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    Reading: Transparent lateral boundary conditions for baroclinic waves III. Including vertical shear

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    Original Research Papers

    Transparent lateral boundary conditions for baroclinic waves III. Including vertical shear

    Author:

    A. McDonald

    Met Éireann, Dublin, IE
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    Abstract

    The problem of how to adapt the so-called transparent boundary conditions to the physical reality that the horizontal advection velocity varies in the vertical, is addressed. A practical demonstration is presented of the transparency of the resulting ‘shear’ boundary conditions.

    How to Cite: McDonald, A., 2009. Transparent lateral boundary conditions for baroclinic waves III. Including vertical shear. Tellus A: Dynamic Meteorology and Oceanography, 61(2), pp.227–231. DOI: http://doi.org/10.1111/j.1600-0870.2008.00367.x
      Published on 01 Jan 2009
    Peer Reviewed
     CC BY 4.0
     Accepted on 20 Aug 2008            Submitted on 26 May 2008

    References

    1. Gill , A. E. 1982 . In: Atmosphere-Ocean Dynamics . Academic Press , 662 pp .  

    2. McDonald , A. 2004 . Transparent lateral boundary conditions for FBRLAM. The final shallow water tests and a first multi-level im-plementation . HIRLAM technical report no . 61 , 26 pp .  

    3. McDonald , A. 2005 . Transparent lateral boundary conditions for baro-clinic waves: a study of two elementary systems of equations . Tellus 57A , 171 – 182 .  

    4. McDonald , A. 2006 . Transparent lateral boundary conditions for baro-clinic waves II. Introducing potential voracity waves . Taus 58A , 210 – 220 .  

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