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Coupled atmosphere-wildland fire modeling with WRF-Fire

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TLDR
In this paper, the authors describe the physical model, numerical algorithms, and software structure of a fire spread model, implemented by the level-set method, coupled with the Weather Research and Forecasting model.
Abstract
We describe the physical model, numerical algorithms, and software structure of WRF-Fire. WRF-Fire consists of a fire-spread model, implemented by the level-set method, coupled with the Weather Research and Forecasting model. In every time step, the fire model inputs the surface wind, which drives the fire, and outputs the heat flux from the fire into the atmosphere, which in turn influences the atmosphere. The level-set method allows submesh representation of the burning region and flexible implementation of various ignition modes. WRF-Fire is distributed as a part of WRF and it uses the WRF parallel infrastructure for parallel computing.

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Journal ArticleDOI

WRF-Fire: Coupled Weather–Wildland Fire Modeling with the Weather Research and Forecasting Model

TL;DR: In this paper, a wildland fire-behavior module, named WRF-fire, was integrated into the Weather Research and Forecasting (WRF) public domain numerical weather prediction model.
Journal ArticleDOI

Overview of the Meso-NH model version 5.4 and its applications

TL;DR: The Meso-NH model as discussed by the authors is an atmospheric non hydrostatic research model that is applied to a broad range of resolutions, from synoptic to turbulent scales, and is designed for studies of physics and chemistry.
Journal ArticleDOI

Simulation of wind-induced snow transport and sublimation in alpine terrain using a fully coupled snowpack/atmosphere model

TL;DR: In this article, a new numerical model is developed to gain understanding on the complex processes that drive the redistribution of snow, which directly cou- ples the detailed snowpack model Crocus with the atmo-spheric model Meso-NH.
Journal ArticleDOI

Towards predictive data-driven simulations of wildfire spread - Part I: Reduced-cost ensemble Kalman filter based on a polynomial chaos surrogate model for parameter estimation.

TL;DR: A wildfire spread simulator combined with an ensemble-based DA algorithm is therefore a promising approach to reduce uncertainties in the forecast position of the fire front and to introduce a paradigm-shift in the wildfire emergency response.
Journal ArticleDOI

Wildland fire emissions, carbon and climate: Characterizing wildland fuels

TL;DR: In this paper, the type, amount, characteristics, and condition of wildland fuels affect combustion and emissions during wildland and prescribed fires, and a fundamental understanding of the relationships between fuel characteristics, fuel conditions, fire occurrence, combustion dynamics, and GHG/A/BC emissions is needed to aid strategy development to mitigate the expected effects of climate change.
References
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Book

Level Set Methods and Dynamic Implicit Surfaces

TL;DR: A student or researcher working in mathematics, computer graphics, science, or engineering interested in any dynamic moving front, which might change its topology or develop singularities, will find this book interesting and useful.
Book

Atmospheric Modeling, Data Assimilation and Predictability

TL;DR: A comprehensive text and reference work on numerical weather prediction, first published in 2002, covers not only methods for numerical modeling, but also the important related areas of data assimilation and predictability.
Book

Standard Fire Behavior Fuel Models: A Comprehensive Set for Use with Rothermel?s Surface Fire Spread Model

TL;DR: In this paper, a new set of standard fire behavior fuel models for use with Rothermel's surface fire spread model and the relationship of the new set to the original set of 13 fire behaviour fuel models is described.
Journal ArticleDOI

Description of a coupled atmosphere–fire model

TL;DR: In this paper, a coupled fire-atmosphere model that uses a sophisticated high-resolution non- hydrostatic numerical mesoscale model to predict the local winds which are then used as input to the prediction of fire spread is presented.
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