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contributor authorReynolds, Ralph D.
date accessioned2017-06-09T17:26:02Z
date available2017-06-09T17:26:02Z
date copyright1973/03/01
date issued1973
identifier issn0021-8952
identifier otherams-8518.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228600
description abstractSynchronous radar, temperature and pressure data of suitable quality, gathered from three balloon flights of the Mountain Wave Project, were analyzed in detail to show the relationships between balloon-depicted waves and isentropic and isopycnic waves. Results show that in wave conditions, superpressure balloons: 1) follow the undulations of density surfaces but overestimate crests and troughs of waves by an average error of 6%; and 2) follow isentropic surfaces, but underestimate true wave crests by.an average error of 5%, and true wave troughs by errors averaging 30%.
publisherAmerican Meteorological Society
titleSuperpressure Balloons as Isentropic/Isopycnic Tracers
typeJournal Paper
journal volume12
journal issue2
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1973)012<0369:SBAIT>2.0.CO;2
journal fristpage369
journal lastpage373
treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 002
contenttypeFulltext


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