YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • 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

    Potential Vorticity as Meridional Coordinate

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 002::page 621
    Author:
    Stan, Cristiana
    ,
    Randall, David A.
    DOI: 10.1175/JAS3839.1
    Publisher: American Meteorological Society
    Abstract: The dynamical equations of atmospheric flow are written using potential vorticity as the meridional coordinate and potential temperature as the vertical coordinate. Within this system, the atmosphere is divided into undulating tubes bounded by isentropic and constant potential vorticity surfaces, and, under adiabatic and frictionless conditions, the air moves through the tubes without penetrating through the walls.
    • Download: (640.7Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Potential Vorticity as Meridional Coordinate

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4218425
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorStan, Cristiana
    contributor authorRandall, David A.
    date accessioned2017-06-09T16:53:24Z
    date available2017-06-09T16:53:24Z
    date copyright2007/02/01
    date issued2007
    identifier issn0022-4928
    identifier otherams-76023.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218425
    description abstractThe dynamical equations of atmospheric flow are written using potential vorticity as the meridional coordinate and potential temperature as the vertical coordinate. Within this system, the atmosphere is divided into undulating tubes bounded by isentropic and constant potential vorticity surfaces, and, under adiabatic and frictionless conditions, the air moves through the tubes without penetrating through the walls.
    publisherAmerican Meteorological Society
    titlePotential Vorticity as Meridional Coordinate
    typeJournal Paper
    journal volume64
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS3839.1
    journal fristpage621
    journal lastpage633
    treeJournal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 002
    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