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dc.contributor.authorCressman, George P.
dc.date.accessioned2017-06-09T14:10:56Z
dc.date.available2017-06-09T14:10:56Z
dc.date.copyright1954/04/01
dc.date.issued1954
dc.identifier.issn0095-9634
dc.identifier.otherams-14052.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149571
dc.description.abstractWith the vorticity equation for horizontal motion as a beginning, and with the aid of several assumptions, the equation ?H·? = ?T·?H In ? is derived, giving the horizontal divergence as the product of (?T) the vector wind-difference between the level in question and 600 mb, and the logarithm of the absolute vorticity (?) at the level where the divergence is desired. The divergence at 850 mb is computed for a variety of situations with the above equation and is compared with vertical velocities, with the divergence computed from the wind field, and with observed weather distributions, the comparisons yielding favorable results. Finally, suggestions are made for the use of the method for divergence determination in the prognostic routine.
dc.publisherAmerican Meteorological Society
dc.titleAN APPROXIMATE METHOD OF DIVERGENCE MEASUREMENT
dc.typeJournal Paper
dc.journal.volume11
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1954)011<0083:AAMODM>2.0.CO;2
dc.journal.fristpage83
dc.journal.lastpage90
dc.treeJournal of Meteorology:;1954:;volume( 011 ):;issue: 002
dc.contenttypeFulltext


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