Sunday 05 May 2024




Rainfall thresholds in Worldwide, sorted by Nation

NationZoneThreshold typeLandslide codeEquationRangeNotesReferenceImage
n.a.n.a.EDDE = 4.93 × D0.5040.1 < D < 100n.a.Innes JL (1983) Debris flows. Progress in Physical Geography 7: 469-501Graphic
n.a.n.a.EDAE = 14.82 × D0.610.167 < D < 500n.a.Caine N (1980) The rainfall intensity-duration control of shallow landslides and debris flows. Geografiska Annaler Series A-Physical Geography 62: 23-27Graphic
n.a.n.a.IDDI = 7.00×D-0.600.1 < D < 3For burnt areasCannon SH, Gartner JE (2005) Wildfire-related debris flow from a hazards perspective. In: Debris flow Hazards and Related Phenomena (Jakob M, Hungr O, eds). Springer Berlin Heidelberg, 363-385Graphic
n.a.n.a.IDSI = 10×D-0.770.1 < D < 1000n.a.Clarizia M, Gullà G, Sorbino G (1996) Sui meccanismi di innesco dei soil slip. International Conference "Prevention of hydrogeological hazards: the role of scientific research" 1: 585-597Graphic
n.a.n.a.IDShI=0.48+7.2×D-1.000.1 < D < 1000n.a.Crosta GB, Frattini P (2001) Rainfall thresholds for triggering soil slips and debris flow. In: Mediterranean Storms (Mugnai A, Guzzetti F, Roth G, eds), Proceedings of the 2nd EGS Plinius Conference on Mediterranean Storms. Siena, Italy, 463-487Graphic
n.a.n.a.IDSh, DI = 4.81×D-0.490.1 < D < 1000Mediterranean warm climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 5.35×D-0.440.1 < D < 48Mediterranean warm climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 3.57×D-0.410.1 < D < 1000Mediterranean cool climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 3.55×D-0.400.1 < D < 48Mediterranean cool climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 6.68×D-0.520.1 < D < 1000Warm humid subtropical climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 6.25×D-0.110.1 < D < 48Warm humid subtropical climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 8.70×D-0.660.1 < D < 1000Mountain climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 8.31×D-0.640.1 < D < 48Mountain climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDDI = 30.53 ×D-0.570.5 < D < 12Lower envelopeJibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
n.a.n.a.IDAI = 14.82×D-0.390.167 < D < 500n.a.Caine N (1980) The rainfall intensity-duration control of shallow landslides and debris flows. Geografiska Annaler Series A-Physical Geography 62: 23–27Graphic
n.a.n.a.IDSh, DI = 2.20×D-0.440.1 < D < 1000Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 2.28×D-0.200.1 < D < 48(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 0.48×D-0.1148 < D < 1000(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 6.90×D-0.580.1 < D < 1000Humid subtropical east coast climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 10.30×D-0.350.1 < D < 48Humid subtropical east coast climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 16.43×D-0.980.1 < D < 1000Mild marine west coast climatesGuzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IDSh, DI = 22.26×D-0.900.1 < D < 48Mild marine west coast climates (Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IMAPDDIMAP = 0.02×D-0.650.5 < D < 12Lower envelopeJibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
n.a.n.a.IMAPDSh, DIMAP = 0.0017×D-0.130.1 < D < 48(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IMAPDSh, DIMAP = 0.0005×D-0.1348 < D < 1000(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IMAPDSh, DIMAP = 0.0016×D-0.400.1 < D < 1000n.a.Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IMAPEMAPDIMAP = 0.003 × EMAP-0.740.03 < EMAP < 0.4Lower envelopeJibson RW (1989) Debris flow in southern Porto Rico. Geological Society of America, Special Paper 236, 29–55Graphic
n.a.n.a.IRDNDSh, DIRDN = 0.25×D-0.390.1 < D < 1000n.a.Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IRDNDSh, DIRDN = 0.27×D-0.140.1 < D < 48(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic
n.a.n.a.IRDNDSh, DIRDN = 0.06×D-0.1248 < D < 1000(Threshold obtained from probability estimates of rainfall data)Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5: 3-17Graphic




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