Two Types of Rainfall Conditions Associated with Shallow Landslide Initiation in Japan as Revealed by Normalized Soil Water Index

Author:

Saito Hitoshi12,Nakayama Daichi1,Matsuyama Hiroshi1

Affiliation:

1. Department of Geography, Tokyo Metropolitan University

2. Research Fellow of the Japan Society for the Promotion of Science

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Reference16 articles.

1. Caine, N., 1980: The rainfall intensity-duration control of shallow landslides and debris flows. Geografiska Annaler. Series A. Physical Geography, 62, 23-27.

2. Furukawa, K., M. Kaibori, T. Kubota, T. Jitousono, Y. Gonda, S. Sugihara, S. Hayashi, A. Ikeda, Y. Araki, and Y. Kashiwabara, 2009: Debris disasters caused by heavy rainfall around Hofu City in Yamaguchi Prefecture on July 21, 2009. Journal of Japan Erosion Control Society (Shin-Sabo), 62, 62-73, (in Japanese with English abstract).

3. Guzzetti, F., S. Peruccacci, M. Rossi, and C. Stark, 2008: The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides, 5, 3-17.

4. IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, 996 pp.

5. JMA, 2010: Soil Water Index (in Japanese). Available at http://www.jma.go.jp/jma/kishou/know/bosai/dojoshisu.html, (accessed 2010.3.10).

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