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    The Use of a Two-Dimensional, Time-Dependent Cloud Model to Predict Convective and Stratiform Clouds and Precipitation

    Source: Weather and Forecasting:;1994:;volume( 009 ):;issue: 001::page 62
    Author:
    Kopp, Fred J.
    ,
    Orville, Harold D.
    DOI: 10.1175/1520-0434(1994)009<0062:TUOATD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A two-dimensional, time-dependent cloud model has been used in two field projects to forecast the convective development during the day from the morning sounding. In effect, the cloud model gives a dynamic analysis of the sounding as affected by heating and evaporation at the earth's surface, divergence of the winds throughout the atmosphere, and cloud shadow effects. During the initial project, the Cooperative Huntsville Meteorological Experiment, the results were mixed. Model runs were easily made when soundings were available, but displaying the results in a meaningful and useful way was the limiting factor. In a later experiment, the North Dakota Thunderstorm Project, the problem of displaying results was overcome and soundings were available from the local weather service forecast office with a high degree of reliability. The experimental model correctly forecasts convective development about 80% of the time, and precipitation or no precipitation more than 70% of the time.
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      The Use of a Two-Dimensional, Time-Dependent Cloud Model to Predict Convective and Stratiform Clouds and Precipitation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4164201
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    contributor authorKopp, Fred J.
    contributor authorOrville, Harold D.
    date accessioned2017-06-09T14:48:30Z
    date available2017-06-09T14:48:30Z
    date copyright1994/03/01
    date issued1994
    identifier issn0882-8156
    identifier otherams-2722.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164201
    description abstractA two-dimensional, time-dependent cloud model has been used in two field projects to forecast the convective development during the day from the morning sounding. In effect, the cloud model gives a dynamic analysis of the sounding as affected by heating and evaporation at the earth's surface, divergence of the winds throughout the atmosphere, and cloud shadow effects. During the initial project, the Cooperative Huntsville Meteorological Experiment, the results were mixed. Model runs were easily made when soundings were available, but displaying the results in a meaningful and useful way was the limiting factor. In a later experiment, the North Dakota Thunderstorm Project, the problem of displaying results was overcome and soundings were available from the local weather service forecast office with a high degree of reliability. The experimental model correctly forecasts convective development about 80% of the time, and precipitation or no precipitation more than 70% of the time.
    publisherAmerican Meteorological Society
    titleThe Use of a Two-Dimensional, Time-Dependent Cloud Model to Predict Convective and Stratiform Clouds and Precipitation
    typeJournal Paper
    journal volume9
    journal issue1
    journal titleWeather and Forecasting
    identifier doi10.1175/1520-0434(1994)009<0062:TUOATD>2.0.CO;2
    journal fristpage62
    journal lastpage77
    treeWeather and Forecasting:;1994:;volume( 009 ):;issue: 001
    contenttypeFulltext
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