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Assessment of adaptive and heuristic time stepping for variably saturated flow
Authors:C M F D'Haese  M Putti  C Paniconi  N E C Verhoest
Institution:1. Laboratory of Hydrology and Water Management (LHWM), Ghent University, Coupure links 653, B‐9000 Ghent, Belgium;2. Dipartimento di Metodi e Modelli Matematici per le Scienze Applicate (DMMMSA), University of Padova, Via Belzoni 7, I‐35131 Padova, Italy;3. Institut National de la Recherche Scientifique ‐ Centre Eau, Terre et Environnement (INRS‐ETE), Université du Québec, 490 de la Couronne, Québec, Canada G1K 9A9
Abstract:The performance of improved initial estimates and ‘heuristic’ and ‘adaptive’ techniques for time step control in the iterative solution of Richards equation is evaluated. The so‐called heuristic technique uses the convergence behaviour of the iterative scheme to estimate the next time step whereas the adaptive technique regulates the time step on the basis of an approximation of the local time truncation error. The sample problems used to assess these various schemes are characterized by nonuniform (in time) boundary conditions, sharp gradients in the infiltration fronts, and discontinuous derivatives in the soil hydraulic properties. It is found that higher order initial solution estimates improve the convergence of the iterative scheme for both the heuristic and adaptive techniques, with greater overall performance gains for the heuristic scheme, as could be expected. It is also found that the heuristic technique outperforms the adaptive method under strongly nonlinear conditions. Previously reported observations suggesting that adaptive techniques perform best when accuracy requirements on the numerical solution are very stringent are confirmed. Overall both heuristic and adaptive techniques have their limitations, and a more general or mixed time stepping strategy combining truncation error and convergence criteria is recommended for complex problems. Copyright © 2006 John Wiley & Sons, Ltd.
Keywords:numerical modelling  subsurface hydrology  unsaturated zone  Richards' equation  nonlinear processes  adaptive time stepping  time truncation error
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