A two‐fluid single‐column model of the dry, shear‐free, convective boundary layer. (18th March 2019)

• Record Type: Journal Article
• Authors: Thuburn, John; Efstathiou, Georgios A.; Beare, Robert J.
• Is Part Of: Quarterly journal of the Royal Meteorological Society. Volume 145:Number 721(2019)
• Page Start: 1535
• Page End: 1550
• Publication Date: 2019-03-18
• Subjects: EDMF -- Kelvin–Helmholtz -- multi‐fluid -- parametrization -- updraught; Meteorology -- Periodicals; 551.5
• DOI: 10.1002/qj.3510
• Languages: English
• ISSNs: 0035-9009

Abstract

Abstract : A single‐column model of the dry, shear‐free, convective boundary layer is presented in which non‐local transports by coherent structures such as thermals are represented by the partitioning of the fluid into two components, updraught and environment, each with a full set of prognostic dynamical equations. Local eddy diffusive transport and entrainment and detrainment are represented by parametrizations similar to those used in eddy diffusivity mass flux schemes. The inclusion of vertical diffusion of the vertical velocity is shown to be important for suppressing an instability inherent in the governing equations. A semi‐implicit semi‐Lagrangian numerical solution method is presented and shown to be stable for large acoustic and diffusive Courant numbers, though it becomes unstable for large advective Courant numbers. The solutions are able to capture key physical features of the dry convective boundary layer. Some of the numerical challenges posed by sharp features in the solution are discussed, and areas where the model could be improved are highlighted. Abstract : A novel single‐column model of the dry convective boundary layer is presented in which non‐local transports by coherent structures such as thermals are represented by partitioning the fluid into two components, updraught and environment, each with a full set of prognostic dynamical equations. The model captures key features such as counter‐gradient potential temperature transport and a boundary‐layer‐top entrainment flux.