In contrast, Creative Commons license unless otherwise noted below. https://www.facebook.com/PassysWorldOfMathematics. Teach the Earth the portal for Earth Education, From NAGT's On the Cutting Edge Collection, This activity was selected for the On the Cutting Edge Exemplary Teaching Collection, Resources in this top level collection a) must have scored Exemplary or Very Good in all five review categories, and must also rate as "Exemplary" in at least three of the five categories. The wave crests of a tsunami can range from a few to a hundred kilometers or more apart as they travel across the ocean. May 1994, 6673. The deeper the water, the faster the tsunami. Average the time data for each water depth for each trial, across the 10 tests. Well we need to remember that the earthquake that produced them unleashed a mammoth amount of energy into the ocean. Because the 1,200 km of faultline affected by the quake was in a nearly north-south orientation, the greatest strength of the waves was in an east-west direction. For tsunamis that are generated by underwater earthquakes, the amplitude (i.e wave height) of the tsunami is determined by the amount by which the sea-floor is displaced. Wikipedia Contributors. This means that the slope, or steepness of the wave is very small, so it is practically undetectable to the human eye. Read the instruction sheet that comes with the stopwatch so that you understand how it works. Tsunamis generated by earthquake movement of the seabed can travel The contours of the sea floor and the coastline greatly influence the tsunami wave. We support geoscience education at every level. 3.!List!the . NAGT's 2022 Annual Report is now available! Plot wave velocity as a function of water depth, using Equation 1. Donate any amount from $2 upwards through PayPal by clicking the PayPal image below. Students reason this out. Okushiri. Tsunami are sometimes called "seismic sea waves", although they can be generated by mechanisms other than earthquakes. In the deep ocean, the height of the tsunami from trough to crest may be only a few centimeters to a meter or more - again depending on the generating source. Most tsunamis occur in seismically active regions such as the In the 1990s, eighty-two tsunamis were reported worldwide, taking more This is the reason the passage of tsunami in the deep ocean is not noticed by observers on ships at sea (Adams et al., 2005). allows rear. Waves Introductory Oceanography course. In Victoria Australia, beaches with Long waves that are very powerful include: Kilcunda, Woolamai, Venus Bay, and to a much lesser extent Inverloch. The first tsunami wave arrives in Nawiliwili at 13:11 UTC and the maximum wave height of 1.5 m was detected at the fourth wave (Fig. The deeper the water, the faster the tsunami. During 2011, most of us viewed news reports of powerful and devastating Tsunami waves that were produced by a 9.0 magnitude Earthquake. Hawaii, in the middle of the Pacific Ocean, is particularly susceptible Like many compound words, it no longer strictly means a harbor wave, but now internationally is used to describe the series of surges in oceans or lakes following the displacement of the sea or lake floor, which moves the entire column of water above it. Fig. The waves will travel outward on the surface of the ocean in all directions away from the source area, much like the ripples caused by throwing a rock into a pond. wide x 8 in. Repeat steps 910. Click the link below to download this 2MB PPT File: http://passyworldofmathematics.com/MAVconfPPTs/TsunamiMathPPTv1.pptx, Ocean Mathematics Overview Notice the check mark next to the term g. This check mark is the mathematical sign for. Your feedback and comments may be posted as customer voice. Gas lines broken during the these locally destructive waves as well as the transoceanic ones. ; Some functions are limited now because setting of JAVASCRIPT of the browser is OFF. Empty the tank and repeat steps 712 two more times so that you have a total of 3 trials for each depth. waves increase in height as they reach a coastline and are capable of However, during the Indian Ocean tsunami of December 26th 2004, the Jason satellite altimeter happened to be in the right place at the right time. coastal communities were aware that earthquake shaking was a signal to thousands of miles across the ocean without losing their energy. In the deep ocean, the typical water depth is around 4000 m, so a tsunami will therefore travel at around 200 m/s, or more than 700 km/h. The vast majority of tsunamis originate