2004 Indian Ocean tsunami]] drawback was not reported on the African coast or any other east-facing coasts that it reached. This was because the initial wave moved downwards on the eastern side of the [[Megathrust earthquake|megathrust]] and upwards on the western side. The western pulse hit coastal Africa and other western areas. [189] => [190] => A tsunami cannot be precisely predicted, even if the magnitude and location of an earthquake is known. [[Geologist]]s, [[oceanographer]]s, and [[seismologist]]s analyse each earthquake and based on many factors may or may not issue a tsunami warning. However, there are some warning signs of an impending tsunami, and automated systems can provide warnings immediately after an earthquake in time to save lives. One of the most successful systems uses bottom pressure sensors, attached to buoys, which constantly monitor the pressure of the overlying water column. [191] => [192] => Regions with a high tsunami risk typically use [[tsunami warning system]]s to warn the population before the wave reaches land. On the west coast of the United States, which is prone to tsunamis from the Pacific Ocean, warning signs indicate evacuation routes. In Japan, the populace is well-educated about earthquakes and tsunamis, and along Japanese shorelines, tsunami warning signs remind people of the natural hazards along with a network of warning sirens, typically at the top of the cliffs of surrounding hills.{{cite journal|author=Chanson, H.|author-link=Hubert Chanson |title= Tsunami Warning Signs on the Enshu Coast of Japan |url= http://espace.library.uq.edu.au/view/UQ:203103 |journal=Shore & Beach|pages=52–54|number=1|volume=78 |date=2010 |issn= 0037-4237}} [193] => [194] => The [[Pacific Tsunami Warning Center|Pacific Tsunami Warning System]] is based in [[Honolulu]], [[Hawaii|Hawai{{okina}}i]]. It monitors Pacific Ocean seismic activity. A sufficiently large earthquake magnitude and other information triggers a tsunami warning. While the subduction zones around the Pacific are seismically active, not all earthquakes generate a tsunami. Computers assist in analysing the tsunami risk of every earthquake that occurs in the Pacific Ocean and the adjoining land masses. [195] => [196] => [197] => File:Bamfield Tsunami Hazard Zone sign.jpg|Tsunami hazard sign at [[Bamfield]], [[British Columbia]] [198] => File: A tsunami warning sign in Kamakura, Japan.jpg|A tsunami warning sign in [[Kamakura, Kanagawa|Kamakura]], Japan [199] => File:Zona de Inundabilidad.jpg|A Tsunami hazard sign (Spanish - English) in [[Iquique]], [[Chile]] [200] => File:Tsunami Evacuation Route signage south of Aberdeen Washington.jpg|alt=Photo of evacuation sign|Tsunami Evacuation Route signage along [[U.S. Route 101 in Washington|U.S. Route 101]], in [[Washington (state)|Washington]] [201] => [202] => [203] => As a direct result of the Indian Ocean tsunami, a re-appraisal of the tsunami threat for all coastal areas is being undertaken by national governments and the United Nations Disaster Mitigation Committee. A tsunami warning system is being installed in the Indian Ocean. [204] => [205] => [[File:Dart tsunamicover.jpg|thumb|upright|One of the deep water [[buoy]]s used in the [[Deep-ocean Assessment and Reporting of Tsunamis|DART]] tsunami warning system]] [206] => [207] => [[Computer model]]s can predict tsunami arrival, usually within minutes of the arrival time. Bottom pressure sensors can relay information in [[present|real time]]. Based on these pressure readings and other seismic information and the seafloor's shape ([[bathymetry]]) and coastal [[topography]], the models estimate the amplitude and surge height of the approaching tsunami. All [[Pacific Rim]] countries collaborate in the Tsunami Warning System and most regularly practise evacuation and other procedures. In Japan, such preparation is mandatory for government, local authorities, emergency services and the population. [208] => [209] => Along the United States west coast, in addition to sirens, warnings are sent on television and radio via the [[National Weather Service]], using the [[Emergency Alert System]]. [210] => [211] => ===Possible animal reaction=== [212] => {{further|Infrasound#Animal reaction}} [213] => Some zoologists hypothesise that some animal species have an ability to sense subsonic [[Rayleigh wave]]s from an earthquake or a tsunami. If correct, monitoring their behaviour could provide advance warning of earthquakes and tsunamis. However, the evidence is controversial and is not widely accepted. There are unsubstantiated claims about the [[1755 Lisbon earthquake|Lisbon quake]] that some animals escaped to higher ground, while many other animals in the same areas drowned. The phenomenon was also noted by media sources in [[Sri Lanka]] in the [[2004 Indian Ocean earthquake]].