YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    A Global Nonhydrostatic Semi-Lagrangian Atmospheric Model with Orography

    Source: Monthly Weather Review:;1998:;volume( 126 ):;issue: 003::page 747
    Author:
    Qian, Jian-Hua
    ,
    Semazzi, Fredrick H. M.
    ,
    Scroggs, Jeffrey S.
    DOI: 10.1175/1520-0493(1998)126<0747:AGNSLA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A global nonhydrostatic semi-implicit semi-Lagrangian (SISL) atmospheric model with orography has been developed. The height-based terrain-following σz coordinate of Gal-Chen and Somerville is used to incorporate the orography. A 3D vector form of the SISL formulation is proposed. It is based on the complete Navier?Stokes equations. The model is stable for large time steps of up to 1 h at horizontal/vertical resolution of 2.8125°/1200 m. Isolated bell-shaped mountain profiles and real orography are employed to evaluate the model performance. The sensitivity of the model with orography to the order of accuracy of the uncentering scheme, the reference temperature (T), and size of the time step are similar to that of the model without orography described in Semazzi et al. The authors find that for successful execution of the model, it is important that the orographic height Zs, the reference state mass variable (qs), and T satisfy the hydrostatic balance relationship in the terrain-following σz coordinate system. This formulation effectively controls the generation of unphysical orographic induced computational noise usually encountered in connection with semi-Lagrangian models. The global model used here is based on the complete dynamical Navier?Stokes equations, however, it is run at coarse resolutions, for which nonhydrostatic effects are negligible. In the future, when the computing resources permit, the model will be a valuable vehicle for investigating the role of multiple-scale interaction, including the effects of nonhydrostatic dynamics.
    • Download: (616.8Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      A Global Nonhydrostatic Semi-Lagrangian Atmospheric Model with Orography

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4204037
    Collections
    • Monthly Weather Review

    Show full item record

    contributor authorQian, Jian-Hua
    contributor authorSemazzi, Fredrick H. M.
    contributor authorScroggs, Jeffrey S.
    date accessioned2017-06-09T16:11:48Z
    date available2017-06-09T16:11:48Z
    date copyright1998/03/01
    date issued1998
    identifier issn0027-0644
    identifier otherams-63074.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204037
    description abstractA global nonhydrostatic semi-implicit semi-Lagrangian (SISL) atmospheric model with orography has been developed. The height-based terrain-following σz coordinate of Gal-Chen and Somerville is used to incorporate the orography. A 3D vector form of the SISL formulation is proposed. It is based on the complete Navier?Stokes equations. The model is stable for large time steps of up to 1 h at horizontal/vertical resolution of 2.8125°/1200 m. Isolated bell-shaped mountain profiles and real orography are employed to evaluate the model performance. The sensitivity of the model with orography to the order of accuracy of the uncentering scheme, the reference temperature (T), and size of the time step are similar to that of the model without orography described in Semazzi et al. The authors find that for successful execution of the model, it is important that the orographic height Zs, the reference state mass variable (qs), and T satisfy the hydrostatic balance relationship in the terrain-following σz coordinate system. This formulation effectively controls the generation of unphysical orographic induced computational noise usually encountered in connection with semi-Lagrangian models. The global model used here is based on the complete dynamical Navier?Stokes equations, however, it is run at coarse resolutions, for which nonhydrostatic effects are negligible. In the future, when the computing resources permit, the model will be a valuable vehicle for investigating the role of multiple-scale interaction, including the effects of nonhydrostatic dynamics.
    publisherAmerican Meteorological Society
    titleA Global Nonhydrostatic Semi-Lagrangian Atmospheric Model with Orography
    typeJournal Paper
    journal volume126
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1998)126<0747:AGNSLA>2.0.CO;2
    journal fristpage747
    journal lastpage771
    treeMonthly Weather Review:;1998:;volume( 126 ):;issue: 003
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian