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    Computation of Ground Surface Conduction Heat Flux by Fourier Analysis of Surface Temperature

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 003::page 277
    Author:
    Cautenet, Guy
    ,
    Legrand, Michel
    ,
    Coulibaly, Yaya
    ,
    Boutin, Christian
    DOI: 10.1175/1520-0450(1986)025<0277:COGSCH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A method for computing the ground surface heat flux density is tested at two places in West Africa during the rainy season and during the dry season. This method is based upon the Fourier analysis of the experimental ground surface temperature. The only required parameter is the soil thermal inertia. The results of these calculations agree with the measurements. This method avoids the use of empirical formulas relating the ground heat flux density to other terms of the surface energy budget. It is shown that these relations are not universal.
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      Computation of Ground Surface Conduction Heat Flux by Fourier Analysis of Surface Temperature

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146138
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    • Journal of Climate and Applied Meteorology

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    contributor authorCautenet, Guy
    contributor authorLegrand, Michel
    contributor authorCoulibaly, Yaya
    contributor authorBoutin, Christian
    date accessioned2017-06-09T14:01:00Z
    date available2017-06-09T14:01:00Z
    date copyright1986/03/01
    date issued1986
    identifier issn0733-3021
    identifier otherams-10963.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146138
    description abstractA method for computing the ground surface heat flux density is tested at two places in West Africa during the rainy season and during the dry season. This method is based upon the Fourier analysis of the experimental ground surface temperature. The only required parameter is the soil thermal inertia. The results of these calculations agree with the measurements. This method avoids the use of empirical formulas relating the ground heat flux density to other terms of the surface energy budget. It is shown that these relations are not universal.
    publisherAmerican Meteorological Society
    titleComputation of Ground Surface Conduction Heat Flux by Fourier Analysis of Surface Temperature
    typeJournal Paper
    journal volume25
    journal issue3
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1986)025<0277:COGSCH>2.0.CO;2
    journal fristpage277
    journal lastpage283
    treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 003
    contenttypeFulltext
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