{{cite news|publisher=BBC|date=2005-03-27|first=Helen|last=Lambourne|title=Tsunami: Anatomy of a disaster |url=http://news.bbc.co.uk/1/hi/world/south_asia/4269847.stm}}{{cite magazine|title=Surviving the Tsunami: What Sri Lanka's animals knew that humans didn't|first=Christine|last=Kenneally|magazine=Slate Magazine|url=http://www.slate.com/id/2111608|date=2004-12-30}} It is possible that certain animals (e.g., [[elephant]]s) may have heard the sounds of the tsunami as it approached the coast. The elephants' reaction was to move away from the approaching noise. By contrast, some humans went to the shore to investigate and many drowned as a result. [214] => [215] => ==Mitigation== [216] => {{see also|Seawall}} [217] => [218] => [[File:Tsunami wall.jpg|thumb|upright|A [[seawall]] at [[Tsu, Mie|Tsu]], [[Mie Prefecture]] in Japan|alt=Photo of seawall, with building in background]] [219] => [220] => In some tsunami-prone countries, [[earthquake engineering]] measures have been taken to reduce the damage caused onshore. [221] => [222] => [[Japan]], where tsunami science and response measures first began following a [[1896 Sanriku earthquake|disaster in 1896]], has produced ever-more elaborate countermeasures and response plans.{{cite web|url=http://journalistsresource.org/studies/government/international/tsunami-japan/ |title=Journalist's Resource: Research for Reporting, from Harvard Shorenstein Center |publisher=Content.hks.harvard.edu |date=2012-05-30 |access-date=2012-06-12}} The country has built many tsunami walls of up to {{convert|12|m|ft}} high to protect populated coastal areas. Other localities have built [[floodgate]]s of up to {{convert|15.5|m|ft}} high and channels to redirect the water from an incoming tsunami. However, their effectiveness has been questioned, as tsunamis often overtop the barriers. [223] => [224] => The [[Fukushima Daiichi nuclear disaster]] was directly triggered by the [[2011 Tōhoku earthquake and tsunami]], when waves exceeded the height of the plant's sea wall.Phillip Lipscy, Kenji Kushida, and Trevor Incerti. 2013. "[http://www.stanford.edu/~plipscy/LipscyKushidaIncertiEST2013.pdf The Fukushima Disaster and Japan’s Nuclear Plant Vulnerability in Comparative Perspective] {{Webarchive|url=https://web.archive.org/web/20131029200435/http://www.stanford.edu/~plipscy/LipscyKushidaIncertiEST2013.pdf |date=2013-10-29 }}". ''Environmental Science and Technology'' 47 (May), 6082–6088. [[Iwate Prefecture]], which is an area at high risk from tsunami, had tsunami barriers walls ([[Taro sea wall]]) totalling {{convert|25|km|mi}} long at coastal towns. The 2011 tsunami toppled more than 50% of the walls and caused catastrophic damage.{{cite news |author=Fukada, Takahiro |url=http://search.japantimes.co.jp/cgi-bin/nn20110921f1.html |title=Iwate fisheries continue struggle to recover |newspaper=[[The Japan Times]] |date=21 September 2011 |page=3 |access-date=2016-09-18}} [225] => [226] => The [[1993 Okushiri earthquake#Tsunami|Okushiri, Hokkaidō tsunami]], which struck within two to five minutes of the [[1993 Okushiri earthquake|earthquake on July 12, 1993]], created waves {{convert|30|m|ft|-1}} tall—as high as a 10-storey building. The port town of [[Aonae]] was completely surrounded by a tsunami wall, but the waves washed right over the wall and destroyed all the wood-framed structures in the area. The wall may have succeeded in slowing down and moderating the height of the tsunami, but it did not prevent major destruction and loss of life.{{cite web |url=http://www.drgeorgepc.com/Tsunami1993JAPANOkushiri.html |title=The Earthquake and Tsunami of July 12, 1993 in the Sea of Japan/East Sea |author=George Pararas-Carayannis |website=www.drgeorgepc.com |access-date=2016-09-18}} [227] => [228] => ==See also== [229] => {{Portal|Tsunamis|Oceans}} [230] => {{div col}} [231] => * {{annotated link|Emergency management}} [232] => * {{annotated link|Higher Ground Project}} [233] => * {{annotated link|Index of wave articles}} [234] => * {{annotated link|Kaikōura Peninsula|Kaikoura Canyon landslide tsunami hazard}} [235] => * {{annotated link|List of tsunamis}} [236] => * {{annotated link|List of natural disasters by death toll}} [237] => * {{annotated link|Lists of earthquakes}} [238] => * {{annotated link|Minoan eruption}} [239] => * {{annotated link|Rogue wave}} [240] => * {{annotated link|Seiche}} [241] => * {{annotated link|Sneaker wave}} [242] => * {{annotated link|Supervolcano}} [243] => * {{annotated link|Tauredunum event}} [244] => * {{annotated link|Tsunami-proof building}} [245] => * {{annotated link|List of tsunamis affecting New Zealand}} [246] => {{div col end}} [247] => [248] => ==Footnotes== [249] => {{Reflist}} [250] => [251] => ==References== [252] => * [http://itic.ioc-unesco.org/index.php?option=com_content&view=article&id=1328&Itemid=1142&lang=en IOC Tsunami Glossary] by the [[Intergovernmental Oceanographic Commission]] (IOC) at the [http://itic.ioc-unesco.org/index.php International Tsunami Information Centre] (ITIC) of [[UNESCO]] [253] => * [https://web.archive.org/web/20110225143835/http://nthmp-history.pmel.noaa.gov/terms.html Tsunami Terminology] at [[NOAA]] [254] => * In June 2011, the VOA [[Special English]] service of the [[Voice of America]] broadcast a 15-minute program on tsunamis as part of its weekly Science in the News series. The program included