Many climate subsystems are thought to be susceptible to tipping—and some might be close
to a tipping point. The general belief and intuition, based on simple conceptual models of …

Long-term, continuous in situ observations of the near-surface atmospheric boundary layer
are critical for many weather and climate applications. Although there is a proliferation of …

The mean wind speed at which the stable boundary layer (SBL) experiences a turbulence
regime transition (V r) depends on other flow characteristics, such as its thermal stability …

Numerical weather prediction and climate models encounter challenges in accurately
representing flow regimes in the stably stratified atmospheric boundary layer and the …

Stable boundary layers are still a relatively problematic component of atmospheric
modeling, despite their frequent occurrence. While general agreement exists that Monin …

The atmospheric stable boundary layer (SBL) is observed to display multiple regimes of
stratification, flow, and turbulence. Transitions between weakly stable regimes of sustained …

The dependence of fluxes on the wind speed near the surface of the stable nocturnal
boundary layer has been organized in terms of a threshold wind speed. When the wind …

Turbulence in the nocturnal boundary layer (NBL) is still not well characterized, especially
over complex underlying surfaces. Herein, gradient tower data and eddy covariance data …

A statistical indicator for dynamic stability, known as the Υ indicator, is used to gauge the
stability and, hence, detect approaching tipping points of simulation data from a reduced five …

Numerical weather prediction and climate models encounter challenges in accurately
representing flow regimes in the stably stratified atmospheric boundary layer and the …