We review developments in the field of boundary-layer flow over complex topography,
focussing on the period from 1970 to the present day. The review follows two parallel …

Monin-Obukhov similarity theory (MOST) forms the basis for parametrizations of turbulent
exchange in virtually all numerical models of atmospheric flows. Yet, its limitations to flat and …

Flows in the atmospheric boundary layer are turbulent, characterized by a large Reynolds
number, the existence of a roughness sublayer and the absence of a well-defined viscous …

While the exchange of mass, momentum, moisture, and energy over horizontally
homogeneous, flat terrain is mostly driven by vertical turbulent mixing, thermally and …

Abstract Model uncertainty is a significant challenge in the wind energy industry and can
lead to mischaracterization of millions of dollars' worth of wind resources. Machine learning …

Based on eddy-covariance measurements over a glacier, we investigate the scalar flux
dissimilarity between sensible heat and water vapor transport in a stably stratified flow. The …

We present the first direct comparison of turbulence conditions measured simultaneously
over exposed ice and a 0.08 m thick supraglacial debris cover on Suldenferner, a small …

Abstract Classic Monin–Obukov similarity scaling states that in a stationary, horizontally
homogeneous flow, in the absence of subsidence, turbulence is dictated by the balance …

A comprehensive analysis of the turbulence structure of relatively deep midlatitude katabatic
flows (with jet maxima between 20 and 50 m) developing over a gentle (1°) mesoscale slope …

Monin–Obukhov similarity theory (MOST) is used in virtually all Earth System Models to
parametrize the near‐surface turbulent exchanges and mean variable profiles. Despite its …