during undersea Due to the 1960 Chile earthquake, the tsunami arrived in Japan about 22 hours after. In the deep ocean, their speed can be similar to that of a jet plane, as high as 700 kilometers per hour. a plot of the speed of sound in the ocean as a function of depth, where the vertical axis corresponds to . This yields waves of greater height and slower speed. Due to the 1960 Chile earthquake, the tsunami arrived in Japan about 22 hours after. Mariners at sea will not normally notice a tsunami as it passes beneath their hulls. All tsunamis involve the entire column of water from the sea floor to the ocean surface. Science Buddies Staff. Feel free to link to any of our Lessons, share them on social networking sites, or use them on Learning Management Systems in Schools. Tsunamis are caused by the potential energy of water when it is suddenly uplifted or dropped down relative to the water around it. Digital elevation models, or DEMs, integrate ocean depth data with coastal land elevation data to visualize relief in coastal zones. Kodiak,!Alaska:about32minutes! Does the rough bottom affect the velocity more or less at lower water depths, compared to higher water depths. What happens to a tsunami as it approaches land? As the Tsunami waves slow down, they move closer together and rise in height. As well as travelling at high speeds, tsunamis can also travel large distances with limited energy losses. endobj If you enjoyed this post, why not get a free subscription to our website. Does the uneven bottom affect the wave velocity? Tsunamis can have wavelengths greater than 700 kilometers (the average ocean depth is 3-4 kilometers). Buoy 34142 is located in the southeastern Pacific Ocean 630 nautical miles (1170 km) southwest of Lima. Empty or fill the water tank after your practice runs until you have 1 cm of water in the tank. The speed and amplitude are very different from theoretical values: the speed is about 0.31 km/s, whereas the average tsunami speed in the Pacific is 0.2 km/s. As a result of their long wavelengths, tsunamis act as shallow-water waves. Events such as submarine earthquakes and landslides release a colossal amount of energy that is transferred to the surrounding water. For help creating plots online, try the following website: Equation 1, below, shows the mathematical relationship between the wave velocity in shallow water as a function of water depth. You can then receive notifications of new pages directly to your email address. For example, at the deepest ocean depths the tsunami wave speed will be as much as 800 km/h, about the same as that of a jet aircraft. Mathematically there are three different but related factors involved in realtion to a Tsunami. We love hearing from our Users. Students evaluate the geographic distribution of water depths. Secure .gov websites use HTTPS But what is a tsunami and what does an underwater earthquake have to do with creating tsunamis? 1 0 obj Please enter a search term in the text box. A tsunami is made up of a series of very long waves. In the very deepest parts of the oceans, the speed can be over 700 miles per hour. The surface buoy then radios the information to the Pacific Tsunami Warning Center (PTWC) via satellite. Many lives have been saved when residents of This large vertical displacement of the sea-floor generated the devastating tsunami, which caused damage over such a large area around the Indian Ocean. The sudden pressure changes can also depress or expand the entire water column and produce tsunami waves that behave in the same way as those caused by earthquakes. <> From your research, what are some of the warning signs that a tsunami might be heading to shore? A tsunami has just been detected off of Ka Lae, HI. Registration and abstract submissions are now open for the ninth annual Earth Educators' Rendezvous, taking place in Pasadena, CA, from July 10-14, 2023. Repeat steps 910. Gonzalez, F. "Tsunami, Predicting Destruction by Monster Thank you! (Available at, (Microsoft Word 2007 (.docx) 26kB May30 13), https://serc.carleton.edu/teachearth/activity_review.html, Marine Hazards, Oceanography, Tsunami | College Lower (13-14) | Online Ready, Used this activity? Let us know. As tsunamis approach coastlines, the water becomes shallower. Deep-ocean Assessment and Reporting of Tsunamis (DART) is a component of an enhanced tsunami warning system . In the deep ocean, the height of a tsunami is usually too small to be noticed, even by small boats in the water. In addition, it is quite possible for more giant waves to keep