Author:
Clements Craig B.,Kochanski Adam K.,Seto Daisuke,Davis Braniff,Camacho Christopher,Lareau Neil P.,Contezac Jonathan,Restaino Joseph,Heilman Warren E.,Krueger Steven K.,Butler Bret,Ottmar Roger D.,Vihnanek Robert,Flynn James,Filippi Jean-Baptiste,Barboni Toussaint,Hall Dianne E.,Mandel Jan,Jenkins Mary Ann,O'Brien Joseph,Hornsby Ben,Teske Casey
Abstract
The FireFlux II experiment was conducted in a tall grass prairie located in south-east Texas on 30 January 2013 under a regional burn ban and high fire danger conditions. The goal of the experiment was to better understand micrometeorological aspects of fire spread. The experimental design was guided by the use of a coupled fire–atmosphere model that predicted the fire spread in advance. Preliminary results show that after ignition, a surface pressure perturbation formed and strengthened as the fire front and plume developed, causing an increase in wind velocity at the fire front. The fire-induced winds advected hot combustion gases forward and downwind of the fire front that resulted in acceleration of air through the flame front. Overall, the experiment collected a large set of micrometeorological, air chemistry and fire behaviour data that may provide a comprehensive dataset for evaluating and testing coupled fire–atmosphere model systems.
Cited by
40 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献