TECHNICAL PAPERS
Oct 1, 1984

Discrete Models for Advection

Publication: Journal of Hydraulic Engineering
Volume 110, Issue 10

Abstract

The advection equation is modeled using finite differences in space, with the time derivative left unaltered. The properties of three schemes are discussed in detail, by considering the propagation of a point disturbance and interpreting the results in terms of the propagation characteristics of the Fourier components of the initial disturbance. Central differences produce a forwardpropagating oscillatory response with an envelope that propagates in both directions. A first order upwind differencing scheme produces single humped forward propagating disturbances which are highly damped, while a two point second order scheme produces a forward propagating disturbance which is preceded by an oscillatory precursor. The role of dispersive and diffuse terms is discussed.

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References

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Roberts, K. V., and Weiss, N. A., “Convective Difference Schemes,” Mathematics of Computation, Vol. 20, No. 94, 1966, pp. 272–299.
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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 110Issue 10October 1984
Pages: 1325 - 1339

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Published online: Oct 1, 1984
Published in print: Oct 1984

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Authors

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Giulio Venezian, M. ASCE
Assoc. Prof. of Civ. and Ocean Engrg., Texas A&M Univ., College Station, Tex. 77843

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