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contributor authorWACO, DAVID E.
date accessioned2017-06-09T15:59:26Z
date available2017-06-09T15:59:26Z
date copyright1970/10/01
date issued1970
identifier issn0027-0644
identifier otherams-58252.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198679
description abstractHorizontal and vertical temperature variations along with true gust velocity measurements of atmospheric turbulence were obtained above hurricane Beulah (1967) by an instrumented U?2. The U?2 flight was part of the U.S. Air Force High Altitude Clear Air Turbulence program. Pertinent findings include: (1) location of the tropopause just above the cloud tops at 54,000 ft (100 mb) with a temperature of ?86°C, 12°C lower than the mean; (2) a vertical temperature rise of 11°C in a few hundred feet just above the tropopause; (3) horizontal temperature changes up to 7°C and smooth flight conditions in the stable layer above the cloud tops; and (4) small temperature fluctuations and generally turbulent conditions at cloud top level. Aircraft measured winds, although questionable as to their exact directions and speeds, indicated that the flow was weak and anticyclonic near Beulah's top, becoming increasingly anticyclonic above.
publisherAmerican Meteorological Society
titleTEMPERATURES AND TURBULENCE AT TROPOPAUSE LEVELS OVER HURRICANE BEULAH (1967)
typeJournal Paper
journal volume98
journal issue10
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1970)098<0749:TATATL>2.3.CO;2
journal fristpage749
journal lastpage755
treeMonthly Weather Review:;1970:;volume( 098 ):;issue: 010
contenttypeFulltext


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