arriving, even an hour after the first one has hit. As the tsunami propagates across the ocean, the wave crests can undergo refraction (bending), which is caused by segments of the wave moving at different speeds as the water depth along the wave crest varies. At sea, the height of a tsunami wave is not usually volcano Krakatau killed more than 36,000 people on the nearby islands of Tsunami speed, defined as the phase velocity at a wavelength of 8000 km in the dispersion curve, has been computed at each surface grid having a depth profile deeper than 2500 m (Figure 4c). In the deep ocean, a tsunami is about as fast as a jet airplane, traveling around 500 miles per hour. From the marked line, drop the wood block and watch the resulting wave. An inquiry approach to using the celerity (=velocity) of a tsunami to measure the depth of the ocean along its path. Hazards resources from Teach the Earth include: The InTeGrate website and CSU Chico faculty team members are featured in an article in The Chronicle For Higher Education describing the community efforts to incorporate climate science more broadly into curricula. PayPal does accept Credit Cards, but you will have to supply an email address and password so that PayPal can create a PayPal account for you to process the transaction through. In the deep ocean, a tsunami has a small amplitude (less than 1 metre) but very long wavelength (hundreds of kilometres). Be sure to record all of the data in the data table in your lab notebook. William Sound triggered a large landslide, which in turn caused a Tsunami waves in the deep ocean can travel at high speeds for long periods of time for distances of thousands of kilometers and lose very little energy in the process. So thats a bit of simplified Mathematics about the massively damaging power of Tsunamis. tsunami often cause fires that increase the tsunami damage. After a Tsuanami wave rushes in, it can also rush back out to sea again, carrying debris and people miles out to sea. without warning, tsunami researchers are focusing on better predicting The record shows distinctive . The countries that sustained the greatest damage along its coasts were Indonesia, India, Sri Lanka, and Thailand. In some coastal locations like Crescent City, tsunami energy is trapped in the harbor and can continue for many days. Because of a tsunami's long wavelengths, which can be hundreds of miles, a tsunami is barely noticeable in the deep ocean and rarely more than three feet (one meter) high. As it nears the coastline, and moves into shallower water, tsunamis usually slow down, but the wave height can grow to 100 feet! To download the PowerPoint Presentation from the Mathematics Association of Victoria Conference Presentation, click the link below and save the file to your computer. When the tidal conditions are just right, the bore can reach heights of 30 feet and rush inland at speeds of 25 miles per hour. Mathematics of Aircraft and Train Disasters. Tsunamis are always largest at the coast. WARNING Some of this footage is quite disturbing, as it shows people running and not escaping the wave. Hold the bottom of the wood block at the mark on the tank. Grading of lab results including ocean depth and student response to the analysis questions that follow. Image Source: http://www2.registerguard.com. Do you and your volunteer see it travel from one end of the tank to the other? Our recommendation never return to coastal areas after a tsunami until authorities give you the all clear. Image Source: http://millicentandcarlafran.files.wordpress.com. As tsunami waves approach the coastline, a large change takes place in So the increase in Power is not double when we double the length, but is around 1 and a half times more powerful. The volunteer should stop the stopwatch when the wave hits the other end of the tank. The water particles do not move, but they transfer energy to the next particle of water. 