Relationship between Low-Level Jet Properties and Turbulence Kinetic Energy in the Nocturnal Stable Boundary Layer

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Exchange Processes in the Atmospheric Boundary Layer Over Mountainous Terrain (2018, background): “Despite being essentially turbulent, katabatic flows or other flows with a low-level wind maximum do not match the standard ABL structure [185,190,191].”
Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “For example, Mahrt et al. (1998) divided turbulence into weakly stable, transition stability, and very stable regimes based on heat fluxes as functions of atmospheric stability. Van de Wiel et al. (2003) divided nocturnal turbulence into the turbulent regime, intermittent regime, and radiative regim”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, methodology): “7, also Banta et al. 2003).”
Doppler Lidar Estimation of Mixing Height Using Turbulence, Shear, and Aerosol Profiles (2009, background): “Stable boundary layer (SBL) conditions may be observed over land, typically at night where, in the absence of surface heating, the BL is in general not well mixed, and proﬁles of u and other quantities are not constant with height (Mahrt 1999; Banta et al. 2002, 2003, 2006; Frehlich et al. 2006).”
Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, methodology): “tower data as described in Banta et al. (2003). The gradients in the bulk Ri calculation”