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contributor authorRotunno, Richard
date accessioned2017-06-09T14:20:35Z
date available2017-06-09T14:20:35Z
date copyright1979/01/01
date issued1979
identifier issn0022-4928
identifier otherams-17633.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153549
description abstractFine-resolution calculations using an axisymmetric numerical model of the flow within a Ward-type vortex chamber are discussed. Particular attention is paid to the vortex-ground interaction. Variations in the swirl ratio S from zero to unity lead to radically different vortex structure in the ?corner? region (i.e., near r = z = 0). For S Lt; 1, a concentrated vortex forms in the upper chamber but not in the corner. At moderate S, we observe vortex breakdown, large-amplitude inertial waves, and very intense swirling motion in the corner. When S = 1, the central downdraft penetrates to the lower surface and the vortex breakdown occurs within the boundary layer. These results are consistent with experimental observations and suggest the explanation of a number of observed facets of tornadoes.
publisherAmerican Meteorological Society
titleA Study in Tornado-Like Vortex Dynamics
typeJournal Paper
journal volume36
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1979)036<0140:ASITLV>2.0.CO;2
journal fristpage140
journal lastpage155
treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 001
contenttypeFulltext


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