From 1000 ft AGL to 2000 ft AGL, both the length scale and turbulence intensity are determined by linear interpolation between the low altitude value at 1000 ft and the medium / high altitude value at 2000 ft.
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Unlike Huisman et al ., they employed a vertically varying turbulent diffusivity in their model instead of a constant diffusivity, addressing whether the mixed layer is truly " thoroughly mixed " if temperature and density are vertically constant but turbulence intensity is not.
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