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• W2896048901 abstract "Abstract. The propagation of a seismic rupture on a fault introduces spatial variations in the seismic wave field surrounding the fault. This directivity effect results in larger shaking amplitudes in the rupture propagation direction. Its seismic radiation pattern also causes amplitude variations between the strike-normal and strike-parallel components of horizontal ground motion. We investigated the landslide response to these effects during the 2016 Kumamoto earthquake (Mw 7.1) in central Kyushu (Japan). Although the distribution of some 1500 earthquake-triggered landslides as a function of rupture distance is consistent with the observed Arias intensity, the landslides were more concentrated to the northeast of the southwest–northeast striking rupture. We examined several landslide susceptibility factors: hillslope inclination, the median amplification factor (MAF) of ground shaking, lithology, land cover, and topographic wetness. None of these factors sufficiently explains the landslide distribution or orientation (aspect), although the landslide head scarps have an elevated hillslope inclination and MAF. We propose a new physics-based ground-motion model (GMM) that accounts for the seismic rupture effects, and we demonstrate that the low-frequency seismic radiation pattern is consistent with the overall landslide distribution. Its spatial pattern is influenced by the rupture directivity effect, whereas landslide aspect is influenced by amplitude variations between the fault-normal and fault-parallel motion at frequencies <2 Hz. This azimuth dependence implies that comparable landslide concentrations can occur at different distances from the rupture. This quantitative link between the prevalent landslide aspect and the low-frequency seismic radiation pattern can improve coseismic landslide hazard assessment." @default.
• W2896048901 created "2018-10-26" @default.
• W2896048901 creator A5013654589 @default.
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• W2896048901 creator A5055696814 @default.
• W2896048901 creator A5059047863 @default.
• W2896048901 date "2019-04-04" @default.
• W2896048901 modified "2023-10-18" @default.
• W2896048901 title "Effects of finite source rupture on landslide triggering: the 2016 &lt;i&gt;M&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt; 7.1 Kumamoto earthquake" @default.
• W2896048901 cites W1512208174 @default.
• W2896048901 cites W1522948060 @default.
• W2896048901 cites W1585992146 @default.
• W2896048901 cites W1912141177 @default.
• W2896048901 cites W1934929475 @default.
• W2896048901 cites W1965270678 @default.
• W2896048901 cites W1969891935 @default.
• W2896048901 cites W1976025756 @default.
• W2896048901 cites W1978338336 @default.
• W2896048901 cites W1979973772 @default.
• W2896048901 cites W1983513512 @default.
• W2896048901 cites W1984223470 @default.
• W2896048901 cites W1985587747 @default.
• W2896048901 cites W1986564501 @default.
• W2896048901 cites W1994553199 @default.
• W2896048901 cites W1995757108 @default.
• W2896048901 cites W1996226159 @default.
• W2896048901 cites W2012103907 @default.
• W2896048901 cites W2013693488 @default.
• W2896048901 cites W2014074025 @default.
• W2896048901 cites W2018293217 @default.
• W2896048901 cites W2020299698 @default.
• W2896048901 cites W2025977027 @default.
• W2896048901 cites W2026360200 @default.
• W2896048901 cites W2027821730 @default.
• W2896048901 cites W2031950708 @default.
• W2896048901 cites W2060382151 @default.
• W2896048901 cites W2080851666 @default.
• W2896048901 cites W2083654887 @default.
• W2896048901 cites W2086215816 @default.
• W2896048901 cites W2086374678 @default.
• W2896048901 cites W2098769624 @default.
• W2896048901 cites W2103146914 @default.
• W2896048901 cites W2105658614 @default.
• W2896048901 cites W2106347413 @default.
• W2896048901 cites W2106776864 @default.
• W2896048901 cites W2109777032 @default.
• W2896048901 cites W2115400997 @default.
• W2896048901 cites W2118345599 @default.
• W2896048901 cites W2123449025 @default.
• W2896048901 cites W2127548879 @default.
• W2896048901 cites W2132487037 @default.
• W2896048901 cites W2135250349 @default.
• W2896048901 cites W2139348131 @default.
• W2896048901 cites W2147663465 @default.
• W2896048901 cites W2149477794 @default.
• W2896048901 cites W2151004954 @default.
• W2896048901 cites W2152093129 @default.
• W2896048901 cites W2153653017 @default.
• W2896048901 cites W2153978805 @default.
• W2896048901 cites W2155625979 @default.
• W2896048901 cites W2166095666 @default.
• W2896048901 cites W2168175751 @default.
• W2896048901 cites W2169045488 @default.
• W2896048901 cites W2169313493 @default.
• W2896048901 cites W2218734670 @default.
• W2896048901 cites W2258577332 @default.
• W2896048901 cites W2278590165 @default.
• W2896048901 cites W2298299893 @default.
• W2896048901 cites W2302086903 @default.
• W2896048901 cites W2317992515 @default.
• W2896048901 cites W2324392039 @default.
• W2896048901 cites W2377820877 @default.
• W2896048901 cites W2472399859 @default.
• W2896048901 cites W2510732674 @default.
• W2896048901 cites W2518588474 @default.
• W2896048901 cites W2529697663 @default.
• W2896048901 cites W2555896059 @default.
• W2896048901 cites W2561683595 @default.
• W2896048901 cites W2588013725 @default.
• W2896048901 cites W2588237346 @default.
• W2896048901 cites W2606671181 @default.
• W2896048901 cites W2611738800 @default.
• W2896048901 cites W2624917962 @default.
• W2896048901 cites W2693190132 @default.
• W2896048901 cites W2788032251 @default.
• W2896048901 cites W2794741889 @default.
• W2896048901 cites W2795101470 @default.
• W2896048901 cites W2803230334 @default.
• W2896048901 cites W2889908037 @default.
• W2896048901 cites W2891781873 @default.
• W2896048901 cites W3109355539 @default.
• W2896048901 cites W4245948025 @default.
• W2896048901 cites W976344994 @default.
• W2896048901 doi "https://doi.org/10.5194/se-10-463-2019" @default.
• W2896048901 hasPublicationYear "2019" @default.
• W2896048901 type Work @default.
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