Year: 2004
Type: conference-paper
Abstract: During clear nights we often observe that winds become very weak near the surface. In this situation surfaceand screen level temperatures reach relatively low values. Also, there is little (if any) turbulence activity close to the surface, so that the stable boundary layer (SBL) is ‘detached’ from the surface leading to a so-called decoupled state (Mahrt, 1999). Despite the fact that it is omnipresent, the process of decoupling is poorly understood. At present there is no theory available to predict this phenomenon.
Institution: Wageningen University & Research
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: green
OpenAlex ID: W1600579855
