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    Three Types of Horizontal Vortices Observed in Wildland Mass and Crown Fires

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 012::page 1624
    Author:
    Haines, Donald A.
    ,
    Smith, Mahlon C.
    DOI: 10.1175/1520-0450(1987)026<1624:TTOHVO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Observation shows that three types of horizontal vortices may form during intense wildland fires. Two of these vortices are longitudinal relative to the ambient wind and the third is transverse. One of the longitudinal types, a vortex pair, occurs with extreme heat and low to moderate wind speeds. It may be a somewhat common structure on the flanks of intense crown firm when burning is concentrated along the fire's perimeter. The second longitudinal type, a single vortex, occurs with high winds and can dominate the entire fire. The third type, the transverse vortex, occurs on the upstream side of the convection column during intense burning and relatively low winds. These vortices are important because they contribute to fire fighter and are a threat to fire fighter safety. This paper documents field observations of the vortices and supplies supportive meteorological and fuel data. The discussion includes applicable laboratory and conceptual studies in fluid flow and heat transfer that may apply to vortex formation.
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      Three Types of Horizontal Vortices Observed in Wildland Mass and Crown Fires

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146475
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    contributor authorHaines, Donald A.
    contributor authorSmith, Mahlon C.
    date accessioned2017-06-09T14:02:04Z
    date available2017-06-09T14:02:04Z
    date copyright1987/12/01
    date issued1987
    identifier issn0733-3021
    identifier otherams-11266.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146475
    description abstractObservation shows that three types of horizontal vortices may form during intense wildland fires. Two of these vortices are longitudinal relative to the ambient wind and the third is transverse. One of the longitudinal types, a vortex pair, occurs with extreme heat and low to moderate wind speeds. It may be a somewhat common structure on the flanks of intense crown firm when burning is concentrated along the fire's perimeter. The second longitudinal type, a single vortex, occurs with high winds and can dominate the entire fire. The third type, the transverse vortex, occurs on the upstream side of the convection column during intense burning and relatively low winds. These vortices are important because they contribute to fire fighter and are a threat to fire fighter safety. This paper documents field observations of the vortices and supplies supportive meteorological and fuel data. The discussion includes applicable laboratory and conceptual studies in fluid flow and heat transfer that may apply to vortex formation.
    publisherAmerican Meteorological Society
    titleThree Types of Horizontal Vortices Observed in Wildland Mass and Crown Fires
    typeJournal Paper
    journal volume26
    journal issue12
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1987)026<1624:TTOHVO>2.0.CO;2
    journal fristpage1624
    journal lastpage1637
    treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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