Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability

Abstract We modify the Zhang‐McFarlane (ZM) deep convection scheme in the Community Atmosphere Model version 5 to couple it with a unified parameterization for boundary‐layer turbulence and shallow convection, that is, Cloud Layers Unified by Binormals (CLUBB). By assuming a lognormal distribution o...

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Autores principales: Ben Yang, Minghuai Wang, Guang J. Zhang, Zhun Guo, Anning Huang, Yaocun Zhang, Yun Qian
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Publicado: American Geophysical Union (AGU) 2021
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spelling oai:doaj.org-article:8e329982bddc4c6ba49eb5cb129133542021-11-24T08:11:41ZLinking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability1942-246610.1029/2020MS002357https://doaj.org/article/8e329982bddc4c6ba49eb5cb129133542021-05-01T00:00:00Zhttps://doi.org/10.1029/2020MS002357https://doaj.org/toc/1942-2466Abstract We modify the Zhang‐McFarlane (ZM) deep convection scheme in the Community Atmosphere Model version 5 to couple it with a unified parameterization for boundary‐layer turbulence and shallow convection, that is, Cloud Layers Unified by Binormals (CLUBB). By assuming a lognormal distribution of entrainment rate across the entire moist convective regimes, we link mass fluxes between shallow and deep convection, which are partitioned by the entrainment rate of the shallowest deep convective plume. Hence, a new deep convective closure is established which is coupled to the sub‐grid vertical motion variability in CLUBB. The convection feedback (or memory) effects are also considered to decrease the entrainment spectrum width and enhance the vertical velocity variability that further affect deep convection. Results show that the revised scheme improves the precipitation simulations in terms of the mean state and variability at various timescales, such as the alleviated double‐intertropical convergence zone and more realistic simulations of the seasonal variation of monsoon precipitation over East Asia, Madden‐Julian Oscillation, and precipitation diurnal phase propagations downstream of large terrains. The improvements are still seen in many aspects such as the mean‐state precipitation when turning off the convection feedback impacts in the revised scheme, emphasizing the benefits of using the modified mass‐flux closure. However, the convection feedbacks have considerable effects on the precipitation diurnal cycle simulations over regions with late‐afternoon precipitation peaks. Overall, the revised scheme provides a unified treatment for sub‐grid vertical motions across regimes of boundary‐layer turbulence, shallow convection, and deep convection, leading to better‐simulated precipitation at various timescales.Ben YangMinghuai WangGuang J. ZhangZhun GuoAnning HuangYaocun ZhangYun QianAmerican Geophysical Union (AGU)articleCLUBBdeep and shallow convectionentrainment distributionmass fluxprecipitation simulationZhang‐McFarlane parameterizationPhysical geographyGB3-5030OceanographyGC1-1581ENJournal of Advances in Modeling Earth Systems, Vol 13, Iss 5, Pp n/a-n/a (2021)
institution DOAJ
collection DOAJ
language EN
topic CLUBB
deep and shallow convection
entrainment distribution
mass flux
precipitation simulation
Zhang‐McFarlane parameterization
Physical geography
GB3-5030
Oceanography
GC1-1581
spellingShingle CLUBB
deep and shallow convection
entrainment distribution
mass flux
precipitation simulation
Zhang‐McFarlane parameterization
Physical geography
GB3-5030
Oceanography
GC1-1581
Ben Yang
Minghuai Wang
Guang J. Zhang
Zhun Guo
Anning Huang
Yaocun Zhang
Yun Qian
Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
description Abstract We modify the Zhang‐McFarlane (ZM) deep convection scheme in the Community Atmosphere Model version 5 to couple it with a unified parameterization for boundary‐layer turbulence and shallow convection, that is, Cloud Layers Unified by Binormals (CLUBB). By assuming a lognormal distribution of entrainment rate across the entire moist convective regimes, we link mass fluxes between shallow and deep convection, which are partitioned by the entrainment rate of the shallowest deep convective plume. Hence, a new deep convective closure is established which is coupled to the sub‐grid vertical motion variability in CLUBB. The convection feedback (or memory) effects are also considered to decrease the entrainment spectrum width and enhance the vertical velocity variability that further affect deep convection. Results show that the revised scheme improves the precipitation simulations in terms of the mean state and variability at various timescales, such as the alleviated double‐intertropical convergence zone and more realistic simulations of the seasonal variation of monsoon precipitation over East Asia, Madden‐Julian Oscillation, and precipitation diurnal phase propagations downstream of large terrains. The improvements are still seen in many aspects such as the mean‐state precipitation when turning off the convection feedback impacts in the revised scheme, emphasizing the benefits of using the modified mass‐flux closure. However, the convection feedbacks have considerable effects on the precipitation diurnal cycle simulations over regions with late‐afternoon precipitation peaks. Overall, the revised scheme provides a unified treatment for sub‐grid vertical motions across regimes of boundary‐layer turbulence, shallow convection, and deep convection, leading to better‐simulated precipitation at various timescales.
format article
author Ben Yang
Minghuai Wang
Guang J. Zhang
Zhun Guo
Anning Huang
Yaocun Zhang
Yun Qian
author_facet Ben Yang
Minghuai Wang
Guang J. Zhang
Zhun Guo
Anning Huang
Yaocun Zhang
Yun Qian
author_sort Ben Yang
title Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
title_short Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
title_full Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
title_fullStr Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
title_full_unstemmed Linking Deep and Shallow Convective Mass Fluxes via an Assumed Entrainment Distribution in CAM5‐CLUBB: Parameterization and Simulated Precipitation Variability
title_sort linking deep and shallow convective mass fluxes via an assumed entrainment distribution in cam5‐clubb: parameterization and simulated precipitation variability
publisher American Geophysical Union (AGU)
publishDate 2021
url https://doaj.org/article/8e329982bddc4c6ba49eb5cb12913354
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