TXT-tool 4.039-1.1: Definition and Use of Empirical Rainfall Thresholds for Possible Landslide Occurrence

Chapter

Abstract

In Italy, landslides are frequent and widespread phenomena triggered chiefly by intense or prolonged rainfall. Individual rainfall events can result in single or multiple slope failures in small areas or in very large regions, causing fatalities and large economic damage. Thus, assessing the rainfall conditions responsible for landslides is important and may contribute to reducing risk. Following a review of methods for establishing the dependence of landslide occurrence on rainfall. Next, we present the statistical method used for the definition of objective cumulated event rainfall-duration (ED) thresholds, and we show regional, lithological and seasonal thresholds in central Italy.

Keywords

Rainfall threshold Shallow landslide Central Italy 

References

  1. Aleotti P (2004) A warning system for rainfall-induced shallow failures. Eng Geol 73:247–265CrossRefGoogle Scholar
  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 Hazards Earth Syst Sci 10:447–458CrossRefGoogle Scholar
  3. Brunetti MT, Peruccacci S, Antronico L, Bartolini D, Deganutti AM, Gariano SL, Iovine G, Luciani S, Luino F, Melillo M, Palladino MR, Parise M, Rossi M, Turconi L, Vennari C, Vessia G, Viero A, Guzzetti F (2015) Catalogue of rainfall events with shallow landslides and new rainfall thresholds in Italy. In: Lollino G et al (eds) Engineering geology for society and territory, vol 2: landslide processes. Springer, Berlin, pp 1575–1579CrossRefGoogle Scholar
  4. Caine N (1980) The rainfall intensity-duration control of shallow landslides and debris flows. Geogr Ann A 62:23–27Google Scholar
  5. Campbell RH (1975) Soil slips, debris flows, and rainstorms in the Santa Monica Mountains and vicinity, southern California. In: US Geological Survey Professional Paper 851. U.S. Government Printing Office, WashingtonGoogle Scholar
  6. Cancelli A, Nova R (1985) Landslides in soil debris cover triggered by rainstorms in Valtellina (central Alps—Italy). In: Proceedings of the 4th international conference and field workshop on landslides. The Japan Geological Society, Tokyo, pp 267–272Google Scholar
  7. Chang K, Chiang SH, Lei F (2007) Analysing the relationship between typhoon-triggered landslides and critical rainfall conditions. Earth Surf Process Landf 33(8):1261–1271CrossRefGoogle Scholar
  8. Chiang SH, Chang K (2008) Application of radar data to modelling rainfall-induced landslides. Geomorphology 103(3):299–309CrossRefGoogle Scholar
  9. Chleborad AF (2003) Preliminary evaluation of a precipitation threshold for anticipating the occurrence of landslides in the Seattle, Washington, Area. US Geological Survey Open-File Report 03-463Google Scholar
  10. Corominas J, Moya J (1999) Reconstructing recent landslide activity in relation to rainfall in the Llobregat River Basin, Eastern Pyrenees, Spain. Geomorphology 30:79–93CrossRefGoogle Scholar
  11. Crozier MJ (1999) Prediction of rainfall-triggered landslides: a test of the antecedent water status model. Earth Surf Proc Land 24:825–833CrossRefGoogle Scholar
  12. Crosta GB, Frattini P (2003) Distributed modelling of shallow landslides triggered by intense rainfall. Nat Hazards Earth Syst Sci 3(1–2):81–93CrossRefGoogle Scholar
  13. Glade T, Crozier MJ, Smith P (2000) Applying probability determination to refine landslide-triggering rainfall thresholds using an empirical ‘‘Antecedent Daily Rainfall Model’’. Pure Appl Geophys 157(6/8):1059–1107CrossRefGoogle Scholar
  14. Guzzetti F, Peruccacci S, Rossi M, Stark CP (2007) Rainfall thresholds for the initiation of landslides in Central and Southern Europe. Meteorol Atmos Phys 98:239–267CrossRefGoogle Scholar
  15. Guzzetti F, Peruccacci S, Rossi M, Stark CP (2008) The rainfall intensity-duration control of shallow landslides and debris flows: an update. Landslides 5(1):3–17CrossRefGoogle Scholar
  16. Innes JL (1983) Debris flows. Prog Phys Geogr 7:469–501CrossRefGoogle Scholar
  17. Iverson RM (2000) Landslide triggering by rain infiltration. Water Resour Res 36(7):1897–1910CrossRefGoogle Scholar
  18. Jakob M, Weatherly H (2003) A hydroclimatic threshold for landslide initiation on the North Shore Mountains of Vancouver, British Columbia. Geomorphology 54:137–156CrossRefGoogle Scholar
  19. Montgomery DR, Dietrich WE (1994) A physically based model for the topographic control of shallow landsliding. Water Resour Res 30(4):1153–1171CrossRefGoogle Scholar
  20. Peruccacci S, Brunetti MT, Luciani S, Vennari C, Guzzetti F (2012) Lithological and seasonal control of rainfall thresholds for the possible initiation of landslides in central Italy. Geomorphology 139–140:79–90CrossRefGoogle Scholar
  21. Reichenbach P, Cardinali M, De Vita P, Guzzetti F (1998) Regional hydrological thresholds for landslides and floods in the Tiber River Basin (Central Italy). Environ Geol 35(2–3):146–159CrossRefGoogle Scholar
  22. Terlien MTJ (1998) The determination of statistical and deterministic hydrological landslide-triggering thresholds. Environ Geol 35(2–3):124–130CrossRefGoogle Scholar
  23. White ID, Mottershead DN, Harrison JJ (1996) Environmental systems, 2nd edn. Chapman & Hall, London, p 616CrossRefGoogle Scholar
  24. Wieczorek GF (1996) Landslide triggering mechanisms. In: Turner AK, Schuster RL (eds) Landslides: investigation and mitigation. Transportation Research Board, National Research Council, Special Report, Washington, pp 76–90Google Scholar
  25. Wieczorek GF, Glade T (2005) Climatic factors influencing occurrence of debris flows. In: Jakob M, Hungr O (eds) Debris flow hazards and related phenomena. Springer, Berlin, pp 325–362CrossRefGoogle Scholar
  26. Wilson RC (1989) Rainstorms, pore pressures, and debris flows: a theoretical framework. In: Morton DM, Sadler PM (eds) Landslides in a semi-arid environment, vol 2. Publications of the Inland Geological Society, California, pp 101–111Google Scholar
  27. Wilson RC, Wieczorek GF (1995) Rainfall thresholds for the initiation of debris flow at La Honda, California. Environ Eng Geosci 1(1):11–12CrossRefGoogle Scholar
  28. Wu W, Sidle RC (1995) A distributed slope stability model for steep forested basins. Water Resour Res 31:2097–2110CrossRefGoogle Scholar

Copyright information

© Springer International Publishing AG 2018

Authors and Affiliations

  1. 1.Istituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle RicercheCNR IRPIPerugiaItaly

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