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Calculation of vertical velocity in three-dimensional, shallow water equation, finite element models

✍ Scribed by J. C. Muccino; W. G. Gray; M. G. G. Foreman


Publisher
John Wiley and Sons
Year
1997
Tongue
English
Weight
470 KB
Volume
25
Category
Article
ISSN
0271-2091

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✦ Synopsis


Computation of vertical velocity within the con®nes of a three-dimensional, ®nite element model is a dif®cult but important task. This paper examines four approaches to the solution of the overdetermined system of equations arising when the ®rst-order continuity equation is solved in conjunction with two boundary conditions. The traditional (TRAD) method neglects one boundary condition, solving the continuity equation with the remaining boundary condition. The vertical derivative of continuity (VDC) method involves solution of the second-order equation obtained by differentiation of the continuity equation with respect to the vertical co-ordinate. The least squares (LS) method minimizes the residuals of the continuity equation (in discrete form) and the two boundary conditions. The adjoint (ADJ) method minimizes the residuals of the continuity equation (in continuous form) and the two boundary conditions.

Two domains are considered: a quarter-annular harbour and the southwest coast of Vancouver Island. Results indicate that the highest-quality solution is obtained with both LS and ADJ. Furthermore, ADJ requires less CPU and memory than LS. Therefore the optimal method for computation of vertical velocity in a three-dimensional ®nite element model is the adjoint (ADJ) method.


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