Atmospheric boundary layers with weak stratification are relatively well described by
similarity theory and numerical models for stationary horizontally homogeneous conditions …

Diurnal mountain wind systems are local thermally driven wind systems that form over
mountainous terrain and are produced by the buoyancy effects associated with the diurnal …

Stable Atmospheric Boundary Layers and Diurnal Cycles: Challenges for Weather and Climate
Models in: Bulletin of the American Meteorological Society Volume 94 Issue 11 (2013) Jump to …

This study compares five planetary boundary-layer (PBL) parametrizations in the Weather
Research and Forecasting (WRF) numerical model for a single day from the Cooperative …

Results are presented from the first intercomparison of large-eddy simulation (LES) models
for the stable boundary layer (SBL), as part of the Global Energy and Water Cycle …

Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during
CASES-99 in: Journal of the Atmospheric Sciences Volume 69 Issue 1 (2012) Jump to Content …

Due to the major role of the sun in heating the earth's surface, the atmospheric planetary
boundary layer over land is inherently marked by a diurnal cycle. The afternoon transition …

Profiles of mean winds and turbulence were measured by the High Resolution Doppler lidar
in the strong-wind stable boundary layer (SBL) with continuous turbulence. The turbulence …

Over the last 100 years, boundary layer meteorology grew from the subject of mostly near-
surface observations to a field encompassing diverse atmospheric boundary layers (ABLs) …

In the present work Blackadar's concept of nocturnal inertial oscillations is extended.
Blackadar's concept describes frictionless inertial oscillations above the nocturnal inversion …