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  1. 防災科研関係論文

Distribution and Characteristics of Slope Movements in the Southern Part of Hiroshima Prefecture Caused by the Heavy Rain in Western Japan in July 2018

https://nied-repo.bosai.go.jp/records/5477
https://nied-repo.bosai.go.jp/records/5477
712c5bfd-119e-4b5a-ba7f-259cec1f8cfd
Item type researchmap(1)
公開日 2023-05-24
タイトル
言語 ja
タイトル Distribution and Characteristics of Slope Movements in the Southern Part of Hiroshima Prefecture Caused by the Heavy Rain in Western Japan in July 2018
タイトル
言語 en
タイトル Distribution and Characteristics of Slope Movements in the Southern Part of Hiroshima Prefecture Caused by the Heavy Rain in Western Japan in July 2018
言語
言語 eng
著者 Hideaki Goto

× Hideaki Goto

ja Hideaki Goto

en Hideaki Goto

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Yasuhiro Kumahara

× Yasuhiro Kumahara

ja Yasuhiro Kumahara

en Yasuhiro Kumahara

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Shoichiro Uchiyama

× Shoichiro Uchiyama

ja Shoichiro Uchiyama

en Shoichiro Uchiyama

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Yoshiya Iwasa

× Yoshiya Iwasa

ja Yoshiya Iwasa

en Yoshiya Iwasa

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Tomoru Yamanaka

× Tomoru Yamanaka

ja Tomoru Yamanaka

en Tomoru Yamanaka

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Rinako Motoyoshi

× Rinako Motoyoshi

ja Rinako Motoyoshi

en Rinako Motoyoshi

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Shun Takeuchi

× Shun Takeuchi

ja Shun Takeuchi

en Shun Takeuchi

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Sho Murata

× Sho Murata

ja Sho Murata

en Sho Murata

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Takashi Nakata

× Takashi Nakata

ja Takashi Nakata

en Takashi Nakata

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抄録
内容記述タイプ Other
内容記述 Record-breaking heavy rainfall in July 2018 caused an extremely large number of slope movements over a broad area of western Japan. We mapped the distribution of slope movements in the southern part of Hiroshima Prefecture through an interpretation of aerial photographs that were acquired after the rainfall by the Geospatial Information Authority of Japan, and counted a total of 8,497 slope-movement starting points. The widespread distribution of slope movements ? from Etajima City of Hiroshima Prefecture to Kasaoka City of Okayama Prefecture ? suggests that the heavy rain affected a very large area. The starting points of debris flow during this disaster were commonly close to the crest of mountain ranges. We compared the distribution of slope movements to the 24-hr rainfall accumulation during the heaviest rainfall event to clarify the factors that caused regional difference in slope-movement distribution. We found the area of highest density of the slope movements was consistent with the area receiving a cumulative rainfall of >250 mm. This observation indicated that the position of slope-movement starting points was not related to differences in geology.
言語 en
書誌情報 ja : Journal of Disaster Research
en : Journal of Disaster Research

巻 14, 号 6, p. 894-902, 発行日 2019-09
出版者
言語 ja
出版者 富士技術出版
出版者
言語 en
出版者 Fuji Technology Press
ISSN
収録物識別子タイプ EISSN
収録物識別子 1883-8030
DOI
関連識別子 10.20965/jdr.2019.p0894
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