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dc.contributor.authorCressman, George P.
dc.date.accessioned2017-06-09T14:10:40Z
dc.date.available2017-06-09T14:10:40Z
dc.date.copyright1953/02/01
dc.date.issued1953
dc.identifier.issn0095-9634
dc.identifier.otherams-13958.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149465
dc.description.abstractThe analysis and use of charts of absolute vorticity are described. Measurements from a winter and a summer series of maps gave 608 and 641 mb, respectively, as the pressure at the mean equivalent barotropic surface. It is shown that, on charts near the equivalent barotropic surface, the absolute-vorticity patterns give indications useful in short-range forecasting, since the lines of constant absolute vorticity are advected with nearly the speed of the wind. Examples are presented, showing typical contour and vorticity patterns for a rapidly moving pattern, a stationary pattern, and a situation of rapid trough development.
dc.publisherAmerican Meteorological Society
dc.titleAN APPLICATION OF ABSOLUTE-VORTICITY CHARTS
dc.typeJournal Paper
dc.journal.volume10
dc.journal.issue1
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1953)010<0017:AAOAVC>2.0.CO;2
dc.journal.fristpage17
dc.journal.lastpage24
dc.treeJournal of Meteorology:;1953:;volume( 010 ):;issue: 001
dc.contenttypeFulltext


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