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- W2559841856 abstract "The COSMO model uses several diffusion and damping mechanisms to stabilize the dynamical core. One of these is an artificial 4th order hyper-diffusion acting in the horizontal direction. For example in the COSMO-DE (i.e. the COSMO model setup covering mainly Germany together with the most part of the Alpine region with a horizontal grid mesh size of 2.8 km) it is used to smooth the wind velocity components u, v, and w. The strength of the constant hyper-diffusion coefficient lies at about 5% of its possible maximum value (which is defined by the stability constraint). Only in a boundary zone it has a higher value and additionally the other dynamic variables pressure p and temperature T ′ (i.e. their deviations from a reference state) are diffused." @default.
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- W2559841856 date "2012-01-01" @default.
- W2559841856 modified "2023-09-26" @default.
- W2559841856 title "Horizontal nonlinear Smagorinsky diffusion" @default.
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