An updated length‐scale formulation for turbulent mixing in clear and cloudy boundary layers

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The Rossby Centre Regional Climate model RCA3: model description and performance (2011, methodology): “The scheme is updated in RCA3 to include moist processes in the calculation of TKE (Cuijpers and Duynkerke, 1993) and to have a smoother transition between stable and unstable conditions (Lenderink and de Rooy, 2000; Lenderink and Holtslag, 2004).”
The CNRM-CM5.1 global climate model: description and basic evaluation (2013, methodology): “For the mixing length formulation within the boundary layer, the cubic profile used in CNRM-CM3 is replaced by a quadratic profile adapted from Lenderink and Holtslag (2004).”
Tropical and Subtropical Cloud Transitions in Weather and Climate Prediction Models: The GCSS/WGNE Pacific Cross-Section Intercomparison (GPCI) (2011, background): “…developing new parameterizations for clouds and the cloudy boundary layer (e.g., Cuijpers and Bechtold 1995; Lock et al. 2000; Golaz et al. 2002; Teixeira and Hogan 2002; Cheinet and Teixeira 2003; Lenderink and Holtslag 2004; Bretherton et al. 2004; Soares et al. 2004; Bretherton and Park 2009).”
A 140-year simulation of European climate with the new version of the Rossby Centre regional atmospheric climate model (RCA3) (2005, methodology): “The scheme is updated in RCA3 to have a smoother transition between stable and unstable conditions and to be more numerically stable (Lenderink and de Rooy 2000, Lenderink and Holtslag 2004).”