Abstract
Numerical simulations of atmospheric flows are based on the conservation principles of mass, momentum and energy. These principles — expressed in terms of conserved integrals — are conveniently cast into differential form, the hydrodynamical equations. Depending on the application, these equations are altered to a variety of different forms with different mathematical properties and different requirements on initial and/or boundary conditions in order to represent well-posed problems.
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Eppel, D.P., Callies, U. (1995). Boundary Conditions and Treatment of Topography in Limited-Area Models. In: Gyr, A., Rys, FS. (eds) Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields. ERCOFTAC Series, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8547-7_2
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DOI: https://doi.org/10.1007/978-94-015-8547-7_2
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