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    Flow around a Complex Building: Comparisons between Experiments and a Reynolds-Averaged Navier–Stokes Approach

    Source: Journal of Applied Meteorology:;2004:;volume( 043 ):;issue: 005::page 696
    Author:
    Calhoun, Ronald
    ,
    Gouveia, Frank
    ,
    Shinn, Joseph
    ,
    Chan, Stevens
    ,
    Stevens, Dave
    ,
    Lee, Robert
    ,
    Leone, John
    DOI: 10.1175/2067.1
    Publisher: American Meteorological Society
    Abstract: An experiment investigating flow around a single complex building was performed in 2000. Sonic anemometers were placed around the building, and two-dimensional wind velocities were recorded. An energy-budget and wind-measuring station was located upstream to provide stability and inflow conditions. In general, the sonic anemometers were located in a horizontal plane around the building at a height of 2.6 m above the ground. However, at the upwind wind station, two levels of the wind were measured. The resulting database can be sampled to produce mean wind fields associated with specific wind directions such as 210°, 225°, and 240°. The data are available generally and should be useful for testing computational fluid dynamical models for flow around a building. An in-house Reynolds-averaged Navier?Stokes approach was used to compare with the mean wind fields for the predominant wind directions. The numerical model assumed neutral flow and included effects from a complex array of trees in the vicinity of the building. Two kinds of comparisons are presented: 1) direct experimental versus modeled vector comparisons and 2) a numerical metric approach that focuses on wind magnitude and direction errors. The numerical evaluation generally corroborates the vector-to-vector inspection, showing reasonable agreement for the mean wind fields around the building. However, regions with special challenges for the model were identified. In particular, recirculation regions were especially difficult for the model to capture correctly. In the 240° case, there is a tendency for the model to exaggerate the turning effect in the wind caused by the effect of the building. Two different kinds of simulations were performed: 1) predictive calculations with a reasonable but not high-fidelity representation of the building's architectural complexity and 2) postexperiment calculations in which a large number of architectural features were well represented. Although qualitative evidence from inspection of the angles of the vectors in key areas such as around the southeast corner of the building indicated an improvement from the higher-fidelity representation of the building, the general numerical evaluation indicated little difference in the quality of the two solutions.
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      Flow around a Complex Building: Comparisons between Experiments and a Reynolds-Averaged Navier–Stokes Approach

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4214294
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    • Journal of Applied Meteorology

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    contributor authorCalhoun, Ronald
    contributor authorGouveia, Frank
    contributor authorShinn, Joseph
    contributor authorChan, Stevens
    contributor authorStevens, Dave
    contributor authorLee, Robert
    contributor authorLeone, John
    date accessioned2017-06-09T16:41:30Z
    date available2017-06-09T16:41:30Z
    date copyright2004/05/01
    date issued2004
    identifier issn0894-8763
    identifier otherams-72305.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214294
    description abstractAn experiment investigating flow around a single complex building was performed in 2000. Sonic anemometers were placed around the building, and two-dimensional wind velocities were recorded. An energy-budget and wind-measuring station was located upstream to provide stability and inflow conditions. In general, the sonic anemometers were located in a horizontal plane around the building at a height of 2.6 m above the ground. However, at the upwind wind station, two levels of the wind were measured. The resulting database can be sampled to produce mean wind fields associated with specific wind directions such as 210°, 225°, and 240°. The data are available generally and should be useful for testing computational fluid dynamical models for flow around a building. An in-house Reynolds-averaged Navier?Stokes approach was used to compare with the mean wind fields for the predominant wind directions. The numerical model assumed neutral flow and included effects from a complex array of trees in the vicinity of the building. Two kinds of comparisons are presented: 1) direct experimental versus modeled vector comparisons and 2) a numerical metric approach that focuses on wind magnitude and direction errors. The numerical evaluation generally corroborates the vector-to-vector inspection, showing reasonable agreement for the mean wind fields around the building. However, regions with special challenges for the model were identified. In particular, recirculation regions were especially difficult for the model to capture correctly. In the 240° case, there is a tendency for the model to exaggerate the turning effect in the wind caused by the effect of the building. Two different kinds of simulations were performed: 1) predictive calculations with a reasonable but not high-fidelity representation of the building's architectural complexity and 2) postexperiment calculations in which a large number of architectural features were well represented. Although qualitative evidence from inspection of the angles of the vectors in key areas such as around the southeast corner of the building indicated an improvement from the higher-fidelity representation of the building, the general numerical evaluation indicated little difference in the quality of the two solutions.
    publisherAmerican Meteorological Society
    titleFlow around a Complex Building: Comparisons between Experiments and a Reynolds-Averaged Navier–Stokes Approach
    typeJournal Paper
    journal volume43
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/2067.1
    journal fristpage696
    journal lastpage710
    treeJournal of Applied Meteorology:;2004:;volume( 043 ):;issue: 005
    contenttypeFulltext
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