For many decades, attempts have been made to find the universal value of the critical bulk Richardson number (Ri Bc ; defined over the entire stable boundary layer). By analyzing an extensive large-eddy simulation database and various published wind-tunnel data, we show that Ri Bc is not a constant, rather it strongly depends on bulk atmospheric stability. A (qualitatively) similar dependency, based on the well-known resistance laws, was reported by Melgarejo and Deardorff (J Atmos Sci 31:1324–1333, 1974) about forty years ago. To the best of our knowledge, this result has largely been ignored. Based on data analysis, we find that the stability-dependent Ri Bc estimates boundary-layer height more accurately than the conventional constant Ri...
The `local scaling' hypothesis, first introduced by Nieuwstadt two decades ago, describes the turbul...
The critical Richardson number, Ric, is used in studies of stably stratified turbulence as a measure...
The flux Richardson number R, (also known as the mixing efficiency) for the stably stratified atmosp...
For many decades, attempts have been made to find the universal value of the critical bulk Richardso...
The bulk Richardson number (Ri Bh ; defined over the entire stable boundary layer) is commonly utili...
Abstract The critical bulk Richardson number (RiBc; defined over the entire stable boundary layer) i...
Experimental data from four field campaigns are used to explore the variability of the bulk Richards...
Stable boundary layer height h is determined from eddy correlation measurements of the vertical prof...
July 1967.Includes bibliographical references.Sponsored by the National Environmental Satellite Cent...
The height (h) of the stable boundary layer (SBL) is of major importance to understand the relevant ...
The performance of diagnostic equations for the stable boundary layer height h is evaluated with fou...
Recently, the equilibrium height of the stable boundary layer received much attention in a series of...
The performance of diagnostic equations for the stable boundary layer height h is evaluated with fou...
Profile measurements of wind and potential temperature from a land site (obtained by a RASS for seve...
In this study, we utilize a novel approach to solve the Ekman equations for eddy-viscosity profiles ...
The `local scaling' hypothesis, first introduced by Nieuwstadt two decades ago, describes the turbul...
The critical Richardson number, Ric, is used in studies of stably stratified turbulence as a measure...
The flux Richardson number R, (also known as the mixing efficiency) for the stably stratified atmosp...
For many decades, attempts have been made to find the universal value of the critical bulk Richardso...
The bulk Richardson number (Ri Bh ; defined over the entire stable boundary layer) is commonly utili...
Abstract The critical bulk Richardson number (RiBc; defined over the entire stable boundary layer) i...
Experimental data from four field campaigns are used to explore the variability of the bulk Richards...
Stable boundary layer height h is determined from eddy correlation measurements of the vertical prof...
July 1967.Includes bibliographical references.Sponsored by the National Environmental Satellite Cent...
The height (h) of the stable boundary layer (SBL) is of major importance to understand the relevant ...
The performance of diagnostic equations for the stable boundary layer height h is evaluated with fou...
Recently, the equilibrium height of the stable boundary layer received much attention in a series of...
The performance of diagnostic equations for the stable boundary layer height h is evaluated with fou...
Profile measurements of wind and potential temperature from a land site (obtained by a RASS for seve...
In this study, we utilize a novel approach to solve the Ekman equations for eddy-viscosity profiles ...
The `local scaling' hypothesis, first introduced by Nieuwstadt two decades ago, describes the turbul...
The critical Richardson number, Ric, is used in studies of stably stratified turbulence as a measure...
The flux Richardson number R, (also known as the mixing efficiency) for the stably stratified atmosp...