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Modelling Fast-moving Flow-like Landslides by Cellular Automata: Simulations of Debris Flows and Lahars

机译:通过蜂窝自动机建模快速移动的流量滑坡:碎片流动和拉哈尔的模拟

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Cellular Automata (CA) represent a computational paradigm for complex fluid-dynamical phenomena that evolve on the basis on local interactions. Macroscopic CA (MCA) characterize a methodological approach for modelling and simulating large scale (extended for kilometers) surface flows. Fast-moving flow-like "landslides", as lahars, debris and mud flows, represent very destructive natural disasters as number of casualties in the world. Simulation of such phenomena could be an important tool for hazard management in threatened regions. This paper presents shortly the modelling methodology of MCA for such type of surface flow together with the models SCIDDICA-SS2, SCIDDICA-SS3 (both for debris, mud and granular flows) and LLUNPIY (for primary and secondary lahars) together with their significant applications in simulating both past and probable future events. At the end, a new result about possible hazard of Cotopaxi volcano is reported; the repetition of the 1877 catastrophic lahar invasion is simulated, beginning from the immediate melting of part of the Cotopaxi icecap because of volcanic activity.
机译:蜂窝自动机(CA)代表复杂流体动态现象的计算范例,即在局部相互作用的基础上发展。宏观CA(MCA)表征了一种用于建模和模拟大规模的方法方法(延长公里)表面流动。作为拉哈尔斯,碎片和泥浆流动的快速流动的流动“山体滑坡”代表了世界上伤亡人数的非常破坏性的自然灾害。这种现象的模拟可能是威胁区域危害管理的重要工具。本文不久呈现了这种类型的表面流动的MCA的建模方法,与SCIDDICA-SS2,SCIDDICA-SS3(用于碎片,泥浆和粒状流量)和Llunpiy(用于次级和次级拉哈尔)的模型一起流动在模拟过去和可能的未来事件中。最后,报告了关于Cotopaxi火山可能危害的新结果;由于火山激活,从一部分Cotopaxi ICECAP的立即熔化开始,模拟了1877年灾难性拉哈尔侵入的重复。

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