Exploring a convection-diffusion-reaction model of the propagation of forest fires: computation of risk maps for heterogeneous environments

Bürger R.; Gavilán, E; Inzunza D.; Mulet, P; Villada L.M.

Keywords: topography, numerical solution, risk map, Forest fire model, convection-diffusion-reaction problem, implicit-explicit time integration, weighted essentially non-oscillatory reconstruction, nonlinear diffusion function

Abstract

The propagation of a forest fire can be described by a convection-diffusion-reaction problem in two space dimensions, where the unknowns are the local temperature and the portion of fuel consumed as functions of spatial position and time. This model can be solved numerically in an efficient way by a linearly implicit-explicit (IMEX) method to discretize the convection and nonlinear diffusion terms combined with a Strang-type operator splitting to handle the reaction term. This method is applied to several variants of the model with variable, nonlinear diffusion functions, where it turns out that increasing diffusivity (with respect to a given base case) significantly enlarges the portion of fuel burnt within a given time while choosing an equivalent constant diffusivity or a degenerate one produces comparable results for that quantity. In addition the effect of spatial heterogeneity as described by a variable topography is studied. The variability of topography influences the local velocity and direction of wind. It is demonstrated how this variability affects the direction and speed of propagation of the wildfire and the location and size of area of fuel consumed. The possibility to solve the base model efficiently is utilized for the computation of so-called risk maps. Here the risk associated with a given position in a sub-area of the computational domain in quantified by the rapidity of consumption of a given amount of fuel by a fire starting in that position. As a result, we obtain that in comparison with the planar case and under the same wind conditions, the model predicts a higher risk for those areas where both the variability of topography (as expressed by the gradient of its height function) and the wind velocity are influential. In general, numerical simulations include that in all cases the risk map with for a non-planar topography includes areas with a reduced risk as well as such with an enhanced risk as compared to the planar case.

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Título de la Revista: Mathematics
Fecha de publicación: 2020