Estimation of the height of intense turbulent heat exchange layer in the stably stratified atmospheric boundary layer

摘要

The relation of the height of intense turbulent heat exchange layer in the atmospheric boundary layer to the air temperature gradients, wind velocity, and turbulent heat flux in the atmospheric surface layer has been analyzed. Experimental data obtained with the sodar, temperature profilometer, and ultrasonic meteostation have been used for the analysis. The emphasis is on the conditions with stable stratification (temperature inversion) in the boundary layer in winter.