The height of the atmospheric boundary layer (ABL) or the mixing height (MH) is a
fundamental parameter characterising the structure of the lower troposphere. Two basic …

Recent theoretical, experimental, and numerical investigations of stratified-fluid turbulent
mixing are reviewed, and sample results are presented in tables, graphs, and photographs …

The thickness of the entrainment zone at the top of the marine atmosphericboundary layer
(MABL) has been documented by an airborne lidar on twoconsecutive days during a cold-air …

We study the response of the thermosphere and ionosphere to the dissipation of gravity
waves (GWs) excited by a deep convective plume on 1 October 2005 at 52.5° W, 15.0° S …

The atmospheric boundary layer is home to a number of horizontally elongated quasi-two-
dimensional phenomena including cloud streets, roll vortices, thermal waves, and surface …

The planetary boundary layer (PBL) represents the part of the atmosphere that is strongly
influenced by the presence of the underlying surface and mediates the key interactions …

A short period gravity wave train was detected by its effect on three upper atmospheric
nightglow emissions, the OI 557.7 nm and Na 589.2 nm lines and the OH bands between …

The parameterization of penetrative convection and other cases of turbulent entrainment by
the atmospheric boundary layer is reviewed in this paper. The conservation equations for a …

A theory of the fluid entrainment rate into a turbulent, mixed layer across a horizontal density
interfaceis presented. By integrating the turbulent kinetic energy equation over the depth of …

The Laboratoire de Météorologie Dynamique (LMD) Mesoscale Model is a new versatile
simulator of the Martian atmosphere and environment at horizontal scales ranging from …