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dc.contributor.authorAustin, James M.
dc.contributor.authorKrawitz, Lowell
dc.date.accessioned2017-06-09T14:11:24Z
dc.date.available2017-06-09T14:11:24Z
dc.date.copyright1956/04/01
dc.date.issued1956
dc.identifier.issn0095-9634
dc.identifier.otherams-14242.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149782
dc.description.abstractData from three recent winters are utilized to study the large changes in the temperature and flow fields at 50 mb. It is reasoned that the major changes in this region arise from the development of an unstable flow pattern through the radiational cooling of air in polar regions. An analysis of tropospheric changes during periods of major activity at 50 mb indicates that the tropospheric circulation can be influenced by the developments in the upper stratosphere.
dc.publisherAmerican Meteorological Society
dc.title50-MILLIBAR PATTERNS AND THEIR RELATIONSHIP TO TROPOSPHERIC CHANGES
dc.typeJournal Paper
dc.journal.volume13
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1956)013<0152:MPATRT>2.0.CO;2
dc.journal.fristpage152
dc.journal.lastpage159
dc.treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 002
dc.contenttypeFulltext


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