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contributor authorFujita, Tetsuya
contributor authorStyber, Kenneth A.
contributor authorBrown, Rodger A.
date accessioned2017-06-09T16:27:45Z
date available2017-06-09T16:27:45Z
date copyright1962/03/01
date issued1962
identifier issn0021-8952
identifier otherams-6829.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209833
description abstractDuring the month of July 1960, a mesometeorological field network was established in an area of 30 by 40 mi centered around San Francisco Mountain, Arizona. Network instrumentation included 33 micro-barographs, 10 hygrothermographs, 10 Beckman-Whitley wind recorders, about 165 nonrecording rain gauges, and 165 hail gauges. Daily precipitation amounts were carefully studied in order to relate them with the characteristics of moisture inflow into the network area. An analysis of the 22 July case over the network area revealed that a very small low-pressure area formed over the heated side of the mountain slope, providing a field of convergence leading to the morning cumulus convection. AS time went on, this low dissipated and cumulonimbus convection occurred. The mesometeorological network was found to be most suitable for the investigation of cumulus to cumulonimbus convection over the San Francisco Mountain area.
publisherAmerican Meteorological Society
titleOn the Mesometeorological Field Studies near Flagstaff, Arizona
typeJournal Paper
journal volume1
journal issue1
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1962)001<0026:OTMFSN>2.0.CO;2
journal fristpage26
journal lastpage42
treeJournal of Applied Meteorology:;1962:;volume( 001 ):;issue: 001
contenttypeFulltext


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