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    The Subgrid Velocity Scale in the Bulk Aerodynamic Relationship for Spatially Averaged Scalar Fluxes

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 010::page 3032
    Author:
    Mahrt, L. T.
    ,
    Sun, Jielun
    DOI: 10.1175/1520-0493(1995)123<3032:TSVSIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The exchange coefficients for area-averaged surface fluxes can become anomalously large when the large-scale flow is weak and significant fluxes of heat and moisture are driven by mesoscale motions within the averaging or subgrid area. To prevent this erratic behavior of the exchange coefficient, the ?subgrid velocity scale? must be included to account for generation of turbulent fluxes by subgrid mesoscale motions. This velocity scale is obtained by spatially averaging the local time-averaged velocity used in the bulk aerodynamic relationship. The subgrid velocity scale is distinct from the free convection velocity scale included in the bulk aerodynamic relationship to represent transport induced by convectively driven boundary-layer-scale eddies (Godfrey and Beljaars; Beljaars).The formulation of Godfrey and Beljaars is derived by time averaging the velocity scale of the bulk aerodynamic relationship. The behavior of the subgrid velocity scale is explored using data from five different field programs. Ubiquitous ?nameless? mesoscale motions of unknown origin are found in all of the datasets. The addition of the subgrid velocity scale reduces the dependence of the exchange coefficients on grid size. Based on the data analysis, the subgrid velocity scale increases with grid size and contains a contribution due to surface heterogeneity.
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      The Subgrid Velocity Scale in the Bulk Aerodynamic Relationship for Spatially Averaged Scalar Fluxes

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203522
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    contributor authorMahrt, L. T.
    contributor authorSun, Jielun
    date accessioned2017-06-09T16:10:30Z
    date available2017-06-09T16:10:30Z
    date copyright1995/10/01
    date issued1995
    identifier issn0027-0644
    identifier otherams-62611.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203522
    description abstractThe exchange coefficients for area-averaged surface fluxes can become anomalously large when the large-scale flow is weak and significant fluxes of heat and moisture are driven by mesoscale motions within the averaging or subgrid area. To prevent this erratic behavior of the exchange coefficient, the ?subgrid velocity scale? must be included to account for generation of turbulent fluxes by subgrid mesoscale motions. This velocity scale is obtained by spatially averaging the local time-averaged velocity used in the bulk aerodynamic relationship. The subgrid velocity scale is distinct from the free convection velocity scale included in the bulk aerodynamic relationship to represent transport induced by convectively driven boundary-layer-scale eddies (Godfrey and Beljaars; Beljaars).The formulation of Godfrey and Beljaars is derived by time averaging the velocity scale of the bulk aerodynamic relationship. The behavior of the subgrid velocity scale is explored using data from five different field programs. Ubiquitous ?nameless? mesoscale motions of unknown origin are found in all of the datasets. The addition of the subgrid velocity scale reduces the dependence of the exchange coefficients on grid size. Based on the data analysis, the subgrid velocity scale increases with grid size and contains a contribution due to surface heterogeneity.
    publisherAmerican Meteorological Society
    titleThe Subgrid Velocity Scale in the Bulk Aerodynamic Relationship for Spatially Averaged Scalar Fluxes
    typeJournal Paper
    journal volume123
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1995)123<3032:TSVSIT>2.0.CO;2
    journal fristpage3032
    journal lastpage3041
    treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 010
    contenttypeFulltext
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