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dc.contributor.authorConover, W. C.
dc.contributor.authorWentzien, C. J.
dc.date.accessioned2017-06-09T14:11:12Z
dc.date.available2017-06-09T14:11:12Z
dc.date.copyright1955/04/01
dc.date.issued1955
dc.identifier.issn0095-9634
dc.identifier.otherams-14153.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149683
dc.description.abstractDuring the years 1948 to 1952, radiosonde flights were made from Belmar, New Jersey, to altitudes of 40 km. Seasonal averages of the temperature and wind data obtained from these flights indicate a definite seasonal trend at all the observed altitudes. On the average, the temperatures above 16 km are higher during the summer than the winter. The average wind speed above 22 km increases with altitude; however, it varies greatly in speed and direction with change in seasons, being in general strong and westerly (25 to 50 meters per second) during the winter, and light and easterly during the summer.
dc.publisherAmerican Meteorological Society
dc.titleWINDS AND TEMPERATURES TO FORTY KILOMETERS
dc.typeJournal Paper
dc.journal.volume12
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1955)012<0160:WATTFK>2.0.CO;2
dc.journal.fristpage160
dc.journal.lastpage164
dc.treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 002
dc.contenttypeFulltext


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