A Study in Tornado-Like Vortex DynamicsSource: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 001::page 140Author:Rotunno, Richard
DOI: 10.1175/1520-0469(1979)036<0140:ASITLV>2.0.CO;2Publisher: American Meteorological Society
Abstract: Fine-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.
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contributor author | Rotunno, Richard | |
date accessioned | 2017-06-09T14:20:35Z | |
date available | 2017-06-09T14:20:35Z | |
date copyright | 1979/01/01 | |
date issued | 1979 | |
identifier issn | 0022-4928 | |
identifier other | ams-17633.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4153549 | |
description abstract | Fine-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. | |
publisher | American Meteorological Society | |
title | A Study in Tornado-Like Vortex Dynamics | |
type | Journal Paper | |
journal volume | 36 | |
journal issue | 1 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1979)036<0140:ASITLV>2.0.CO;2 | |
journal fristpage | 140 | |
journal lastpage | 155 | |
tree | Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 001 | |
contenttype | Fulltext |