Title of article :
Parametric vertical coordinate formulation for multiscale, Boussinesq, and non-Boussinesq ocean modeling
Author/Authors :
Song، نويسنده , , Y. Tony and Hou، نويسنده , , Thomas Y.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2006
Pages :
35
From page :
298
To page :
332
Abstract :
Two physical parameters are introduced into the basic ocean equations to generalize numerical ocean models for various vertical coordinate systems and their hybrid features. The two parameters are formulated by combining three techniques: the arbitrary vertical coordinate system of Kasahara [Kasahara, A., 1974. Various vertical coordinate systems used for numerical weather prediction. Mon. Weather Rev. 102, 509–522], the Jacobian pressure gradient formulation of Song [Song, Y.T., 1998. A general pressure gradient formation for ocean models. Part I: Scheme design and diagnostic analysis. Mon. Weather Rev. 126 (12), 3213–3230], and a newly introduced parametric function that permits both Boussinesq (volume-conserving) and non-Boussinesq (mass-conserving) conditions. Based on this new formulation, a generalized modeling approach is proposed. Several representative oceanographic problems with different scales and characteristics––coastal canyon, seamount topography, non-Boussinesq Pacific Ocean with nested eastern Tropics, and a global ocean model––have been used to demonstrate the model’s capabilities for multiscale applications. The inclusion of non-Boussinesq physics in the topography-following ocean model does not incur computational expense, but more faithfully represents satellite-observed ocean-bottom-pressure data. Such a generalized modeling approach is expected to benefit oceanographers in solving multiscale ocean-related problems by using various coordinate systems on the same numerical platform.
Keywords :
Non-Boussinesq , Generalized vertical coordinate system , Multiscale applications
Journal title :
Ocean Modelling
Serial Year :
2006
Journal title :
Ocean Modelling
Record number :
2279896
Link To Document :
بازگشت