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Article >  Journal of Tropical Meteorology  > 2000 >  6(2): 219-224

A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER

  • Guangzhou Institute of Tropical and Oceanic Meteorology, Guangzhou 510080 China

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  • Derivation of bulk transport coefficients helps solving land surface processes. A similarity-based method for determining the turbulent transfer (including the flux exchange, the vertical distribution of wind and potential temperature) in the atmospheric surface layer is presented. Comparisons with iterative schemes (Businger, 1971) are given to demonstrate the advantages of the calculation methods.
  • [1] BUSINGER J A, WYNGAARD J C, IZUMI Y, BRADLEY E F, 1971. Flux-profile relationships in the atmos-pheric surface layer [J]. J. Atmos. Sci., 28:181-189.
    [2] DYER A J, 1974. A review of flux-profile relationships [J]. Boundary Layer Meteorology, 7:363-372.
    [3] PANOFSKY H A, 1963. Determination of stress from wind and temperature measurements [J]. Quart. J. Roy. Meteor. Soc., 89:85-94.
    [4] RACHELE H, TUNICK A, HANSEN F V, 1995. MARIAH-A similarity-based method for determining wind temperature, and humidity profile structure in the atmospheric surface layer [J]. J. Appl.Meteor., 34:1000-1005.
    [5] YAGLOM A M, 1977. Comments on wind and temperature flux profile relationships [M]. Boundary Layer Meteorology,11:89-102.
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WAN Qi-lin. A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER [J]. Journal of Tropical Meteorology, 2000, 6(2): 219-224.
WAN Qi-lin. A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER [J]. Journal of Tropical Meteorology, 2000, 6(2): 219-224.
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    • Manuscript History

    Manuscript received: 30 August 1999
    Manuscript revised: 25 August 2000
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    A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER

    • Guangzhou Institute of Tropical and Oceanic Meteorology, Guangzhou 510080 China
    • Received Date: 1999-08-30
    • Rev Recd Date: 2000-08-25

    Abstract: Derivation of bulk transport coefficients helps solving land surface processes. A similarity-based method for determining the turbulent transfer (including the flux exchange, the vertical distribution of wind and potential temperature) in the atmospheric surface layer is presented. Comparisons with iterative schemes (Businger, 1971) are given to demonstrate the advantages of the calculation methods.

    WAN Qi-lin. A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER [J]. Journal of Tropical Meteorology, 2000, 6(2): 219-224.
    Citation: WAN Qi-lin. A METHOD FOR DETERMINING TURBULENT TRANSFER IN THE ATMOSPHERIC SURFACE LAYER [J]. Journal of Tropical Meteorology, 2000, 6(2): 219-224.
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