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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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