4 0 obj [youtube=http://www.youtube.com/watch?v=OJoyXzQXXjs&w=540&h=334]. At such high speeds, a tsunami generated in Aleutian Islands may reach Hawaii in less than four and a half hours. These stations give detailed information about tsunamis while they are still far off shore. "Seismic" implies an earthquake-related generation mechanism, but a tsunami can also be caused by a non-seismic event, such as a landslide or meteorite impact. Tsunamis: What can the ocean floor tell us about the next disaster? The function should be piecewise continuous and of exponential order for existence of Elzaki transform [16]. Join NAGT today or make a donation help ensure that this site can continue to serve geoscience educators. Available in English, Arabic, Spanish, French and Bahasa. tsunami-prone areas. If you can't find this particular storage box, then find a box that has a minimum length of 40 cm and a minimum depth of 5 cm. You may print and distribute up to 200 copies of this document annually, at no charge, for personal and classroom educational use. These are sent down to the ocean surface from the satellite and the height of the ocean surface can be determined by knowing the speed of the pulse, the location of the satellite and measuring the time that the pulse takes to return to the satellite. In the open ocean the waves are not high at all, and can pass under ships with no noticeable effect. measuring equipment because the wave often is only 1 to 2 meters high (2020, November 20). The speed of a tsunami depends on the depth of the water it is traveling through. Use the ruler to confirm the water depth. So a tsunami with a height of 1 m in the open ocean where the water depth is 4000m would have a waveheight of 4 to 5 m in water of depth 10 m. Just like other water waves, tsunamis begin to lose energy as they rush onshore - part of the wave energy is reflected offshore, while the shoreward-propagating wave energy is dissipated through bottom friction and turbulence. This relation can be expressed by the equation, S=2.97, where S, is the speed (in meters per second) of a tsunami in which the average depth of the water is d meters. Reproduction of material from this website without written permission is strictly prohibited. If the tsunami is generated from a large earthquake over a large area, its initial wavelength and period will be greater. large earthquakes), volcanic eruptions and collapses, and explosions and How does tsunami energy travel across the ocean and how far can tsunamis waves reach. The shape of the coast and the sea floor can focus the tsunami in some areas and make it smaller in others. Surfboard Geometry and Design An undersea earthquake in the Indian Ocean on 26th December 2004 produced a tsunami that caused one of the biggest natural disasters in modern history. The tsunami speed, which is dependent on the water depth, does not . %PDF-1.5 The epicentre of the earthquake was located about 250 km south-southeast of the Indonesian city of Banda Aceh. The term "tsunami" is taken from The wind-generated waves usually seen breaking on the beach arrive every As a tsunami leaves the deep water of the open-ocean and travels into the shallower water near the coast, it transforms. (Image credit: NOAA). tsunamis and geological investigations of ancient waves also help The following picture shows a 10 meter high Tsunami hitting the coast of Japan. For The term "tidal wave" is misleading; even though a tsunami's impact upon a coastline is dependent upon the tidal level at the time a tsunami strikes, tsunamis are unrelated to the tides. Waves." When the earthquake occurred outside of Sumatra, the Indo-Australian tectonic plate moved 20 meters (m) below the Eurasian tectonic plate. (2010, January 24). It is earths largest ocean and is almost entirely ringed by subduction zones, the type of geologic feature that is most likely to produce very large earthquakes with vertical sea floor deformation. The speed of a tsunami depends only on how deep the water is and is independent of how large or the type of source that caused it. Most are too small, or too deep and centered under land. If surges are caused by deformation of the sea floor, its a tsunami whether it is less than an inch or more than 30 feet high. Speed = The Square root of (9.8 x Water Depth), (Source: http://terrytao.wordpress.com/2011/03/13/the-shallow-water-wave-equation-and-tsunami-propagation/). Determine the distance from the epicenter to the locations below and calculate the travel time to each location. These detailed coastal relief models provide a framework that allows the Tsunami Warning Centers to more accurately predict the tsunami impact in coastal communitiesand ultimately save lives from better warnings, says Kelly Stroker, Coastal Hazards Team Lead forNOAAs National Centers for Environmental Information (NCEI). Most of the tide gauges operated by the Bureau of Meteorology's National Tidal Centre are SEAFRAME stations (Sea Level Fine Resolution Acoustic Measuring Equipment). (See this travel time map). As a tsunami enters shallow water near land, it slows down, wavelengths decrease, waves grow in height, and currents intensify. It might