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    APPLICATION OF THE HEAT BALANCE APPROACH TO MAXIMUM TEMPERATURE FORECASTING

    Source: Monthly Weather Review:;1958:;volume( 086 ):;issue: 005::page 165
    Author:
    KLEINSASSER, THEODORE W.
    ,
    YOUNKIN, RUSSELL J.
    DOI: 10.1175/1520-0493(1958)086<0165:AOTHBA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The daily net energy available for heating the air from 0300 GMT to the following afternoon, as determined by Myers, is used to compute objectively the maximum temperature expected under static, clear-sky conditions at 12 cities in the power distribution area of the Tennessee Valley Authority. The maximum temperatures thus obtained are plotted and analyzed to resolve irregular features of the isotherm patterns. The analysis is then adjusted subjectively primarily for the effect of temperature advection but also for cloudiness, precipitational cooling, and vertical motion?to take account of changes expected by mid-afternoon of the current day and also of the following day. Verification results for seven cities in the TVA area during 1954 and 1955 are presented. The current-day forecast errors are approximately 50 percent less than persistence forecast errors.
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      APPLICATION OF THE HEAT BALANCE APPROACH TO MAXIMUM TEMPERATURE FORECASTING

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4197286
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    • Monthly Weather Review

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    contributor authorKLEINSASSER, THEODORE W.
    contributor authorYOUNKIN, RUSSELL J.
    date accessioned2017-06-09T15:56:10Z
    date available2017-06-09T15:56:10Z
    date copyright1958/05/01
    date issued1958
    identifier issn0027-0644
    identifier otherams-57000.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197286
    description abstractThe daily net energy available for heating the air from 0300 GMT to the following afternoon, as determined by Myers, is used to compute objectively the maximum temperature expected under static, clear-sky conditions at 12 cities in the power distribution area of the Tennessee Valley Authority. The maximum temperatures thus obtained are plotted and analyzed to resolve irregular features of the isotherm patterns. The analysis is then adjusted subjectively primarily for the effect of temperature advection but also for cloudiness, precipitational cooling, and vertical motion?to take account of changes expected by mid-afternoon of the current day and also of the following day. Verification results for seven cities in the TVA area during 1954 and 1955 are presented. The current-day forecast errors are approximately 50 percent less than persistence forecast errors.
    publisherAmerican Meteorological Society
    titleAPPLICATION OF THE HEAT BALANCE APPROACH TO MAXIMUM TEMPERATURE FORECASTING
    typeJournal Paper
    journal volume86
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1958)086<0165:AOTHBA>2.0.CO;2
    journal fristpage165
    journal lastpage170
    treeMonthly Weather Review:;1958:;volume( 086 ):;issue: 005
    contenttypeFulltext
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