2013
DOI: 10.1016/j.proci.2012.07.022
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Assessment of ForeFire/Meso-NH for wildland fire/atmosphere coupled simulation of the FireFlux experiment

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Cited by 68 publications
(62 citation statements)
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“…Recently, the coupling of an empirical forest fire spread model with a mesoscale atmospheric model (ForeFire-MesoNH) has been proposed to simulate, at large scale, the propagation and smoke emissions of wildfires [5,6]. In this kind of model, the fire front is represented as a thick line and the depth of the front is calculated from the fire residence time evaluated using the expression proposed by Anderson [2].…”
Section: Introductionmentioning
confidence: 99%
“…Recently, the coupling of an empirical forest fire spread model with a mesoscale atmospheric model (ForeFire-MesoNH) has been proposed to simulate, at large scale, the propagation and smoke emissions of wildfires [5,6]. In this kind of model, the fire front is represented as a thick line and the depth of the front is calculated from the fire residence time evaluated using the expression proposed by Anderson [2].…”
Section: Introductionmentioning
confidence: 99%
“…Idealized studies have examined fine-scale fire phenomena such as fire whirls [16] and tested sensitivity to fire environment parameters [67]. Some studies attempt to reproduce real prescribed fires [68], often fires conducted during instrumented experiments [19,23,69,70], yet struggle with representing the ambient wind environment [69], which can vary over a small area, and small-scale atmospheric fluctuations [19]. Also, prescribed fires may be ignited with complex ignition patterns and tampered with over time, interfering with the fire's natural evolution.…”
Section: Configuration For Small-scale Firesmentioning
confidence: 99%
“…Due to the high computational cost of flame-scale CFD and due to the lack of knowledge in environmental conditions, the use of CFDbased detailed modeling approaches such as FIRETEC (Linn et al, 2002), WFDS (Mell et al, 2007) or AVBP-PRISSMA-PYROWO (Rochoux, 2014) is currently restricted to research projects and is not compatible with operational applications. On the other hand, regional-scale fire spread models such as FARSITE (Finney, 1998), FOREFIRE (Filippi et al, , 2013, PROMETHEUS (Tymstra et al, 2010) or PHOENIX RapidFire (Chong et al, 2013) use a semiempirical model that treats the ROS as a parametric function of biomass fuel properties, terrain topography and meteorological conditions; for instance, FARSITE uses a semiempirical model due to Rothermel (1972), while FOREFIRE is based on the quasi-physical model due to Balbi et al (2009); a detailed review of ROS models is provided in Sullivan (2009). One recent strategy to better account for time-varying weather conditions at regional scales consists of coupling a front-tracking simulator for surface fires with a meso-scale CFD atmospheric model for fire-induced atmospheric dynamics, see for instance WRF-Fire (Kochanski et al, 2013) or FOREFIRE-MESONH (Filippi et al, 2013).…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, regional-scale fire spread models such as FARSITE (Finney, 1998), FOREFIRE (Filippi et al, , 2013, PROMETHEUS (Tymstra et al, 2010) or PHOENIX RapidFire (Chong et al, 2013) use a semiempirical model that treats the ROS as a parametric function of biomass fuel properties, terrain topography and meteorological conditions; for instance, FARSITE uses a semiempirical model due to Rothermel (1972), while FOREFIRE is based on the quasi-physical model due to Balbi et al (2009); a detailed review of ROS models is provided in Sullivan (2009). One recent strategy to better account for time-varying weather conditions at regional scales consists of coupling a front-tracking simulator for surface fires with a meso-scale CFD atmospheric model for fire-induced atmospheric dynamics, see for instance WRF-Fire (Kochanski et al, 2013) or FOREFIRE-MESONH (Filippi et al, 2013). Still, many uncertainties remain due to simplifications in the description of the physics and to knowledge gaps in the description of environmental conditions and yet, errors in the properties of the biomass fuel or in the flame/wind interactions induce strong changes in the heat transfer from the flame to the vegetation and in the biomass fuel pyrolysis for instance.…”
Section: Introductionmentioning
confidence: 99%