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  Service overview 
  
 
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                        |  The system predicts inundation area and its water depth caused by possible
                        Tsunami by using the difference method of Shallow-water theory. It also
                        evaluates wave power, calculates drift carrying capacity, the wave height
                        and the velocity at mesh points and generates distribution map of tsunami
                        wave height.
 |  |  Planned to link with UC-win/Road
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                        |  |  UC-win/Road Ver.5 |  
                        | UC-win/Road xpswmm plug-in Ver.2 (for Tsunami) $3,000 (+tax)
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                    Tsunami reproducing function by 3D Virtual Reality UC-win/RoadYou can set the position, range and height with a visual option as well as tsunami generation by linking with xpswmm.(Japanese)
 
 >> Public sector solution: Tsunami Analysis Service
 
 
 
                      
                        
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                          |  Simulation result by xpswmm |  |  Screen for setting Tsunami |  
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            |  |  Mechanism of tsunami generation | 
          
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                  | If an earthquake occurs, the uplift or subsidence is caused by ground movement
                  under the sea bottom. With this movement, the overlying water vertically
                  displaced, and the spread of water generates tsunami. When tsunami warning
                  is announced, ships inside port go out of the port to avoid tsunami strike.
                  That is because the energy of tsunami is smaller due to the deep water
                  compared with shallow water area. The word tsunami derives from the larger
                  damage on ships in the port (=tsu) compared with that of offshore. Currently,
                  the word "tsunami", is also used in English. The velocity of
                  tsunami is obtained by multiplying the gravity by water depth and rooting
                  the value(v=ăgd). If the water depth is 4000m and the velocity of tsunami
                  is approximately 720km/h(200m/S). It almost ties that of jet airplane. |  |  
  image of tsunami occurrence |  
 
 
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            |  |  Recent tsunami devastated areas | 
          
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                  |  Animated simulation of the 2004 Indian Ocean Tsunami disaster |  
 
 
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            |  |  Several functions of coastal forest in Japan (Hamada & Imamura,2003) | 
          
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            |  |  Tsunami analysis case | 
          
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                    OverviewNumerical calculation of tsunami at Imamura laboratory adapts the difference
                    method of shallow water theory. As for tsunami simulation, the laboratory
                    conducts run-up simulation which predicts inundation area and its water
                    depth caused by possible Tsunami. Through the calculation, It evaluates
                    wave power, calculates drift carrying capacity, the wave height and the
                    velocity at mesh points and generates distribution map of tsunami wave
                    height. Information on submarine topography includes documents published
                    by Japan Coast Guard.
 
 
Input condition etc.The condition to be entered includes epicenter information (magnitude,
                    dept and position) and submarine topography data (altitude and position).
 
 
Analysis sample caseThis is the case of Fukushima Earthquake, which occurred July 19th, 2008.
                    Magnitude of the earthquake: M=6.6, depth of epicenter: about 10km.This
                    case shows that the result of analysis is close to the estimation of meteorological
                    agency, while the arrival time is 20 minutes later than that of meteorological
                    agency.
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  distribution map of maximum tsunami wave height |  
 
 
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            |  |  Link with Tsunami analysis code of Imamura laboratory | 
          
            |  | FORUM8 will start analysis support service and make a link between the
            analysis code and UC-win/Road, by using the code developed by the laboratory.
            The analysis code can be adopted to the creation of hazard maps and the
            forecast of tsunami evacuation.FORUM8 is going to start a new service below.
 
 
 
              
                
                  | Tsunami analysis code support service |  
                  | The service reduces the load of data entry by transferring the basic data
                  of topography, buildings, trees and etc from UC-win/Road. After importing the calculation result of the analysis code, UC-win/Road
                  visualizes the analysis.
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            |  |  Research activity at Imamura Laboratory of Tohoku University | 
          
            |  | Tsunami Engineering Laboratory (Professor Fumihiko Imamura) studies Tsunami
            and the followings are its research activities.Natural disaster is caused
            by the interaction between natural phenomena and human society. Damage
            phase is constantly changing depending on the evolving civilization. Developing
            countermeasures against tsunami disaster is one of the significant issues
            for coastal communities, which has been realized to be more important especially
            after the 2004 Indian ocean tsunami. The Tsunami Engineering Laboratory
            in DCRC, Tohoku University is the only one laboratory that studies tsunami
            disasters based on engineering approach. Based on the philosophy of prevention
            and control, their research focuses on field research work in Japan and
            abroad, development of prediction system based on numerical modeling technique
            and support for disaster prevention activities in local community. Especially,
            TIME (Tsunami Inundation Modeling Exchange) project is representative of
            our efforts, which transfers numerical modeling technique to more than
            7 countries and communities at risk. The project is supporting the reconstruction
            and disaster prevention activities in the tsunami damaged countries.
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