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    Turbulence Kinetic Energy Budget Profiles Derived from Doppler Sodar Measurements

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 002::page 99
    Author:
    Greenhut, Gary K.
    ,
    Mastrantonio, Giangiuseppe
    DOI: 10.1175/1520-0450(1989)028<0099:TKEBPD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Doppler sodar wind measurements made in light wind conditions in September 1979 near a power plant in Turbigo, Italy, are used to derive terms in the turbulence kinetic energy (TKE) budget. Measurements on five days are grouped into two classes: fair-weather conditions and boundary layer interaction with subsiding air. Profiles of σ3w/z are used to obtain the surface heat flux and the vertical velocity scaling parameter, as well as the buoyancy production term in the TKE budget. The vertical transport of TKE is derived from the profiles of (w?)3. The horizontal components are approximated using a parameterization based on the data of Lenschow et al. Dissipation in the TKE budget is obtained from a spectral analysis of the Doppler sodar data in the inertial subrange. The resulting TKE budget profiles for the two classes are compared with budgets obtained previously, using a number of different methods.
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      Turbulence Kinetic Energy Budget Profiles Derived from Doppler Sodar Measurements

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4146640
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    contributor authorGreenhut, Gary K.
    contributor authorMastrantonio, Giangiuseppe
    date accessioned2017-06-09T14:02:36Z
    date available2017-06-09T14:02:36Z
    date copyright1989/02/01
    date issued1989
    identifier issn0894-8763
    identifier otherams-11414.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146640
    description abstractDoppler sodar wind measurements made in light wind conditions in September 1979 near a power plant in Turbigo, Italy, are used to derive terms in the turbulence kinetic energy (TKE) budget. Measurements on five days are grouped into two classes: fair-weather conditions and boundary layer interaction with subsiding air. Profiles of σ3w/z are used to obtain the surface heat flux and the vertical velocity scaling parameter, as well as the buoyancy production term in the TKE budget. The vertical transport of TKE is derived from the profiles of (w?)3. The horizontal components are approximated using a parameterization based on the data of Lenschow et al. Dissipation in the TKE budget is obtained from a spectral analysis of the Doppler sodar data in the inertial subrange. The resulting TKE budget profiles for the two classes are compared with budgets obtained previously, using a number of different methods.
    publisherAmerican Meteorological Society
    titleTurbulence Kinetic Energy Budget Profiles Derived from Doppler Sodar Measurements
    typeJournal Paper
    journal volume28
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1989)028<0099:TKEBPD>2.0.CO;2
    journal fristpage99
    journal lastpage106
    treeJournal of Applied Meteorology:;1989:;volume( 028 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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