A DEFECT-DEFERRED CORRECTION METHOD FOR FLUID-FLUID INTERACTION

被引:40
作者
Aggul, Mustafa [1 ,2 ]
Connors, Jeffrey M. [3 ]
Erkmen, Dilek [1 ,4 ]
Labovsky, Alexander E. [1 ]
机构
[1] Michigan Technol Univ, Dept Math Sci, Houghton, MI 49931 USA
[2] Mus Alparslan Univ, Dept Math Sci, TR-49250 Mus, Turkey
[3] Univ Connecticut, Dept Math, Storrs, CT 06269 USA
[4] Agri Ibrah Cecen Univ, Dept Math Sci, TR-04100 Agri, Turkey
关键词
defect-deferred correction; high accuracy; fluid-fluid interaction; ocean-atmosphere coupling; implicit-explicit method; AIR-SEA INTERACTION; OCEAN MODEL; SIMULATION;
D O I
10.1137/17M1148219
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
A method is proposed to improve two aspects of numerical simulations for a model of two fluids coupled across a flat interface. This problem is motivated by atmosphere-ocean interaction. A deferred correction approach lifts the numerical order of accuracy formally from first order (very common in applications) to second order in terms of the time interval of communication between the fluid code components. This is accomplished in a two-step predictor-corrector-type method. In the second step, a further defect correction is included as well. The "defect" represents artificial diffusion used in the fluid solvers, which is often included to control numerical noise or to model subscale mixing processes. The addition of the defect correction adds only marginally to the expense, but in exchange may provide a significant reduction of overdiffusive effects. The defect and deferred correction approaches are combined into a so-called defect-deferred correction (DDC) method. A full DDC algorithm is studied using finite elements in space, including an analysis of the stability and convergence. The method is unconditionally stable and optimally convergent, and also enforces a formal reduction in artificial diffusion effects. A computational example using a known (manufactured) solution illustrates the theoretical predictions. We observe a computational benefit in this example even for coarse time steps and over a wide range of artificial viscosity values. Some discussion is provided regarding the possibility to generalize the approach for application codes. Briefly, legacy atmosphere and ocean codes may be used as-is over a coupling time interval for a predictor computation. The corrector step would then potentially be implemented as a straightforward modification of the predictor step that leverages the existing code structure.
引用
收藏
页码:2484 / 2512
页数:29
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