Simulating the Nocturnal Boundary Layer During Low-Level Jet Events
نویسنده
چکیده
Simulating the correct evolution of the nocturnal boundary layer (NBL), also often referred to as the stable boundary layer, is a challenge for any numerical model, since the NBL is influenced by a variety of sub-grid scale phenomena (Lenschow et al. 1988). These phenomena include propagating gravity waves, stationary waves that are fixed with respect to the terrain, Kelvin-Helmholtz waves, and various drainage flows (Finnigan et al. 1984; Lenschow et al. 1988).
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