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Large‐Eddy Simulation of a katabatic jet along a convexly curved slope: 2. Evidence of Görtler vortices
Author(s) -
Brun Christophe
Publication year - 2017
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2016jd025416
Subject(s) - katabatic wind , turbulence , jet (fluid) , vortex , large eddy simulation , boundary layer , orography , geology , mechanics , detached eddy simulation , geometry , flow (mathematics) , physics , meteorology , reynolds averaged navier–stokes equations , mathematics , precipitation
This paper is the second part of a study of katabatic jet along a convexly curved slope with a maximum angle of about 35.5°. Large‐Eddy Simulation (LES) is performed with a special focus on the outer‐layer shear of the katabatic jet. In the first part, a basic statistical quantitative analysis of the flow was performed. Here a qualitative and quantitative description of vortical structures is used to gain insight in the present 3‐D turbulent flow. It is shown that Görtler vortices oriented in the streamwise downslope direction develop in the shear layer. They spread with a specific mushroom shape in the vertical direction up to about 100 m height. They play a main role with respect to local turbulent mixing in the ground surface boundary layer. The present curved slope configuration constitutes a realistic model for alpine orography. This paper provides a procedure based on local turbulence anisotropy to track Görtler vortices for in situ measurements, which has never been proposed in the literature.