an interview with an NOAA official who oversees the agency's tsunami warning system. A transcript and MP3 of the program, intended for English learners, can be found at [http://www.voanews.com/learningenglish/home/science-technology/Large-Tsunamis-Do-Not-Happen-Often-But-the-Threat-is-Always-Present-123226568.html The Ever-Present Threat of Tsunamis.] [255] => * [http://www.abelard.org/briefings/tsunami.php abelard.org.] ''tsunamis: tsunamis travel fast but not at infinite speed''. retrieved March 29, 2005. [256] => * Dudley, Walter C. & Lee, Min (1988: 1st edition) ''Tsunami!'' {{ISBN|0-8248-1125-9}} [https://web.archive.org/web/20120717025233/http://www.tsunami.org/references.html website] [257] => * Iwan, W.D., ''editor'', 2006, Summary report of the Great Sumatra Earthquakes and Indian Ocean tsunamis of December 26, 2004 and March 28, 2005: Earthquake Engineering Research Institute, EERI Publication #2006-06, 11 chapters, 100-page summary, plus CD-ROM with complete text and supplementary photographs, EERI Report 2006–06. {{ISBN|1-932884-19-X}} [http://www.eeri.org/ website] [258] => * Kenneally, Christine (December 30, 2004). "Surviving the Tsunami." ''Slate''. [http://www.slate.com/id/2111608/ website] [259] => * Lambourne, Helen (March 27, 2005). "Tsunami: Anatomy of a disaster." ''[[BBC News]]''. [http://news.bbc.co.uk/1/hi/sci/tech/4381395.stm website] [260] => * Macey, Richard (January 1, 2005). "The Big Bang that Triggered A Tragedy," ''[[The Sydney Morning Herald]]'', p 11—quoting Dr Mark Leonard, seismologist at Geoscience Australia. [261] => * [http://maps.ngdc.noaa.gov/viewers/hazards/ Interactive Map of Historical Tsunamis] from NOAA National Centers for Environmental Information [262] => * Tappin, D; 2001. Local tsunamis. Geoscientist. 11–8, 4–7. [263] => * [https://www.telegraph.co.uk/news/1480192/Girl-10-used-geography-lesson-to-save-lives.html Girl, 10, used geography lesson to save lives], ''[[Telegraph.co.uk]]'' [264] => * [http://www.noypi.ph/index.php/nation/3283-key-locations-in-philippines-warned-to-prepare-for-tsunami.html Philippines warned to prepare for Japan's tsunami], ''Noypi.ph'' [265] => [266] => ==Further reading== [267] => * Boris Levin, Mikhail Nosov: ''Physics of tsunamis''. Springer, Dordrecht 2009, {{ISBN|978-1-4020-8855-1}}. [268] => * Kontar, Y. A. et al.: ''Tsunami Events and Lessons Learned: Environmental and Societal Significance.'' Springer, 2014. {{ISBN|978-94-007-7268-7}} (print); {{ISBN|978-94-007-7269-4}} (eBook) [269] => * Kristy F. Tiampo: ''Earthquakes: simulations, sources and tsunamis''. Birkhäuser, Basel 2008, {{ISBN|978-3-7643-8756-3}}. [270] => * [[Linda Maria Koldau]]: Tsunamis. Entstehung, Geschichte, Prävention, (Tsunami development, history and prevention) C.H. Beck, Munich 2013 (C.H. Beck Reihe Wissen 2770), {{ISBN|978-3-406-64656-0}} (in German). [271] => * Walter C. Dudley, Min Lee: ''Tsunami!'' University of Hawaii Press, 1988, 1998, Tsunami! University of Hawai'i Press 1999, {{ISBN|0-8248-1125-9}}, {{ISBN|978-0-8248-1969-9}}. [272] => * [[Charles L. Mader]]: ''Numerical Modeling of Water Waves'' CRC Press, 2004, {{ISBN|0-8493-2311-8}}. [273] => [274] => ==External links== [275] => {{Wiktionary}} [276] => {{Commonscat|Tsunamis}} [277] => Reporting Centers; [278] => * [http://www.jma.go.jp/en/tsunami/joho.html Tsunami alert] page (in English) from [[Japan Meteorological Agency]] [279] => * [http://www.tsunami.noaa.gov/ NOAA Centre] – [[National Oceanic and Atmospheric Administration]] [280] => * [https://www.ctic.ioc-unesco.org/ Caribbean Tsunami Information Centre] (CTIC) [281] => * [http://nctr.pmel.noaa.gov/database_devel.html Recent and Historical Tsunami Events and Relevant Data] – [[Pacific Marine Environmental Laboratory]] [282] => [283] => History & Research; [284] => * [http://itic.ioc-unesco.org/index.php?option=com_content&view=article&id=1328&Itemid=1142&lang=en IOC Tsunami Glossary] – International Tsunami Information Center ([[UNESCO]]) [285] => * [http://ngdc.noaa.gov/hazard/tsu.shtml Tsunami Data and Information] – [[National Centers for Environmental Information]] [286] => * [http://geology.com/records/biggest-tsunami.shtml World's Tallest Tsunami] – geology.com [287] => * [http://walrus.wr.usgs.gov/tsunami/ Tsunami & Earthquake Research at the USGS] – [[United States Geological Survey]] [288] => * [http://www.unesco.org/new/en/natural-sciences/ioc-oceans/ Intergovernmental Oceanographic Commission] – [[Intergovernmental Oceanographic Commission]] [289] => * [https://www.pbs.org/wgbh/nova/tsunami/ Wave That Shook The World] – ''[[Nova (American TV series)|Nova]]'' [290] => [291] => News & animations; [292] => * [https://www.youtube.com/watch?v=k4w27IczOTk Raw Video: Tsunami Slams Northeast Japan] – [[Associated Press]] [293] => * [https://www.youtube.com/watch?v=feXCIfatJYo Tsunami animation – Geoscience Australia] [294] => [295] => {{physical oceanography}} [296] => {{natural disasters}} [297] => {{Authority control}} [298] => [299] => [[Category:Tsunami| ]] [300] => [[Category:Articles containing video clips]] [] => )
good wiki

