2016
DOI: 10.1007/s11069-016-2285-1
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Tsunami inundation area and run-up height in the Iwate coastal region following the Great East Japan Earthquake as estimated from aerial photographs and digital elevation data

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Cited by 3 publications
(5 citation statements)
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“…Even the numerical simulation is unable to approximate extremely high inundation points of more than 25 m located outside the bay (marked in Figure 7a). These extreme run‐ups were possibly induced by the steep cliff and were also observed at the shorelines along the Sanriku coasts characterized by similar terrain (Yanagawa & Koshino, 2016). Consequently, the performance of the numerical simulation in Otsuchi ( K = 1.144 and κ = 1.257) (Figure 7a) is inferior compared to Rikuzentakata.…”
Section: Resultsmentioning
confidence: 82%
See 1 more Smart Citation
“…Even the numerical simulation is unable to approximate extremely high inundation points of more than 25 m located outside the bay (marked in Figure 7a). These extreme run‐ups were possibly induced by the steep cliff and were also observed at the shorelines along the Sanriku coasts characterized by similar terrain (Yanagawa & Koshino, 2016). Consequently, the performance of the numerical simulation in Otsuchi ( K = 1.144 and κ = 1.257) (Figure 7a) is inferior compared to Rikuzentakata.…”
Section: Resultsmentioning
confidence: 82%
“…terrain (Yanagawa & Koshino, 2016). Consequently, the performance of the numerical simulation in Otsuchi (K ¼ 1.144 and κ ¼ 1.257) ( Figure 7a) is inferior compared to Rikuzentakata.…”
Section: 1029/2020jb019690mentioning
confidence: 96%
“…However, this is not always the case because of the high degree of nonlinearity of inundation flow depths, particularly over complex regions. Higher misfits are apparent near shorelines with complex coastal geometry and steep cliff typically characterizing the southern Sanriku coasts 29 (Fig. 5b ).…”
Section: Resultsmentioning
confidence: 99%
“…The tsunami caused by the GEJE also had significant impacts. In Iwate Prefecture, a maximum run-up height of 39.71 m was directly observed during the 2011 tsunami (Mori et al, 2012), whereas results from geographic information system (GIS) analyses estimated a maximum run-up height of 49.8 ± 0.2 m (Yanagawa et al, 2016). On March 11, 2014, Japan's National Police Agency confirmed 18,517 dead and missing persons within 12 prefectural and city government jurisdictions as a result of the tsunami caused by the GEJE and its aftershocks.…”
Section: Introductionmentioning
confidence: 99%
“…Each of the other areas had significantly higher Hatori destruction ratios. Among them, 15 areas had ratios over 90%, indicating that most or all of the buildings were washed away or completely destroyed (Yanagawa et al, 2014b).…”
Section: Introductionmentioning
confidence: 99%