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contributor authorKuo, H. L.
date accessioned2017-06-09T14:14:50Z
date available2017-06-09T14:14:50Z
date copyright1969/05/01
date issued1969
identifier issn0022-4928
identifier otherams-15595.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151284
description abstractOn including a frictional drag proportional and opposite to the velocity of a rotating cylinder or vortex placed in a shearing current, it is found that the combined influence of the drag and the rotor force resulting from the net pressure acting on the cylinder (vortex) is to make the cylinder or vortex move in a mean direction at an angle to the mean flow, toward the right if the circulation& Γ around the cylinder is positive, and toward the left if Γ is negative. In addition, the center of the cylinder also undergoes an oscillatory motion about its mean path, and the period of this oscillation and the shape of the path depend both on Γ and on the mean current. The analysis also shows that when the absolute vorticity of the basic flow is not uniform, another force in the direction of the vorticity gradient acts on the vortex, which tends to drive cyclonic vortices toward higher vorticity regions and anticyclonic vortices toward lower vorticity regions.
publisherAmerican Meteorological Society
titleMotions of Vortices and Circulating Cylinder in Shear Flow with Friction
typeJournal Paper
journal volume26
journal issue3
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1969)026<0390:MOVACC>2.0.CO;2
journal fristpage390
journal lastpage398
treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003
contenttypeFulltext


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