Momentum balance of katabatic flow on steep slopes covered with short vegetation

Katabatic flows over alpine mountainous terrain differ from their forested or bare slope counterparts due to the presence of well-ventilated, short vegetation. The impact of a grass canopy and larger-scale pressure perturbations on the one-dimensional mean momentum balance is explored via theory and field measurements. The model presented here reproduces the measured velocity jet shape and turbulent flux gradients. These two features imply that even when Monin-Obuhkov similarity theory breaks down, its use for a stability adjusted mixing length remains effective to first order. Results reveal that outer layer pressure effects can be significant under low-speed wind conditions at the top of the thin katabatic layer when larger variations in the wind direction are observed. An analytical expression to estimate the jet height, which can be utilized in large-scale weather prediction models, shows the importance of including canopy effects for the thin katabatic flow region above the vegetation. Key Points New measurements and a model reveal unmeasured physics of katabatic flow Outer layer pressure effects are significant in low-speed highly variable wind Explicit treatment of the canopy is important in thin steep-slope katabatic jets ©2014. American Geophysical Union. All Rights Reserved.

Duke Scholars

Author Gabriel G. Katul Civil and Environmental Engineering