Thursday 21 November 2024


Threshold typeThreshold codeDescription
IEI-ERainfall intensity (I) - Cumulative event rainfall (E): IE



Thresholds sorted by Continent

ContinentNationZoneThreshold typeLandslide codeEquationRangeNotesReferenceImage
AsiaJapann.a.IEDI = 112.25 - 0.20×E165 < E < 440n.a.Jibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
AsiaJapann.a.IEDI = 67.38 × E-0.0023×E50 < E < 400n.a.Jibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
AsiaJapanShikoku IslandIEAI = 1000 × E-1.23100 < E < 230n.a.Hong Y, Hiura H, Shino K, Sassa K, Suemine A, Fukuoka H Wang G (2005) The influence of intense rainfall on the activity of large-scale crystalline schist landslides in Shikoku Island, Japan. Landslides 2(2): 97-105Graphic
North AmericaUSAn.a.IEDI = 31.99 - 0.10×E0 < E < 315n.a.Jibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
South AmericaBrazilSerra do Mar, Cubatao, Sao PaoloIESl, EI = 2603 × E96h-0.9330 < E96h < 500Human induced failuresTatizana C, Ogura M, Rocha M, Cerri LES (1987) Analise de correlacao entre chuvas e escorregamentos, Serra do Mar, Municipio de Cubatao. Proceedings 5th Congress Brasiler, Geol Eng San Paolo: 225–236Graphic




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