2020
DOI: 10.3390/w12071997
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Efficient Urban Inundation Model for Live Flood Forecasting with Cellular Automata and Motion Cost Fields

Abstract: The mitigation of societal damage from urban floods requires fast hydraulic models for emergency and planning purposes. The simplified mathematical model Cellular Automata is combined with Motion Cost fields, which score the difficulty to traverse an area, to the urban inundation model CAMC. It is implemented with simple matrix and logic operations to achieve high computational efficiency. The development concentrated on an application in dense urban built-up areas with numerous buildings. CAMC is efficient an… Show more

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Cited by 8 publications
(4 citation statements)
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“…The motion cost can include soil characteristics, such as roughness and infiltration potential. The weights for water distribution are a function of the motion cost at the central and neighbor cells [ 62 ], which, in the simplest case, is proportional to the normalized gradients. The simulation stops when all the surplus water has reached the coast.…”
Section: Methodsmentioning
confidence: 99%
“…The motion cost can include soil characteristics, such as roughness and infiltration potential. The weights for water distribution are a function of the motion cost at the central and neighbor cells [ 62 ], which, in the simplest case, is proportional to the normalized gradients. The simulation stops when all the surplus water has reached the coast.…”
Section: Methodsmentioning
confidence: 99%
“…In the application of flood simulation, numerous models have been developed based on different rules. Examples include the ranking system [11] , minimization [ 23 , 34 ], weighted parameters [12] , and the motion cost file [16] . The DBM method swiftly generates a maximum inundation map using a mass conservation and topographical data.…”
Section: Background Motivationmentioning
confidence: 99%
“…Most RFIMs route the surface flow to derive flood inundation information, taking advantage of the greater availability of high-resolution topographic data and high-performance computing resources [34]. The surface flow can be routed by the simplified forms of 2D shallow water equation, including diffusive wave [35][36][37][38], kinematic wave [39,40] and inertial wave [41][42][43], and also by the Cellular Automata approaches [44][45][46][47]. In these models, surface flow is typically routed on a regular cell basis, but the computational efficiency is still a challenge for large areas represented by high-resolution topographic data.…”
Section: Introductionmentioning
confidence: 99%