A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection

Abstract Because of their limited spatial resolution, numerical weather prediction and climate models have to rely on parameterizations to represent atmospheric turbulence and convection. Historically, largely independent approaches have been used to represent boundary layer turbulence and convectio...

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Main Authors: Ignacio Lopez‐Gomez, Yair Cohen, Jia He, Anna Jaruga, Tapio Schneider
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-11-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Online Access:https://doi.org/10.1029/2020MS002161
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spelling doaj-147d48c51bbe4a32926d80952a12f3182021-04-13T10:34:32ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662020-11-011211n/an/a10.1029/2020MS002161A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and ConvectionIgnacio Lopez‐Gomez0Yair Cohen1Jia He2Anna Jaruga3Tapio Schneider4Department of Environmental Science and Engineering California Institute of Technology Pasadena CA USADepartment of Environmental Science and Engineering California Institute of Technology Pasadena CA USADepartment of Environmental Science and Engineering California Institute of Technology Pasadena CA USADepartment of Environmental Science and Engineering California Institute of Technology Pasadena CA USADepartment of Environmental Science and Engineering California Institute of Technology Pasadena CA USAAbstract Because of their limited spatial resolution, numerical weather prediction and climate models have to rely on parameterizations to represent atmospheric turbulence and convection. Historically, largely independent approaches have been used to represent boundary layer turbulence and convection, neglecting important interactions at the subgrid scale. Here we build on an eddy‐diffusivity mass‐flux (EDMF) scheme that represents all subgrid‐scale mixing in a unified manner, partitioning subgrid‐scale fluctuations into contributions from local diffusive mixing and coherent advective structures and allowing them to interact within a single framework. The EDMF scheme requires closures for the interaction between the turbulent environment and the plumes and for local mixing. A second‐order equation for turbulence kinetic energy (TKE) provides one ingredient for the diffusive local mixing closure, leaving a mixing length to be parameterized. Here, we propose a new mixing length formulation, based on constraints derived from the TKE balance. It expresses local mixing in terms of the same physical processes in all regimes of boundary layer flow. The formulation is tested at a range of resolutions and across a wide range of boundary layer regimes, including a stably stratified boundary layer, a stratocumulus‐topped marine boundary layer, and dry convection. Comparison with large eddy simulations (LES) shows that the EDMF scheme with this diffusive mixing parameterization accurately captures the structure of the boundary layer and clouds in all cases considered.https://doi.org/10.1029/2020MS002161boundary layer turbulencesubgrid‐scale parameterizationeddy‐diffusivity mass‐flux scheme
collection DOAJ
language English
format Article
sources DOAJ
author Ignacio Lopez‐Gomez
Yair Cohen
Jia He
Anna Jaruga
Tapio Schneider
spellingShingle Ignacio Lopez‐Gomez
Yair Cohen
Jia He
Anna Jaruga
Tapio Schneider
A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
Journal of Advances in Modeling Earth Systems
boundary layer turbulence
subgrid‐scale parameterization
eddy‐diffusivity mass‐flux scheme
author_facet Ignacio Lopez‐Gomez
Yair Cohen
Jia He
Anna Jaruga
Tapio Schneider
author_sort Ignacio Lopez‐Gomez
title A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
title_short A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
title_full A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
title_fullStr A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
title_full_unstemmed A Generalized Mixing Length Closure for Eddy‐Diffusivity Mass‐Flux Schemes of Turbulence and Convection
title_sort generalized mixing length closure for eddy‐diffusivity mass‐flux schemes of turbulence and convection
publisher American Geophysical Union (AGU)
series Journal of Advances in Modeling Earth Systems
issn 1942-2466
publishDate 2020-11-01
description Abstract Because of their limited spatial resolution, numerical weather prediction and climate models have to rely on parameterizations to represent atmospheric turbulence and convection. Historically, largely independent approaches have been used to represent boundary layer turbulence and convection, neglecting important interactions at the subgrid scale. Here we build on an eddy‐diffusivity mass‐flux (EDMF) scheme that represents all subgrid‐scale mixing in a unified manner, partitioning subgrid‐scale fluctuations into contributions from local diffusive mixing and coherent advective structures and allowing them to interact within a single framework. The EDMF scheme requires closures for the interaction between the turbulent environment and the plumes and for local mixing. A second‐order equation for turbulence kinetic energy (TKE) provides one ingredient for the diffusive local mixing closure, leaving a mixing length to be parameterized. Here, we propose a new mixing length formulation, based on constraints derived from the TKE balance. It expresses local mixing in terms of the same physical processes in all regimes of boundary layer flow. The formulation is tested at a range of resolutions and across a wide range of boundary layer regimes, including a stably stratified boundary layer, a stratocumulus‐topped marine boundary layer, and dry convection. Comparison with large eddy simulations (LES) shows that the EDMF scheme with this diffusive mixing parameterization accurately captures the structure of the boundary layer and clouds in all cases considered.
topic boundary layer turbulence
subgrid‐scale parameterization
eddy‐diffusivity mass‐flux scheme
url https://doi.org/10.1029/2020MS002161
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