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dc.contributor.authorMoore, C. B.
dc.contributor.authorSmith, J. R.
dc.contributor.authorGaalswyk, A.
dc.date.accessioned2017-06-09T14:10:58Z
dc.date.available2017-06-09T14:10:58Z
dc.date.copyright1954/06/01
dc.date.issued1954
dc.identifier.issn0095-9634
dc.identifier.otherams-14062.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149582
dc.description.abstractIn the course of government-sponsored work in the development of the constant-level balloon, the writers supervised many constant-level balloon flights on the standard meteorological surface of 300 millibars. The tracks of these flights are of general meteorological interest, as they are believed to delineate the actual trajectory of an equivalent mass of air travelling on a constant-pressure surface. Some of the original flight data are presented for the information of other investigators of air motion, and to illustrate the application of constant-level balloons to meteorological problems, particularly atmospheric diffusion and the variability of the wind. Suggestions are made regarding the significance of the data presented, and further experiments are proposed which might result in a better understanding of the mechanisms of air motion. Possible applications of constant-level balloons in routine observations, to obtain representative measurements of wind velocity, are set forth.
dc.publisherAmerican Meteorological Society
dc.titleON THE USE OF CONSTANT-LEVEL BALLOONS TO MEASURE HORIZONTAL MOTIONS IN THE ATMOSPHERE
dc.typeJournal Paper
dc.journal.volume11
dc.journal.issue3
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1954)011<0167:OTUOCL>2.0.CO;2
dc.journal.fristpage167
dc.journal.lastpage172
dc.treeJournal of Meteorology:;1954:;volume( 011 ):;issue: 003
dc.contenttypeFulltext


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