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    On the Mesometeorological Field Studies near Flagstaff, Arizona

    Source: Journal of Applied Meteorology:;1962:;volume( 001 ):;issue: 001::page 26
    Author:
    Fujita, Tetsuya
    ,
    Styber, Kenneth A.
    ,
    Brown, Rodger A.
    DOI: 10.1175/1520-0450(1962)001<0026:OTMFSN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: During 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.
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      On the Mesometeorological Field Studies near Flagstaff, Arizona

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4209833
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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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