Tsunami

A tsunami is a series of ocean waves triggered by an underwater disturbance, such as an earthquake, volcanic eruption, or landslide. These waves can travel across the open ocean at high speeds, reaching the coastline with devastating force.

More about us

About

These waves can travel across the open ocean at high speeds, reaching the coastline with devastating force. The word "tsunami" comes from the Japanese language, where it means "harbor wave. " The Wikipedia page on tsunamis provides detailed information about these natural disasters. It covers various aspects, including the causes and characteristics of tsunamis, as well as their historical occurrences and impacts on human populations and the environment. The page also discusses the science of detecting and monitoring tsunamis, and the efforts made to mitigate their destructive effects. The article highlights some of the most significant tsunamis in history, dating back to ancient times. It mentions the devastating Indian Ocean tsunami in 2004, which claimed the lives of hundreds of thousands of people and caused widespread destruction. The Fukushima Tsunami in 2011, triggered by a powerful earthquake in Japan, is also discussed, emphasizing the widespread damage and the subsequent nuclear disaster. The impacts of tsunamis on coastal communities are examined, including the destruction of infrastructure, loss of life, and economic consequences. The article also explores the aftermath of tsunamis, such as the need for disaster response and recovery, as well as the importance of early warning systems to save lives. Overall, the Wikipedia page on tsunamis provides a comprehensive overview of this natural phenomenon, offering readers a wealth of information about their causes, impacts, and the ongoing efforts to understand and mitigate them.

Expert Team

Vivamus eget neque lacus. Pellentesque egauris ex.

Award winning agency

Lorem ipsum, dolor sit amet consectetur elitorceat .

10 Year Exp.

Pellen tesque eget, mauris lorem iupsum neque lacus.

You might be interested in

Earthquake

An earthquake is a natural occurrence that involves the shaking and trembling of the Earth's surface.

MOON

The Moon is Earth's only natural satellite and is the fifth-largest satellite in the Solar System.

NOAA

Seismologist

Sun

The Sun is the star at the center of the Solar System, and it is by far the most important source of energy for life on Earth.