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    The Use of Satellite Imagery and Surface Pressure-Gradient Analysis Modified for Sloping Terrain to Analyze the Mesoscale Events Preceding the Severe Hailstorms of 2 August 1986

    Source: Weather and Forecasting:;1990:;volume( 005 ):;issue: 002::page 279
    Author:
    Weaver, John F.
    ,
    Toth, James J.
    DOI: 10.1175/1520-0434(1990)005<0279:TUOSIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Conditions leading up to an outbreak of severe hailstorms in northeast Colorado are examined using satellite and surface data. A persistent mesoscale ridge of surface-high pressure, caused by outflow from a mesoscale- convective system, is seen to coincide with the occurrence of large hail which was confined to a narrow band extending nearly parallel to the Front Range of the Rocky Mountains. The development of the mesoscale ridge during its most intense stages is documented using a procedure that yields an approximate streamfunction for the surface geostrophic wind. Unlike alternatives over sloping terrain, this method is quick and can be adjusted to minimize the error over a limited portion of the analysis area.
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      The Use of Satellite Imagery and Surface Pressure-Gradient Analysis Modified for Sloping Terrain to Analyze the Mesoscale Events Preceding the Severe Hailstorms of 2 August 1986

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162190
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    contributor authorWeaver, John F.
    contributor authorToth, James J.
    date accessioned2017-06-09T14:43:48Z
    date available2017-06-09T14:43:48Z
    date copyright1990/06/01
    date issued1990
    identifier issn0882-8156
    identifier otherams-2541.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162190
    description abstractConditions leading up to an outbreak of severe hailstorms in northeast Colorado are examined using satellite and surface data. A persistent mesoscale ridge of surface-high pressure, caused by outflow from a mesoscale- convective system, is seen to coincide with the occurrence of large hail which was confined to a narrow band extending nearly parallel to the Front Range of the Rocky Mountains. The development of the mesoscale ridge during its most intense stages is documented using a procedure that yields an approximate streamfunction for the surface geostrophic wind. Unlike alternatives over sloping terrain, this method is quick and can be adjusted to minimize the error over a limited portion of the analysis area.
    publisherAmerican Meteorological Society
    titleThe Use of Satellite Imagery and Surface Pressure-Gradient Analysis Modified for Sloping Terrain to Analyze the Mesoscale Events Preceding the Severe Hailstorms of 2 August 1986
    typeJournal Paper
    journal volume5
    journal issue2
    journal titleWeather and Forecasting
    identifier doi10.1175/1520-0434(1990)005<0279:TUOSIA>2.0.CO;2
    journal fristpage279
    journal lastpage298
    treeWeather and Forecasting:;1990:;volume( 005 ):;issue: 002
    contenttypeFulltext
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