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dc.contributor.authorPalmer, Clarence E.
dc.date.accessioned2017-06-09T14:11:42Z
dc.date.available2017-06-09T14:11:42Z
dc.date.copyright1957/10/01
dc.date.issued1957
dc.identifier.issn0095-9634
dc.identifier.otherams-14368.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149921
dc.description.abstractIt is possible that the technique of wind analysis, developed long ago by Sandstrom and V. Bjerknes, may supplement the standard isobaric and frontal analysis of surface weather maps. A first approximation to a theory concerning the relation between asymptotes in the wind field and frontal zones suggests that the technique might reveal, by simple inspection of the separate frontal and wind analyses, the speed of movement of frontal zones, changes in their intensity and the sign of the vertical motion in their neighborhood.
dc.publisherAmerican Meteorological Society
dc.titleSOME KINEMATIC ASPECTS OF FRONTAL ZONES
dc.typeJournal Paper
dc.journal.volume14
dc.journal.issue5
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1957)014<0403:SKAOFZ>2.0.CO;2
dc.journal.fristpage403
dc.journal.lastpage409
dc.treeJournal of Meteorology:;1957:;volume( 014 ):;issue: 005
dc.contenttypeFulltext


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