TECHNICAL PAPERS
Sep 1, 1988

Finite Element Characteristic Advection Model

Publication: Journal of Hydraulic Engineering
Volume 114, Issue 9

Abstract

For advection‐dominated transport processes, the traditional numerical techniques for solving the advection‐diffusion equation fail because of numerical oscillations. Fractional step solutions, in which the advection and diffusion processes are treated in separate steps, have been proposed as one way of overcoming this problem. Here a solution to the advection step based on the method of characteristics on a fixed grid is used. Interpolation is achieved with the finite element technique. Linear and quadratic elements are evaluated in terms of artificial diffusion, phase, and other errors. It was found that linear interpolation creates too much numerical diffusion, while the quadratic scheme is reasonably accurate, but under certain conditions generates spurious extrema. A method retaining the accuracy of the quadratic interpolation and eliminating its shortcoming is suggested. Boundary conditions and source loadings are considered in detail. An application of the model to salinity distribution resulting from canal discharges in Biscayne Bay is described.

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 114Issue 9September 1988
Pages: 1098 - 1114

History

Published online: Sep 1, 1988
Published in print: Sep 1988

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Authors

Affiliations

John D. Wang, Member, ASCE
Prof., RSMAS, Univ. of Miami, Appl. Marine Physics, 4600 Rickenbacker Causeway, Miami, FL 33149
Stephen V. Cofer‐Shabica
Oceanographer, Nat. Park Service, Cooperative Park Study Unit, Inst., of Ecology, Univ. of Georgia, Athens, GA 30602; formerly, Oceanographer, Biscayne Nat. Park, Homestead, FL 33030
Joycelyn Chin Fatt, Associate Member ASCE
Tech. Program Coordinator, South Florida Water Mgmt. Dist., P.O. Box V, West Palm Beach, FL 33402; formerly, Grad. Student, RSMAS, Univ. of Miami

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