On open boundary conditions for three dimensional primitive equation ocean circulation models

Stevens, DP (1990) On open boundary conditions for three dimensional primitive equation ocean circulation models. Geophysical & Astrophysical Fluid Dynamics, 51 (1). pp. 103-133. ISSN 0309-1929

[img]
Preview
PDF (DS_1.pdf)
Download (918kB) | Preview

    Abstract

    An open boundary condition is constructed for three dimensional primitive equation ocean circulation models. The boundary condition utilises dominant balances in the governing equations to assist calculations of variables at the boundary. The boundary condition can be used in two forms. Firstly as a passive one in which there is no forcing at the boundary and phenomena generated within the domain of interest can propagate outwards without distorting the interior. Secondly as an active condition where a model is forced by the boundary condition. Three simple idealised tests are performed to verify the open boundary condition, (1) a passive condition to test the outflow of free Kelvin waves, (2) an active condition during the spin up phase of an ocean, (3) finally an example of the use of the condition in a tropical ocean.

    Item Type: Article
    Faculty \ School: Faculty of Science > School of Mathematics
    University of East Anglia > Faculty of Science > Research Groups > Marine and Atmospheric Sciences
    University of East Anglia > Faculty of Science > Research Groups > Meteorology, Oceanography and Climate Dynamics
    ?? RGCOASC ??
    Related URLs:
    Depositing User: David Stevens
    Date Deposited: 01 Dec 2010 11:09
    Last Modified: 25 Jul 2018 08:19
    URI: https://ueaeprints.uea.ac.uk/id/eprint/15856
    DOI: 10.1080/03091929008219853

    Actions (login required)

    View Item