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    The Simulation of the Southern Great Plains Nocturnal Boundary Layer and the Low-Level Jet with a High-Resolution Mesoscale Atmospheric Model

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 007::page 1497
    Author:
    Werth, David
    ,
    Kurzeja, Robert
    ,
    Dias, Nelson Luís
    ,
    Zhang, Gengsheng
    ,
    Duarte, Henrique
    ,
    Fischer, Marc
    ,
    Parker, Matthew
    ,
    Leclerc, Monique
    DOI: 10.1175/2011JAMC2272.1
    Publisher: American Meteorological Society
    Abstract: field project over the Atmospheric Radiation Measurement?Cloud and Radiation Test Bed (ARM?CART) site during a period of several nights in September 2007 was conducted to explore the evolution of the low-level jet (LLJ). Data were collected from in situ (a multilevel tower) and remote (sodar) sensors, and the observed LLJ activity during the project was found to agree well with data from earlier studies regarding jet speed, height, and direction. To study nocturnal boundary layer (NBL) behavior, the Regional Atmospheric Modeling System was used to simulate the ARM?CART NBL field experiment and was validated against the data collected from the site. This model was run at high resolution for calculating the interactions among the various motions within the boundary layer and their influence on the surface. The model faithfully simulated the formation and dissolution of the low-level nocturnal jet during a synoptic situation in which low pressure with warm southerly advection replaced high pressure. An additional simulation at 32.5-m resolution was performed for the most stable 5.5-h period, using a turbulence scheme adjusted to allow for greater resolved turbulent kinetic energy, and the model reproduced the turbulence statistics as determined by a power spectrum. The benefit of the high-resolution simulation is evident in the much more realistically resolved model turbulent kinetic energy and the fluxes of momentum, heat, and water vapor.
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      The Simulation of the Southern Great Plains Nocturnal Boundary Layer and the Low-Level Jet with a High-Resolution Mesoscale Atmospheric Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4213535
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    • Journal of Applied Meteorology and Climatology

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    contributor authorWerth, David
    contributor authorKurzeja, Robert
    contributor authorDias, Nelson Luís
    contributor authorZhang, Gengsheng
    contributor authorDuarte, Henrique
    contributor authorFischer, Marc
    contributor authorParker, Matthew
    contributor authorLeclerc, Monique
    date accessioned2017-06-09T16:39:13Z
    date available2017-06-09T16:39:13Z
    date copyright2011/07/01
    date issued2011
    identifier issn1558-8424
    identifier otherams-71622.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213535
    description abstractfield project over the Atmospheric Radiation Measurement?Cloud and Radiation Test Bed (ARM?CART) site during a period of several nights in September 2007 was conducted to explore the evolution of the low-level jet (LLJ). Data were collected from in situ (a multilevel tower) and remote (sodar) sensors, and the observed LLJ activity during the project was found to agree well with data from earlier studies regarding jet speed, height, and direction. To study nocturnal boundary layer (NBL) behavior, the Regional Atmospheric Modeling System was used to simulate the ARM?CART NBL field experiment and was validated against the data collected from the site. This model was run at high resolution for calculating the interactions among the various motions within the boundary layer and their influence on the surface. The model faithfully simulated the formation and dissolution of the low-level nocturnal jet during a synoptic situation in which low pressure with warm southerly advection replaced high pressure. An additional simulation at 32.5-m resolution was performed for the most stable 5.5-h period, using a turbulence scheme adjusted to allow for greater resolved turbulent kinetic energy, and the model reproduced the turbulence statistics as determined by a power spectrum. The benefit of the high-resolution simulation is evident in the much more realistically resolved model turbulent kinetic energy and the fluxes of momentum, heat, and water vapor.
    publisherAmerican Meteorological Society
    titleThe Simulation of the Southern Great Plains Nocturnal Boundary Layer and the Low-Level Jet with a High-Resolution Mesoscale Atmospheric Model
    typeJournal Paper
    journal volume50
    journal issue7
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2011JAMC2272.1
    journal fristpage1497
    journal lastpage1513
    treeJournal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 007
    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