Most operational numerical weather prediction models update their lateral boundaries via the Davies–Kållberg relaxation scheme. In this paper some potential alternatives that take transparency and well-posedness into consideration are derived and tested for the shallow-water equations. The accuracy of the new boundary strategies is displayed by integrating the shallow-water equations in a nested environment using real meteorological data. In these tests they are seen to be superior to the traditional relaxation boundary strategy.
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A. McDonald (2003) studied this question.
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