作者: P. Orlandi , G. F. Carnevale
DOI: 10.1007/978-94-015-9285-7_3
关键词:
摘要: In order to capture the large range of scales that are important in dynamics geophysical systems, it is necessary turn large-eddy simulations (LES). There various candidates for subgrid-scale modeling used LES. A preliminary examination role temporal and spatial variability eddy viscosity diffusivity such models presented here. specific comparison between Smagorinsky model a simplified dynamic (SDM) allows only variation made an application oceanic fine structure.