Mechanism and future risk of slope instability induced by extreme rainfall event in Izu Oshima Island, Japan

Author:

Towhata IkuoORCID,Goto Satoshi,Goto Shigeru,Akima Takeshi,Tanaka Junya,Uchimura Taro,Wang Gonghui,Yamaguchi Hiroshi,Aoyama Shogo

Funder

MEXT of Japanese Government

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Water Science and Technology

Reference35 articles.

1. Baum RL, Godt W (2010) Early warning of rainfall-induced shallow landslides and debris flows in the USA. Landslides 7(3):259–272

2. Brunetti MT, Peruccacci S, Rossi M, Luciani S, Valigi D, Guzzetti F (2010) Rainfall thresholds for the possible occurrence of landslides in Italy. Nat Haz Earth Syst Sci 10(3):447–458

3. Caine N (1980) The rainfall intensity: duration control of shallow landslides and debris flows. Geografiska annaler: series A, physical geography. Svenska Sallskapet för Antropologi och Geografi (Swedish Soc Anthropol Geogr) 62(1/2):23–27

4. Campbell RH (1975) Soil slips, debris flows, and rainstorms in the Santa Monica mountains and vicinity geological survey professional paper. US Geological Survey Professional Paper, Southern California, p 851

5. Committee for Publication of Oshima's History (2000) General Summary of Oshima History, p.765 (in Japanese).

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