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contributor authorWakimoto, Roger M.
date accessioned2017-06-09T16:05:45Z
date available2017-06-09T16:05:45Z
date copyright1986/04/01
date issued1986
identifier issn0027-0644
identifier otherams-60804.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201515
description abstractOn 5 June 1982, a clear-air mesocyclone translated through the observational network of the Joint Airport Weather Studies (JAWS) Project new Denver, Colorado. Mesoscale analysis revealed both a mesocirculation defined by the wind field, and a mesolow defined by the pressure field. The mesocyclone appeared to be a result of a foehn-type wind descending the slopes of the Front Range of the Rocky Mountains. It is believed that this feature is the ?shallow orographic low? that has been shown in past studies to be an important stage in the development of cyclones in the lee of large mountain ranges.
publisherAmerican Meteorological Society
titleClear-Air Mesocyclone during the JAWS Project
typeJournal Paper
journal volume114
journal issue4
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1986)114<0736:CAMDTJ>2.0.CO;2
journal fristpage736
journal lastpage744
treeMonthly Weather Review:;1986:;volume( 114 ):;issue: 004
contenttypeFulltext


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