Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach

The modular structure of the boundary layer and convection parameterizations in atmospheric models have long been affecting the numerical representation of subgrid-scale motions and their mutual interactions. A promising alternative, the eddy-diffusivity/mass-flux approach (EDMF), has the potential...

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Main Authors: Marcin J. Kurowski, Heidar Th. Thrastarson, Kay Suselj, Joao Teixeira
Format: Article
Language:English
Published: MDPI AG 2019-08-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/9/484
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author Marcin J. Kurowski
Heidar Th. Thrastarson
Kay Suselj
Joao Teixeira
author_facet Marcin J. Kurowski
Heidar Th. Thrastarson
Kay Suselj
Joao Teixeira
author_sort Marcin J. Kurowski
collection DOAJ
description The modular structure of the boundary layer and convection parameterizations in atmospheric models have long been affecting the numerical representation of subgrid-scale motions and their mutual interactions. A promising alternative, the eddy-diffusivity/mass-flux approach (EDMF), has the potential for unifying the existing formulations into a consistent scheme and improving some of the long-standing issues. This study documents a step towards developing such a unified approach by implementing a stochastic multi-plume EDMF scheme into the Community Atmosphere Model (Version 5.0). Its performance in single-column mode is evaluated against the control parameterization and large-eddy simulation (LES) for two benchmark cases: marine and continental shallow convection. Overall, the results for the two parameterizations agree well with each other and with LES in terms of mean profiles of moist conserved variables and their vertical fluxes, as well as the updraft properties. However, systematic differences between the two schemes, especially for transient continental convection, are also documented. Using EDMF helps improve some of the parameterized features of shallow convection. In particular, for the highest tested vertical resolution, the EDMF cloud base and top heights and the vertical fluxes of energy and water are remarkably close to LES.
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spelling doaj.art-54f11ef13fb84ba7974d2af07ad93edf2022-12-21T18:41:41ZengMDPI AGAtmosphere2073-44332019-08-0110948410.3390/atmos10090484atmos10090484Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux ApproachMarcin J. Kurowski0Heidar Th. Thrastarson1Kay Suselj2Joao Teixeira3Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive M/S: 233-300, Pasadena, CA 91109, USAJet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive M/S: 233-300, Pasadena, CA 91109, USAJet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive M/S: 233-300, Pasadena, CA 91109, USAJet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive M/S: 233-300, Pasadena, CA 91109, USAThe modular structure of the boundary layer and convection parameterizations in atmospheric models have long been affecting the numerical representation of subgrid-scale motions and their mutual interactions. A promising alternative, the eddy-diffusivity/mass-flux approach (EDMF), has the potential for unifying the existing formulations into a consistent scheme and improving some of the long-standing issues. This study documents a step towards developing such a unified approach by implementing a stochastic multi-plume EDMF scheme into the Community Atmosphere Model (Version 5.0). Its performance in single-column mode is evaluated against the control parameterization and large-eddy simulation (LES) for two benchmark cases: marine and continental shallow convection. Overall, the results for the two parameterizations agree well with each other and with LES in terms of mean profiles of moist conserved variables and their vertical fluxes, as well as the updraft properties. However, systematic differences between the two schemes, especially for transient continental convection, are also documented. Using EDMF helps improve some of the parameterized features of shallow convection. In particular, for the highest tested vertical resolution, the EDMF cloud base and top heights and the vertical fluxes of energy and water are remarkably close to LES.https://www.mdpi.com/2073-4433/10/9/484planetary boundary layershallow convectioncoarse-resolution atmospheric modelseddy-diffusivity/mass-flux approachunified convection parameterizations
spellingShingle Marcin J. Kurowski
Heidar Th. Thrastarson
Kay Suselj
Joao Teixeira
Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
Atmosphere
planetary boundary layer
shallow convection
coarse-resolution atmospheric models
eddy-diffusivity/mass-flux approach
unified convection parameterizations
title Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
title_full Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
title_fullStr Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
title_full_unstemmed Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
title_short Towards Unifying the Planetary Boundary Layer and Shallow Convection in CAM5 with the Eddy-Diffusivity/Mass-Flux Approach
title_sort towards unifying the planetary boundary layer and shallow convection in cam5 with the eddy diffusivity mass flux approach
topic planetary boundary layer
shallow convection
coarse-resolution atmospheric models
eddy-diffusivity/mass-flux approach
unified convection parameterizations
url https://www.mdpi.com/2073-4433/10/9/484
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