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contributor authorAbdullah, Abdul Jabbar
date accessioned2017-06-09T14:13:50Z
date available2017-06-09T14:13:50Z
date copyright1966/07/01
date issued1966
identifier issn0022-4928
identifier otherams-15209.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150856
description abstractIn this paper an attempt is made to explain the shape and behavior of the spiral bands of a hurricane. The main hypothesis is that the bands are associated with gravitational waves of finite amplitude propagating at. the interface of a high-level inversion. An external source of disturbance is postulated in the form of a fresh surge of air at the exterior region of the hurricane. It is shown that this mechanism leads to the formation of bands of the required shape. The spiral bands are therefore related to the squall lines of temperate latitudes. Two numerical examples are worked out to illustrate the proposed mechanism.
publisherAmerican Meteorological Society
titleThe Spiral Bands of a Hurricane: A Possible Dynamic Explanation
typeJournal Paper
journal volume23
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1966)023<0367:TSBOAH>2.0.CO;2
journal fristpage367
journal lastpage375
treeJournal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 004
contenttypeFulltext


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