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Self-Organized Criticality Applied to Natural Hazards

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Abstract

The concept of self-organizedcriticality evolved from studies of three simplecellular-automata models: the sand-pile, slider-block,and forest-fire models. In each case, there is asteady “input” and the “loss” is associated with afractal (power-law) distribution of “avalanches.” Each of the three models can be associated with animportant natural hazard: the sand-pile model withlandslides, the slider-block model with earthquakes,and the forest-fire model with forest fires. We showthat each of the three natural hazards havefrequency-size statistics that are well approximatedby power-law distributions. The model behaviorsuggests that the recurrence interval for a severeevent can be estimated by extrapolating the observedfrequency-size distribution of small and mediumevents. For example, the recurrence interval for amagnitude seven earthquake can be obtained directlyfrom the observed frequency of occurrence of magnitudefour earthquakes. This concept leads to thedefinition of a seismic intensity factor. Both globaland regional maps of this seismic intensity factor aregiven. In addition, the behavior of the modelssuggests that the risk of occurrence of large eventscan be substantially reduced if small events areencouraged. For example, if small forest fires areallowed to burn, the risk of a large forest fire issubstantially reduced.

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Authors and Affiliations

  1. Department of Geological Sciences, Cornell University, Ithaca, NY, 14853-1504, U.S.A.

    Bruce D. Malamud & Donald L. Turcotte

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  1. Bruce D. Malamud
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  2. Donald L. Turcotte
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Malamud, B.D., Turcotte, D.L. Self-Organized Criticality Applied to Natural Hazards. Natural Hazards 20, 93–116 (1999). https://doi.org/10.1023/A:1008014000515

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