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The average depth of the coseismic landslides was 1.5?m, which is deeper than the depth of the rainfall-induced landslides prior to these. The total sediment production of the coseismic landslides reached 2.5 × 104?m3/km2, which is of the same order as the sediment production triggered by the previous single heavy rainfall event. This result indicates that the effects of the 2016 Kumamoto earthquake in terms of sediment production and topographic changes were similar to those of the rainfall-induced landslide event in the study area. 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  1. 防災科研関係論文

Landslides triggered by an earthquake and heavy rainfalls at Aso volcano, Japan, detected by UAS and SfM-MVS photogrammetry

https://nied-repo.bosai.go.jp/records/6167
https://nied-repo.bosai.go.jp/records/6167
e19231a7-ea1b-4beb-a284-ee4db3bb3693
Item type researchmap(1)
公開日 2023-05-24
タイトル
言語 ja
タイトル Landslides triggered by an earthquake and heavy rainfalls at Aso volcano, Japan, detected by UAS and SfM-MVS photogrammetry
タイトル
言語 en
タイトル Landslides triggered by an earthquake and heavy rainfalls at Aso volcano, Japan, detected by UAS and SfM-MVS photogrammetry
言語
言語 eng
著者 Saito Hitoshi

× Saito Hitoshi

ja Saito Hitoshi

en Saito Hitoshi

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Uchiyama Shoichiro

× Uchiyama Shoichiro

ja Uchiyama Shoichiro

en Uchiyama Shoichiro

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Hayakawa Yuichi S

× Hayakawa Yuichi S

ja Hayakawa Yuichi S

en Hayakawa Yuichi S

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Obanawa Hiroyuki

× Obanawa Hiroyuki

ja Obanawa Hiroyuki

en Obanawa Hiroyuki

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抄録
内容記述タイプ Other
内容記述 Unmanned aerial systems (UASs) and structure-from-motion multi-view stereo (SfM-MVS) photogrammetry have attracted a tremendous amount of interest for use in the creation of high-definition topographic data for geoscientific studies. By using these techniques, this study examined the topographic characteristics of coseismic landslides triggered by the 2016 Kumamoto earthquake (Mw 7.1) in the Sensuikyo area (1.0?km2) at Aso volcano, Japan. The study area has frequently experienced rainfall-induced landslide events, such as those in 1990, 2001, and 2012. We obtained orthorectified images and digital surface models (DSMs) with a spatial resolution of 0.06?m before and after the 2016 Kumamoto earthquake. By using these high-definition images and DSMs, we detected a total of 54 coseismic landslides with volumes of 9.1?3994.6?m3. These landslides, many of which initiated near topographic ridges, were typically located on upside hillslopes of previous rainfall-induced landslide scars that formed in 2012. This result suggests that the topographic effect on seismic waves, i.e., amplification of ground acceleration, was important for coseismic landslide initiation in the study area. The average depth of the coseismic landslides was 1.5?m, which is deeper than the depth of the rainfall-induced landslides prior to these. The total sediment production of the coseismic landslides reached 2.5 × 104?m3/km2, which is of the same order as the sediment production triggered by the previous single heavy rainfall event. This result indicates that the effects of the 2016 Kumamoto earthquake in terms of sediment production and topographic changes were similar to those of the rainfall-induced landslide event in the study area. [Figure not available: see fulltext.].
言語 en
書誌情報 ja : PROGRESS IN EARTH AND PLANETARY SCIENCE
en : PROGRESS IN EARTH AND PLANETARY SCIENCE

巻 5, 号 1, 発行日 2018-03
出版者
言語 en
出版者 Springer Berlin Heidelberg
ISSN
収録物識別子タイプ ISSN
収録物識別子 2197-4284
DOI
関連識別子 10.1186/s40645-018-0169-6
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