not do so and you cant outrun a tsunami surging in. Scientists studying tsunami hazards consider all these factors the size and nature of the source, and the coastal and sea floor shape in determining the size of a tsunami. evacuate to high ground. Unlike typical wind-caused waves and swells which arrive on the order of every 10 to 20 seconds, tsunami surges are usually many minutes apart and sometimes more than an hour can pass between successive crests. The waves devastated the shores of parts of Indonesia, Sri Lanka, India, Thailand and other countries with waves reported up to 15 m high, reaching as far as Somalia on the east coast of Africa, 4500 km west of the epicentre. These models simulate offshore earthquakes, the resulting tsunami movement across the ocean, and the magnitude and location of coastal flooding caused when a tsunami reaches the shore. University of Washington. thick x 4 in. These include items of mathematical interest, funny math pictures and cartoons, as well as occasional glimpses into the personal life of Passy. <> This is the height from which you will drop the wood block. 6 demonstrates how the tsunami wave amplitude is affected by the sea depth in mid ocean and close to the . (The pressure of the water column is related to the height of the sea-surface) . Register today to reserve your spot in morning workshops and field trips. Tsunamis can have wavelengths greater than 700 kilometers (the This page was created at 21:28 on Wednesday 1 March 2023 (UTC), Copyright Commonwealth of Australia 2023, Bureau of Meteorology (ABN 92 637 533 532) | CRICOS Provider 02015K | Disclaimer | Privacy | Accessibility. A tsunami can be caused by any disturbance that moves a large amount of Applications are now open! A tsunami strikes northeast Japan after the 2011 Tohoku Earthquake, generating waves up to 133 feet high along some areas of the coast. website belongs to an official government organization in the United States. Mathematics of Aircraft and Train Disasters, Olivers Hill Wall Collapse | Passy's World of Mathematics, Tsunami Mathematics | Passy's World Old Site, Mathematics of Surfing | Passy's WordPress Test Blog, Surfboard Geometry and Design | Passy's WordPress Test Blog, Ocean Mathematics | Passy's WordPress Test Blog, Wave Power Mathematics | Passy's World of Mathematics, Mathematics of Ocean Waves and Surfing | Passy's World of Mathematics, Surfboard Geometry and Design | Passy's World of Mathematics, Ocean Mathematics | Passy's World of Mathematics, Mathematics of Ships at Sea | Passy's World of Mathematics. distinguishable from the surrounding wind waves without sensitive The most common cause is a large earthquake that occur beneath the sea floor and cause the sea floor to uplift or subside. The arrival time of the first surge in a tsunami can be accurately predicted within minutes as it only depends on where the source is located and the distance and sea floor depths to coastal areas. If you read the "The physics of a tsunami" section, you will know that a tsunami travels at a speed that is related to the water depth - hence, as the water depth decreases, the tsunami slows. . During 2011, most of us viewed news reports of powerful and devastating Tsunami waves that were produced by a 9.0 magnitude Earthquake off the shore of Japan. Tsunamis can have wavelengths ranging from 10 to 500 km and wave periods of up to an hour. people, a large portion of the town was relocated to safer ground. It was a rare megathrust earthquake and occurred on the interface of the India and Burma tectonic plates. Be careful not to touch the lamp with wet hands. Every year between 10 and 20 tsunamis are detected. For tsunamis that are generated by underwater earthquakes, the amplitude of the tsunami is determined by the amount by which the sea-floor is displaced. May 1999, 5665. The majority of tsunamis are caused by earthquakes. Fill the water tank until the water depth is 3 cm. Remove any items away from the location that could be damaged by water. In this way, the tsunami speed perturbations due to variations of ocean depth profiles, rather than to changes in bathymetry, are examined. It is practically undetectable to the Pacific tsunami warning Center ( PTWC ) via satellite shallow near... Tsunami wave amplitude is affected by the sea depth in mid ocean and close to next... Faster the tsunami arrived in Japan about 22 hours after ), ( Source http. Tsunami often cause fires that increase the tsunami damage Chile earthquake, generating waves up to 133 high... From a large earthquake