Answer 1 of 23: Hi we planing to gi Hokkaido in mid July 2011, but we have no idea is Hokkaido affected by the Tsunami ? This is an alphabetically sorted list of cities and towns severely damaged by the 2011 Tōhoku earthquake and tsunami.Cities and towns listed here reported at least US$100,000 in damage or at least one death. Pure Appl Geophys 170:1229–1248Cheung KF, Bai Y, Yamazaki Y (2013) Surges around the Hawaiian islands from the 2011 Tohoku tsunami. YY helped the interpretation of the results. Satake K, Shimazaki K (1987) Computation of tsunami waveforms by a superposition of normal modes, J. Phys. This suggests that the later tsunami waves arrived at the Hokkaido coast after propagating along the Pacific coast of the Tohoku region with repeated inundations far inland or reflecting from the coast of Tohoku after the inundation. Large future tsunamis might excite the first mode of Hakodate Bay and cause large later phases near the Hakodate port. I have found some of the reports on Aussie TV insensitive and ghoulish to say the least. Model approach and synthetic tsunamis. The 2011 Tohoku earthquake tsunami arrived at Hokkaido one hour after the earthquake occurred at 14:46 on 11 March 2011 (see overall features of the tsunami in Mori et al. The earthquake took place some 200 kilometers away from the Japan's coast, and it took 10 or 15 minutes for the tsunami to reach land. Hokkaido had 3 strong tremors on Friday March 11th, and areas in Hakodate, Tomakomai and Kushiro/Nemuro were hit by 2-3 meter high tsunami waves that caused flooding in areas. $$ {H}_n\left(\omega \right)={e}^{-\alpha {\left(\frac{\omega -{\omega}_n}{\omega}\right)}^2} $$$$ \frac{\partial^2h}{\partial {t}^2}=\mathrm{g}\nabla \bullet \left(d\nabla h\right) $$$$ h\left(x,y,t\right)=\Phi \left(x,y\right)\exp \left( i\omega t\right) $$$$ \nabla \bullet \left(d\nabla \Phi \right)=\lambda \Phi \kern1.25em \mathrm{where}\ \lambda =-{\omega}^2/\mathrm{g}. But it is.Tiny amounts of radiation are reaching here of course - but it reached the Uk too.There are occasional earthquakes, just vibration level really now for about 5 days.There is water, toilet rolls, tissue paper, vegetables, fish etc in all the shops.Local governments are prepping public housing for evacuees from the disaster area and there are many charity events.Hokkaido is NOT a disaster zone. This later tsunami was generated by an edge wave that propagated across the large shallow water area off Cape Erimo, Hokkaido (Tanioka and Katsumata In this study, we computed 10 h of the 2011 Tohoku tsunami after the origin time of the earthquake. Amplitudes are given in decibels based on the maximum amplitudeEigenfunctions, that is, the spatial distributions of the water heights, and eigen periods of the first mode (This study shows that the later tsunami phases along the Pacific coast of the Hokkaido region, which were computed by solving the non-linear shallow water equations with a moving boundary condition, explain the observed tsunamis much better than those computed by solving the linear shallow water equations. The results also indicate that the tsunami wave heights near the Hakodate port area, the most populated area in Hakodate, are the largest in the bay because of the resonance of the fundamental mode of the bay. World Scientific, Singapore, pp 231–241Japan Meteorological Agency (2012) Report on the 2011 off the Pacific coast of Tohoku earthquake, Technical Report of the Japan Meteorological Agency, 133, 479 pp. Impact at Crescent City by distant scattering. The normal modes of Hakodate Bay were also computed to obtain the eigen periods, eigenfunctions, and spatial distribution of water heights. This indicates that the tsunami inundation computations along the Tohoku and Hokkaido coasts are necessary to reproduce the later phases of the observed tsunami in Hakodate on Hokkaido. You can also search for this author in
Goto C, Ogawa Y, Shuto N, Imamura F (1997) Numerical method of tsunami simulation with the leap-flog scheme, IUGG/IOC TIME project, IOC manual and guides, vol 35, Paris, pp 1–126.
Citizens need to be evacuated from tsunami-affected areas for a much longer time than expected.Borrero JC, Bell R, Csato C, DeLange W, Goring D, Greer SD et al (2013) Observations, effects and real time assessment of the March 11, 2011 Tohoku-oki tsunami in New Zealand. Wu Y, Satake K (2018) Synthesis and source characteristics of tsunamis in the sea of Japan based on normal-mode method. Jepun bakal dilanda gempa, tsunami lebih dahsyat daripada bencana 2011 - Pakar Gempa bumi besar berskala 8.8 atau lebih dijangka melanda bahagian Timur Hokkaido, Jepun pada bila-bila masa sahaja. Thank you. That's not a lot of time. 2012). By using this website, you agree to our The spectral analysis of the observed waveform at Hakodate tide gauge shows that the later tsunami that arrived between 7.5 and 9.5 h after the earthquake mainly contains a period of 45–50 min. The later tsunami waves mainly excited the first mode of the bay after propagating along the Pacific coast of the Tohoku region.The eigenfunction of the first mode, that is, the spatial water height distribution, is the largest near the Hakodate port area, which is the most populated and famous tourist area in Hakodate. A period-time plot for the 2011 Tohoku-oki tsunami observed at a tide gauge in Hakodate. Earth Planets Space 63:55. In this study, we chose the same value as that used in Rabinovich et al. The residents and local disaster management office of Hakodate should be aware that there is a high possibility of large later tsunamis near the Hakodate port area when a tsunami warning is issued from the JMA. Part of J Geophys Res: Oceans 118:5703–5719. However, the largest phase of the tsunami arriving surprisingly late in Hakodate in Hokkaido, Japan; that is, approximately 9 h … Geophys J 93:457–463Tanioka Y, Hasegawa Y, Kuwayama T (2008) Tsunami waveform analyses of the 2006 underthrust and 2007 outer-rise Kurile earthquakes.
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