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dc.contributor.authorLowe, A. B.
dc.contributor.authorMcKay, G. A.
dc.date.accessioned2017-06-09T16:28:13Z
dc.date.available2017-06-09T16:28:13Z
dc.date.copyright1962/06/01
dc.date.issued1962
dc.identifier.issn0021-8952
dc.identifier.otherams-6844.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210000
dc.description.abstractComposite charts of tornado situations are presented for the surface, 850-, 700-, 500-, and 200-mb levels for Manitoba and Saskatchewan. These charts do not cover all possible situations but are only for the most common type and for the regions of highest frequency. Tornado situations were typed according to surface-level synoptic patterns. The most common occurrence (76 per cent) was along an instability line which preceded, and was parallel to, a cold front. This instability line may have intersected a diffuse warm front near the tornado location. Three other categories were noted. The average airmass characteristics and composite charts are very similar to those found for the Great Plains area of the United States.
dc.publisherAmerican Meteorological Society
dc.titleTornado Composite Charts for the Canadian Prairies
dc.typeJournal Paper
dc.journal.volume1
dc.journal.issue2
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1962)001<0157:TCCFTC>2.0.CO;2
dc.journal.fristpage157
dc.journal.lastpage162
dc.treeJournal of Applied Meteorology:;1962:;volume( 001 ):;issue: 002
dc.contenttypeFulltext


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