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    Lagrangian Dispersion Model for Nonneutrally Buoyant Plumes

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 003::page 427
    Author:
    Yamada, Tetsuji
    DOI: 10.1175/1520-0450(2000)039<0427:LDMFNB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A capability to address positive and negative buoyancy was added to the Higher-Order Turbulence Model for Atmospheric Circulation?Random Puff Transport and Diffusion (HOTMAC?RAPTAD) modeling system. The modeling system was applied to simulate dense gas plumes, and the modeled concentrations were compared with observations reported in the Modelers? Data Archives (MDA). Sampling sites reported in MDA were located mostly 50?800 m from the source over flat terrain. To detect a peak concentration, RAPTAD sampling sites were placed on the arcs whose radii correspond to the sampling distance reported in MDA. Concentration averaging time for a peak concentration was varied from 1 to 600 s. RAPTAD simulation time varied from 4 to 30 min. The overall performance of the current model in terms of geometric mean biases, geometric variances, and residual plots was found to be at least as good as those of the better models examined previously with the same dataset.
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      Lagrangian Dispersion Model for Nonneutrally Buoyant Plumes

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148209
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    contributor authorYamada, Tetsuji
    date accessioned2017-06-09T14:07:21Z
    date available2017-06-09T14:07:21Z
    date copyright2000/03/01
    date issued2000
    identifier issn0894-8763
    identifier otherams-12827.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148209
    description abstractA capability to address positive and negative buoyancy was added to the Higher-Order Turbulence Model for Atmospheric Circulation?Random Puff Transport and Diffusion (HOTMAC?RAPTAD) modeling system. The modeling system was applied to simulate dense gas plumes, and the modeled concentrations were compared with observations reported in the Modelers? Data Archives (MDA). Sampling sites reported in MDA were located mostly 50?800 m from the source over flat terrain. To detect a peak concentration, RAPTAD sampling sites were placed on the arcs whose radii correspond to the sampling distance reported in MDA. Concentration averaging time for a peak concentration was varied from 1 to 600 s. RAPTAD simulation time varied from 4 to 30 min. The overall performance of the current model in terms of geometric mean biases, geometric variances, and residual plots was found to be at least as good as those of the better models examined previously with the same dataset.
    publisherAmerican Meteorological Society
    titleLagrangian Dispersion Model for Nonneutrally Buoyant Plumes
    typeJournal Paper
    journal volume39
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2000)039<0427:LDMFNB>2.0.CO;2
    journal fristpage427
    journal lastpage436
    treeJournal of Applied Meteorology:;2000:;volume( 039 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian