Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme

Abstract We implement a Stochastic Multicloud Model (SMCM) in an observation‐informed configuration into the convection scheme of the state‐of‐the‐art GCM ECHAM6.3. The SMCM configuration we use here has been tuned to represent observed tropical convection by associating the occurrence and strength...

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Main Authors: Karsten Peters, Traute Crueger, Christian Jakob, Benjamin Möbis
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2017-03-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Online Access:https://doi.org/10.1002/2016MS000809
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author Karsten Peters
Traute Crueger
Christian Jakob
Benjamin Möbis
author_facet Karsten Peters
Traute Crueger
Christian Jakob
Benjamin Möbis
author_sort Karsten Peters
collection DOAJ
description Abstract We implement a Stochastic Multicloud Model (SMCM) in an observation‐informed configuration into the convection scheme of the state‐of‐the‐art GCM ECHAM6.3. The SMCM configuration we use here has been tuned to represent observed tropical convection by associating the occurrence and strength of deep convection to midtropospheric vertical velocity and relative humidity. We show that compared to the ECHAM6.3 standard model, the SMCM‐modified version shows improved capacity to simulate features of tropical intraseasonal variability, including MJO‐like disturbances, without significantly distorting the mean model climate. This improvement goes in hand with ameliorated coupling of atmospheric convection to tropospheric moisture and spatiotemporal coherence of tropical convection compared to reanalysis and observations. We attribute these effects to (i) improved coupling of triggering and suppression of deep convective events to the model's large‐scale environment and (ii) the observations‐informed closure formulation which leads to an overall reduction of deep convective mass fluxes. Sensitivity tests show that while (ii) improves the convection‐moisture relationship, it is (i) which improves the spatiotemporal coherence of tropical rainfall and is important for MJO simulation. Further, the simulated spatiotemporal coherence of tropical rainfall is an intrinsic property of the convection schemes themselves and not of their parameters. We stress that this study serves as a proof‐of‐concept and motivates further efforts towards building a novel convection parameterization with the SMCM as a central element.
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spelling doaj.art-641d4d2f5bc94cbeb875bb6dcb7a47842023-08-28T13:36:50ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662017-03-019119321910.1002/2016MS000809Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection schemeKarsten Peters0Traute Crueger1Christian Jakob2Benjamin Möbis3ARC Centre of Excellence for Climate System Science, School of Earth, Atmosphere and Environment, Monash UniversityClayton AustraliaMax‐Planck‐Institut für MeteorologieHamburg GermanyARC Centre of Excellence for Climate System Science, School of Earth, Atmosphere and Environment, Monash UniversityClayton AustraliaARC Centre of Excellence for Climate System Science, School of Earth, Atmosphere and Environment, Monash UniversityClayton AustraliaAbstract We implement a Stochastic Multicloud Model (SMCM) in an observation‐informed configuration into the convection scheme of the state‐of‐the‐art GCM ECHAM6.3. The SMCM configuration we use here has been tuned to represent observed tropical convection by associating the occurrence and strength of deep convection to midtropospheric vertical velocity and relative humidity. We show that compared to the ECHAM6.3 standard model, the SMCM‐modified version shows improved capacity to simulate features of tropical intraseasonal variability, including MJO‐like disturbances, without significantly distorting the mean model climate. This improvement goes in hand with ameliorated coupling of atmospheric convection to tropospheric moisture and spatiotemporal coherence of tropical convection compared to reanalysis and observations. We attribute these effects to (i) improved coupling of triggering and suppression of deep convective events to the model's large‐scale environment and (ii) the observations‐informed closure formulation which leads to an overall reduction of deep convective mass fluxes. Sensitivity tests show that while (ii) improves the convection‐moisture relationship, it is (i) which improves the spatiotemporal coherence of tropical rainfall and is important for MJO simulation. Further, the simulated spatiotemporal coherence of tropical rainfall is an intrinsic property of the convection schemes themselves and not of their parameters. We stress that this study serves as a proof‐of‐concept and motivates further efforts towards building a novel convection parameterization with the SMCM as a central element.https://doi.org/10.1002/2016MS000809tropical convectionMadden‐Julian‐Oscillationconvection parametrizationstochastic parametrizationconvective organizationECHAM6.3
spellingShingle Karsten Peters
Traute Crueger
Christian Jakob
Benjamin Möbis
Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
Journal of Advances in Modeling Earth Systems
tropical convection
Madden‐Julian‐Oscillation
convection parametrization
stochastic parametrization
convective organization
ECHAM6.3
title Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
title_full Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
title_fullStr Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
title_full_unstemmed Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
title_short Improved MJO‐simulation in ECHAM6.3 by coupling a Stochastic Multicloud Model to the convection scheme
title_sort improved mjo simulation in echam6 3 by coupling a stochastic multicloud model to the convection scheme
topic tropical convection
Madden‐Julian‐Oscillation
convection parametrization
stochastic parametrization
convective organization
ECHAM6.3
url https://doi.org/10.1002/2016MS000809
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