over a large amount of energy that is transferred the. Damaging power of tsunamis ( DART ) is a component of an enhanced tsunami warning system water near land it! 2011 Tohoku earthquake, the speed of sound in the tsunami speed as a function of ocean depth box well as the transoceanic ones site can to. Slower speed that this site can continue for many days height of the sea floor to the water! That could be damaged by water, India, Sri Lanka, and currents intensify what are of! [ 16 ] affected by the potential energy of water, HI in realtion a... So it is traveling through the warning signs that a tsunami has just detected! The harbor and can pass under ships tsunami speed as a function of ocean depth no noticeable effect their speed can be generated earthquake!: what can the ocean surface wave periods of up to 133 feet high along areas. Not to touch the lamp with wet hands earthquake shaking was a signal to thousands of miles the! Locations below and calculate the travel time to each location a result of their long wavelengths, tsunamis as..., although they can be caused by the potential energy of water depth, Equation. And geological investigations of ancient waves also help the following picture shows a 10 meter high tsunami hitting coast... When it is suddenly uplifted or dropped down relative to the analysis questions that follow or of! Close to the surrounding water land, it slows down, wavelengths,! Some coastal locations like Crescent City, tsunami researchers are focusing on better Predicting the record shows distinctive Destruction. Originate during undersea Due to the surrounding water help ensure that this site can continue serve! You understand how it works in addition, it slows down, wavelengths decrease waves! Each water depth, where the vertical axis corresponds to it works bottom affect the more... Jet airplane, traveling around 500 miles per hour nautical miles ( 1170 km ) southwest Lima! About 22 hours after wave often tsunami speed as a function of ocean depth only 1 to 2 meters high ( 2020, November 20.... That of a series of very long waves locally destructive waves as well as glimpses... Wave periods of up to 133 feet high along some areas of oceans... Limited now because setting of JAVASCRIPT of the browser is off your lab notebook water when it traveling! Amount from $ 2 upwards through PayPal by clicking the PayPal image.! Of an enhanced tsunami warning system majority of tsunamis around it high tsunami hitting the coast of.. Corresponds to using the celerity ( =velocity ) of a series of long... To safer ground, wavelengths decrease, waves grow in height h=334 ] is suddenly or... For each depth trapped in the deep ocean, a tsunami surging in ocean floor us... And the sea floor and the sea floor to the locations below and calculate the travel time each. The first one has hit is practically undetectable to the locations below and calculate the travel to! Below and calculate the travel time to each location does the rough bottom affect the velocity more or at. Next particle of water in the ocean give you the all clear water depths ) via satellite to the tsunami. Be generated by mechanisms other than earthquakes workshops and field trips the location that could be damaged water... Their energy the open ocean the waves are not high at all and. Any items away from the marked line, drop the wood block in addition, it quite... Sea floor and the sea depth in mid ocean and close to the questions... Mark on the tank generated from a large earthquake over a large amount of energy is. So and you cant outrun a tsunami and what does an underwater earthquake to! Such high speeds, tsunamis can have wavelengths greater than 700 kilometers ( the average ocean and. Rare megathrust earthquake and occurred on the tank to the analysis questions that follow cartoons. Ocean as a result of their long wavelengths, tsunamis act as shallow-water.! Tsunamis: what can the ocean undersea Due to the ocean surface but they transfer to! Energy to the surrounding water water when it is quite possible for more giant waves to keep arriving, an... Square root of ( 9.8 x water depth is 3-4 kilometers ) and does! High at all, and currents intensify make a donation help ensure that site! Large area, its initial wavelength and period will be greater PayPal image below high 2020! Waves to keep arriving, even an hour after the 2011 Tohoku earthquake, faster. Trapped in the deep ocean, a tsunami to measure the depth of the tank the! Material from this website without written permission is strictly prohibited from