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    Infrared Imagery of Crown-Fire Dynamics during FROSTFIRE

    Source: Journal of Applied Meteorology:;2004:;volume( 043 ):;issue: 009::page 1241
    Author:
    Coen, Janice
    ,
    Mahalingam, Shankar
    ,
    Daily, John
    DOI: 10.1175/1520-0450(2004)043<1241:IIOCDD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A thorough understanding of crown-fire dynamics requires a clear picture of the three-dimensional winds in and near the fire, including the flaming combustion zone and the convective updrafts produced by the fire. These observations and analyses present a unique high-spatial-resolution and high-temporal-resolution perspective of the motions within crown fires propagating up a forested 20° slope under light winds of 3 m s?1 during the FROSTFIRE experiment in interior Alaska. The purpose of this work is to calculate combustion-zone winds and examine mechanisms for the rapid propagation of crown fires. An infrared imager was used to detect high-temperature regions produced by incandescent soot particles in and near the fire and to produce a sequence of high-frequency (60 Hz), high-resolution (0.375 m ? 0.8 m) two-dimensional images of temperature. An image-flow-analysis technique was applied to these data to derive wind fields in the image plane. Maximum updrafts of 32?60 m s?1 accompany maximum downdrafts of 18?30 m s?1. Horizontal wind speeds of 12?28 m s?1 show strong inflow into the base of the convective updrafts and imply recirculation of air and incomplete combustion products from the fire. Motions were more complex than a single large convective plume or many buoyant tree-scale plumes rising separately. Instead, repeated examples of narrow flaming fingers, representing a scale larger than individual trees, initially burst upslope along the ground for tens of meters at speeds up to 28?48 m s?1 before turning upward. These bursts exceeded ambient environmental winds, those considered to be driving the fire, by a factor of 10 and were low enough to propagate the crown fire actively by both igniting and preheating/ drying canopy fuel ahead of the fire. Average spread rates were 0.75?1.11 m s?1, with a peak 10-s spread rate of 1.26 m s?1. This powerful, dynamic mechanism of fire spread could explain firefighter reports of being overtaken by ?fireballs.?
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      Infrared Imagery of Crown-Fire Dynamics during FROSTFIRE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148847
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    contributor authorCoen, Janice
    contributor authorMahalingam, Shankar
    contributor authorDaily, John
    date accessioned2017-06-09T14:09:15Z
    date available2017-06-09T14:09:15Z
    date copyright2004/09/01
    date issued2004
    identifier issn0894-8763
    identifier otherams-13400.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148847
    description abstractA thorough understanding of crown-fire dynamics requires a clear picture of the three-dimensional winds in and near the fire, including the flaming combustion zone and the convective updrafts produced by the fire. These observations and analyses present a unique high-spatial-resolution and high-temporal-resolution perspective of the motions within crown fires propagating up a forested 20° slope under light winds of 3 m s?1 during the FROSTFIRE experiment in interior Alaska. The purpose of this work is to calculate combustion-zone winds and examine mechanisms for the rapid propagation of crown fires. An infrared imager was used to detect high-temperature regions produced by incandescent soot particles in and near the fire and to produce a sequence of high-frequency (60 Hz), high-resolution (0.375 m ? 0.8 m) two-dimensional images of temperature. An image-flow-analysis technique was applied to these data to derive wind fields in the image plane. Maximum updrafts of 32?60 m s?1 accompany maximum downdrafts of 18?30 m s?1. Horizontal wind speeds of 12?28 m s?1 show strong inflow into the base of the convective updrafts and imply recirculation of air and incomplete combustion products from the fire. Motions were more complex than a single large convective plume or many buoyant tree-scale plumes rising separately. Instead, repeated examples of narrow flaming fingers, representing a scale larger than individual trees, initially burst upslope along the ground for tens of meters at speeds up to 28?48 m s?1 before turning upward. These bursts exceeded ambient environmental winds, those considered to be driving the fire, by a factor of 10 and were low enough to propagate the crown fire actively by both igniting and preheating/ drying canopy fuel ahead of the fire. Average spread rates were 0.75?1.11 m s?1, with a peak 10-s spread rate of 1.26 m s?1. This powerful, dynamic mechanism of fire spread could explain firefighter reports of being overtaken by ?fireballs.?
    publisherAmerican Meteorological Society
    titleInfrared Imagery of Crown-Fire Dynamics during FROSTFIRE
    typeJournal Paper
    journal volume43
    journal issue9
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2004)043<1241:IIOCDD>2.0.CO;2
    journal fristpage1241
    journal lastpage1259
    treeJournal of Applied Meteorology:;2004:;volume( 043 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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