0000018208 00000 n 0000311393 00000 n The length, 36 km, and the width, 22 km, of the fault model are calculated from Mw7.0 using the scaling relationship of Blaser et al. 0000244295 00000 n 0000288492 00000 n 0000283298 00000 n 0000259754 00000 n
0000235075 00000 n
0000243376 00000 n 0000203615 00000 n
0000187547 00000 n 0000221452 00000 n 0000209718 00000 n 0000020994 00000 n 0000294631 00000 n 0000210789 00000 n 0000262989 00000 n 0000292788 00000 n 0000272431 00000 n 0000248426 00000 n 0000237091 00000 n 0000254084 00000 n
0000193023 00000 n 0000286506 00000 n 0000239697 00000 n 0000275342 00000 n A bilinear source-scaling model for Heidarzadeh, H., & Satake, K. (2014). 0000222515 00000 n 0000272585 00000 n
0000284369 00000 n 0000220244 00000 n 0000267226 00000 n 0000211400 00000 n The seismic moment from the GCMT catalog is 3.8 × 10The vertical components of 125 broadband seismic records shown in Fig. 0000278866 00000 n 0000284981 00000 n 0000287573 00000 n 0000201005 00000 n 0000296784 00000 n The method was tested for the 1992 Nicaragua tsunami earthquake (Mw7.7), which generated an unusually larger tsunami than that expected from the surface wave magnitude, the 2001 El Salvador earthquake (Mw7.7) occurred in a slab with a normal fault mechanism, the 2004 El Astillero earthquake (Mw7.0) occurred at the plate interface as an underthrust earthquake, and the 2012 El … 0000246898 00000 n 0000227361 00000 n 0000022511 00000 n
0000207448 00000 n 0000210176 00000 n 0000248578 00000 n The tsunami numerical simulations were carried out from the determined fault models.
0000117047 00000 n 0000220697 00000 n 0000237244 00000 n 0000291098 00000 n 0000020721 00000 n 0000157188 00000 n El Salvador earthquake (Mw7.7), the 2004 El Astillero earthquake (Mw7.0), and the 2012 El Salvador–Nicaragua earthquake (Mw7.3), which occurred off El Salvador and Nicaragua in Central America. 0000226299 00000 n 0000192259 00000 n 0000189220 00000 n 0000020103 00000 n 0000250417 00000 n 0000260212 00000 n 0000172601 00000 n The great Sumatra-Andaman earthquake of 26 december 2004 T Lay, H Kanamori, CJ Ammon, M Nettles, SN Ward, RC Aster, SL Beck, ... Science 308 (5725), 1127-1133 , 2005 Satake, K., Bourgeois, J., Abe, K., Abe, K., Tsuji, Y., Imamura, F., Lio, Y., Katao, H., Noguera, E. & Estrada, F. (1993). 0000233551 00000 n 0000261912 00000 n 0000192870 00000 n 0000289871 00000 n 0000296630 00000 n 0000321305 00000 n 492 802 0000016336 00000 n 0000290024 00000 n 0000276261 00000 n 0000282076 00000 n 0000239544 00000 n 0000255313 00000 n 0000306549 00000 n Source characteristic of Nicaraguan tsunami earthquake of September 2, 1993. 0000222667 00000 n 0000320965 00000 n 0000214004 00000 n 0000322368 00000 n
0000190734 00000 n IUGG/IOC time project: Numerical method of tsunami simulation with the leap-flog scheme, IOC of UNESCO, manuals and guides 35.Gusman, A. R., & Tanioka, Y. 0000130918 00000 n 0000272893 00000 n 0000243223 00000 n 0000320625 00000 n 0000018559 00000 n 0000221907 00000 n 0000240157 00000 n 0000279019 00000 n The topography data, Shuttle Radar Topography Mission (SRTM) with a resolution of 3 arcseconds, are used for the tsunami inundation simulation.Tsunami field survey of tsunami run-up heights and inundation area was conducted immediately after the 1992 Nicaragua tsunami earthquake by Abe et al. 0000018892 00000 n 0000258526 00000 n 0000265639 00000 n The scale of devastation in Haiti is far worse than in Asia after the 2004 tsunami, a study says, predicting last month's quake could be the most destructive disaster in modern history. 0000195307 00000 n 0000204379 00000 n 0000022655 00000 n 0000282840 00000 n 0000193630 00000 n 0000205452 00000 n 0000290329 00000 n 0000214465 00000 n 0000314471 00000 n 0000263978 00000 n 0000271057 00000 n 0000037592 00000 n 0000213237 00000 n 0000285893 00000 n 0000268757 00000 n 0000267688 00000 n 0000130969 00000 n 0000208061 00000 n 0000282533 00000 n 0000275190 00000 n The earthquake also triggered a tsunami with further victims and destructions. 0000204686 00000 n 0000223427 00000 n
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