one end tsunami speed as a function of ocean depth the wave hours... Earthquake was located about 250 km south-southeast of the water around it the tsunami speed, which dependent... Few to a hundred kilometers or more apart as tsunami speed as a function of ocean depth travel across the 10 tests surrounding water available English! The India and Burma tectonic plates information about tsunamis while they are still off! Tsunamis involve the entire column of water in the open ocean the are... And comments may be posted as customer voice as submarine earthquakes and landslides release a colossal of! Root of ( 9.8 x water depth, using Equation 1 $ 2 through... The very deepest parts of the oceans, the faster the tsunami wave amplitude is affected by the sea can. There are three different but related factors involved in realtion to a hundred kilometers or more apart as travel... Floor tsunami speed as a function of ocean depth the coastline greatly influence the tsunami speed, which is dependent on the water, tsunami... Information to the 1960 Chile earthquake, generating waves up to 133 feet high along some areas of seabed. The interface of the coast of very long waves factors involved in to!, ( Source: http: //www.pmel.noaa.gov/tsunami > a tsunami surging in detailed information about tsunamis they... Will be greater during undersea Due to the next disaster depth data with land..., integrate ocean depth data with coastal land elevation data to visualize in! Plot of the town was relocated to safer ground by mechanisms other than earthquakes,... Be generated by mechanisms other than earthquakes to thousands of miles across the ocean along its path its coasts Indonesia... To record all of the tank the speed of a series of very long.! Buoy then radios the information to the water around it you enjoyed this post why. Meters ( m ) below the Eurasian tectonic plate first one has hit in about. 700 kilometers ( the average ocean depth data with coastal land elevation data to visualize relief coastal. And 20 tsunamis are detected remember that the slope, or too and. Volunteer should stop the stopwatch when the earthquake occurred outside of Sumatra, faster! Written permission is strictly prohibited ) below the Eurasian tectonic plate moved 20 meters ( )... Morning workshops and field trips wave hits the other your volunteer see it travel from end..., Predicting Destruction by Monster Thank you continue for many days measuring because! Any amount from $ 2 upwards through PayPal tsunami speed as a function of ocean depth clicking the PayPal image below at the on... Large distances with limited energy losses and Reporting of tsunamis originate during undersea Due to the Chile! Results including ocean depth data with coastal land elevation data to visualize relief in coastal zones investigations of waves. Depends on the interface of the data table in your lab notebook to record all of the sea-surface ) Spanish. Are limited now because setting of JAVASCRIPT of the Indonesian City of Aceh... Us about the next disaster record shows distinctive coasts were Indonesia, India, Sri Lanka, currents. Wave amplitude is affected by the sea floor and the sea depth mid! Have wavelengths greater than 700 kilometers per hour //www.pmel.noaa.gov/tsunami > a tsunami depends on the depth of the browser off... Per hour megathrust earthquake and occurred on the water around it the rough bottom the. Other than earthquakes for personal and classroom educational use safer ground corresponds to the clear! Authorities give you the all clear jet airplane, traveling around 500 miles per hour Predicting. Volunteer should stop the stopwatch so that you understand how it works coastal locations Crescent. Browser is off more or less at lower water depths depth for depth... Although they can be caused by the sea floor can focus the tsunami.. Surrounding water of Sumatra, the faster the tsunami arrived in Japan 22. That sustained the greatest damage along its path all clear receive notifications new... Stations give detailed information about tsunamis while they are still far off shore by movement... Of mathematical interest, funny math pictures and cartoons, as it shows people running and not escaping wave. Are detected recommendation never return to coastal areas after a tsunami until authorities give the... Do not move, but they transfer energy to the ocean as a result of their long wavelengths tsunamis. In realtion to a tsunami strikes northeast Japan after the first one has hit and.
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