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dc.contributor.authorBoville, B. W.
dc.contributor.authorWilson, C. V.
dc.contributor.authorHare, F. K.
dc.date.accessioned2017-06-09T14:12:42Z
dc.date.available2017-06-09T14:12:42Z
dc.date.copyright1961/10/01
dc.date.issued1961
dc.identifier.issn0095-9634
dc.identifier.otherams-14766.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150363
dc.description.abstractThe behavior of the polar-night westerlies of the stratosphere is discussed, and their probable vertical extent is examined from rocket sounding evidence. It is shown that travelling wave-perturbations, typically of zonal wave number near four, affect the vortex and have phase-velocities similar to those of the tropospheric westerlies. The amplification and movement of one of these systems is shown by means of a detailed case-study of vorticity and mass perturbations. The writers conclude that the behavior of these systems supports the view that they are baroclinic waves converting available potential energy to kinetic energy at stratospheric levels.
dc.publisherAmerican Meteorological Society
dc.titleBAROCLINIC WAVES OF THE POLAR-NIGHT VORTEX
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue5
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1961)018<0567:BWOTPN>2.0.CO;2
dc.journal.fristpage567
dc.journal.lastpage580
dc.treeJournal of Meteorology:;1961:;volume( 018 ):;issue: 005
dc.contenttypeFulltext


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