In very stable boundary layers (VSBL), a “cocktail” of submeso motions routinely result in
elevated mean wind speed maxima above the ground, acting as a new source of turbulence …

The aerodynamic roughness length (z0) is an essential parameter in surface energy
balance studies, but few literature values exist for debris‐covered glaciers. We use …

Under the background of global climate change, typhoons have been attracting increasing
attention due to their extraordinary destructive potential and great impact on the coastal …

Multiple Regimes of Wind, Stratification, and Turbulence in the Stable Boundary Layer in:
Journal of the Atmospheric Sciences Volume 72 Issue 8 (2015) Jump to Content Jump to Main …

Turbulence structures and exchange of momentum and heat in the nocturnal stable
boundary layer (SBL) show distinct features under different stability conditions prompting …

Heavy haze pollution events are closely related to the turbulent structure of the stable
boundary layer (SBL). SBL can be divided into two regimes, weak (coupled) and strong …

The paper presents the results of probing the stable atmospheric boundary layer in the
coastal zone of Lake Baikal with a coherent Doppler wind lidar and a microwave …

In this study, observational data from the Semi-Arid Climate and Environment Observatory of
Lanzhou University (SACOL) in July 2008 were used to analyze the characteristics of the …

A gust front is generated when the cold downdraft from a thunderstorm reaches the surface,
causing the warm air mass at the surface to lift. This is always accompanied by gusts and …

The presence of waves is proven to be ubiquitous within nocturnal stable boundary layers
over complex terrain, where turbulence is in a continuous, although weak, state of activity …