Identification and elimination of an inflow boundary computational solution in limited area model integrations
Open Access
- 1 December 1986
- journal article
- research article
- Published by Taylor & Francis in Atmosphere-Ocean
- Vol. 24 (4) , 369-385
- https://doi.org/10.1080/07055900.1986.9649258
Abstract
The linearized non‐divergent barotropic vorticity equation in one dimension is used for the study of a problem associated with the specification of lateral boundaries in limited area models. This problem presents itself in the form of a “pillow” that builds up near the inflow boundary of the model. Linear analysis shows that this pillow can easily be eliminated. Linear integrations carried out with a corrector seem to be reasonably accurate. Similar integrations with the linearized shallow water equations in one dimension also produce a pillow and the same corrector gives improved results. Additional runs are performed in order to show that some commonly used nesting strategies do not control this computational problem in a satisfactory manner. It seems that these strategies could be improved with an appropriate corrector.Keywords
This publication has 19 references indexed in Scilit:
- Elimination of the Helmholtz Equation Associated with the Semi-Implicit Scheme in a Grid Point Model of the Shallow Water EquationsMonthly Weather Review, 1986
- Semi-Implicit Semi-Lagrangian Integration Schemes for a Barotropic Finite-Element Regional ModelMonthly Weather Review, 1986
- A Semi-Lagrangian and Semi-Implicit Two Time-Level Integration SchemeMonthly Weather Review, 1986
- Regional Models of the Atmosphere in Middle LatitudesMonthly Weather Review, 1983
- The Excitation of Large-Scale Free Rossby Waves in Numerical Weather PredictionMonthly Weather Review, 1981
- A stable numerical integration scheme for the primitive meteorological equationsAtmosphere-Ocean, 1981
- A Variable-Resolution Finite-Element Technique for Regional Forecasting with the Primitive EquationsMonthly Weather Review, 1978
- A Nested Grid Computation for the Barotropic Free Surface AtmosphereMonthly Weather Review, 1974
- Effects of an Equatorial “Wall” on an Atmospheric ModelMonthly Weather Review, 1973
- Boundary Conditions for Fine-Mesh Limited-Area ForecastsJournal of Applied Meteorology, 1970