nicaragua earthquake 2004
0000263978 00000 n Large earthquakes, such as the Mw 7.7 1992 Nicaragua earthquake, have occurred off the Pacific coasts of El Salvador and Nicaragua in Central America and have generated distractive tsunamis along these coasts. 0000212473 00000 n 0000193630 00000 n 0000273200 00000 n 0000210789 00000 n 0000218275 00000 n
0000241538 00000 n 0000020849 00000 n 0000304321 00000 n 0000268453 00000 n 0000237091 00000 n
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0000313407 00000 n 0000321120 00000 n 0000268757 00000 n 0000219182 00000 n
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0000318212 00000 n The length, 50 km, and the width, 28 km, of the fault model are calculated from Mw7.2 using the scaling relationship of Blaser et al. 0000281464 00000 n 0000245827 00000 n 0000229197 00000 n 0000237399 00000 n
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0000130969 00000 n 0000037199 00000 n The seismic moment from the GCMT catalog is 3.8 × 10The vertical components of 125 broadband seismic records shown in Fig. 0000261139 00000 n
0000213543 00000 n Borrero, J. C., Kalligeris, N., Lynett, P. J., Fritz, H. M., Newman, A. V., & Convers, J. 0000207140 00000 n
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A large earthquake occurred off El Salvador or Nicaragua on August 27, 2012.
Bilek, L., & Lay, T. (1999). 0000288644 00000 n 0000272431 00000 n
0000197601 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 …
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0000225695 00000 n The El Salvador and Philippines tsunamis of August 2012: insights from sea level data analysis and numerical modeling.
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0000252709 00000 n 0000257760 00000 n 0000262684 00000 n 0000320100 00000 n The northwest-southeast-trending trench marks the boundary where the Cocos plate begins subducting beneath the overriding Caribbean plate at a rate of about 80 mm/yr. 0000022270 00000 n 0000284829 00000 n 0000294173 00000 n 0000274423 00000 n
0000265485 00000 n 0000322612 00000 n 0000215509 00000 n 0000287726 00000 n 0000267688 00000 n 0000295093 00000 n
0000274270 00000 n 0000212013 00000 n
0000274577 00000 n The length, 100 km, and the width, 52 km, of the fault model are calculated from Mw7.7 using the scaling relationship of Blaser et al. 0000212319 00000 n 0000019829 00000 n 0000019363 00000 n 0000195918 00000 n 0000202079 00000 n The method was tested for four large earthquakes, the 1992 Nicaragua tsunami earthquake (Mw7.7), the 2001 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.
0000246286 00000 n 0000253779 00000 n (Because the observed tsunami was less than 0.25 m, the numerical tsunami simulation solving the non-linear shallow water equations without inundation was carried out. 0000244755 00000 n 0000240463 00000 n
0000310708 00000 n
0000238932 00000 n 0000018208 00000 n 0000072427 00000 n 0000260364 00000 n 0000021609 00000 n 0000322368 00000 n 0000262066 00000 n 0000319708 00000 n 0000193175 00000 n 0000271671 00000 n The fault parameters estimated from the W-phase inversion (Kanamori and Rivera However, uncertainties of a scaling relationship and a depth-dependent rigidity should be more carefully examined to use the method for a real tsunami early warning.
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0000249807 00000 n 0000311393 00000 n 0000248120 00000 n We found that the observed tsunami heights, run-up heights, and inundation areas were reasonably well …
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