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    A Mathematical Model for the Generation of Hourly Temperatures

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 009::page 935
    Author:
    Hansen, James E.
    ,
    Driscoll, Dennis M.
    DOI: 10.1175/1520-0450(1977)016<0935:AMMFTG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A stochastic model for hourly temperatures for Big Spring, Tex., has been developed. The governing parameters were deduced from an 11-year developmental sample, and give hourly temperatures as a function of harmonics representing annual and diurnal variations, and a first-order Markov chain process. The latter incorporates adjustments for the seasonal variation of the serial (hour-to-hour) correlation coefficient, and for the seasonal and diurnal variations of the variability and non-normality of frequency distributions of hourly temperatures. Each of the characteristics is given explicitly as a function of hour of the year. Two 10-year samples were generated and compared to the developmental sample. Criteria were established to determine how well the model duplicates nature. The variability of mean monthly temperature and the frequency of occurrence of low diurnal ranges are underestimated. However, the model gives good estimates of the duration of temperatures below 32°F, and above 65° and 90°F, and of the frequency distribution of monthly 3, 6, 12, 24, 72 and 144 h maximum and minimum temperatures. The general applicability of the model and its utility are discussed. The model could be used to determine the effects of climatic trends, e.g., a gradual cooling, on the average length of the growing season, the mean number of heating/cooling degree days, and other temperature-related parameters.
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      A Mathematical Model for the Generation of Hourly Temperatures

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    contributor authorHansen, James E.
    contributor authorDriscoll, Dennis M.
    date accessioned2017-06-09T17:39:09Z
    date available2017-06-09T17:39:09Z
    date copyright1977/09/01
    date issued1977
    identifier issn0021-8952
    identifier otherams-9324.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232800
    description abstractA stochastic model for hourly temperatures for Big Spring, Tex., has been developed. The governing parameters were deduced from an 11-year developmental sample, and give hourly temperatures as a function of harmonics representing annual and diurnal variations, and a first-order Markov chain process. The latter incorporates adjustments for the seasonal variation of the serial (hour-to-hour) correlation coefficient, and for the seasonal and diurnal variations of the variability and non-normality of frequency distributions of hourly temperatures. Each of the characteristics is given explicitly as a function of hour of the year. Two 10-year samples were generated and compared to the developmental sample. Criteria were established to determine how well the model duplicates nature. The variability of mean monthly temperature and the frequency of occurrence of low diurnal ranges are underestimated. However, the model gives good estimates of the duration of temperatures below 32°F, and above 65° and 90°F, and of the frequency distribution of monthly 3, 6, 12, 24, 72 and 144 h maximum and minimum temperatures. The general applicability of the model and its utility are discussed. The model could be used to determine the effects of climatic trends, e.g., a gradual cooling, on the average length of the growing season, the mean number of heating/cooling degree days, and other temperature-related parameters.
    publisherAmerican Meteorological Society
    titleA Mathematical Model for the Generation of Hourly Temperatures
    typeJournal Paper
    journal volume16
    journal issue9
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1977)016<0935:AMMFTG>2.0.CO;2
    journal fristpage935
    journal lastpage948
    treeJournal of Applied Meteorology:;1977:;volume( 016 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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