Abstract
Two simple numerical models of the shallow-water equations identical in all respects but for their conservation properties have been tested regarding their internal mixing processes. The experiments show that violation of entropy conservation results in a spurious accumulation of rotational energy in the smaller scales, reflected by an unrealistic increase of entropy, which ultimately produces a finite rate of energy dissipation in the zero viscosity limit, thus violating the well-known dynamics of two-dimensional flow. Further, the experiments show a tendency to equipartition of the kinetic energy of the divergent part of the flow in the inviscid limit, suggesting the possibility of a divergent energy cascade in the physical system, as well as a possible influence of the energy mixing on the process of adjustment toward balanced flow.
Cite
CITATION STYLE
Sadourny, R. (1975). DYNAMICS OF FINITE-DIFFERENCE MODELS OF THE SHALLOW-WATER EQUATIONS. Journal of the Atmospheric Sciences, 32(4), 680–689. https://doi.org/10.1175/1520-0469(1975)032<0680:TDOFDM>2.0.CO;2
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