Cloud Controlling Factor Analysis Reveals E3SMv3 Structural Bias and Mean State Controls on Stratocumulus Radiative Sensitivity

Abstract We investigate marine stratocumulus cloud radiative sensitivity to meteorological and aerosol controlling factors in a perturbed parameter ensemble of the Energy Exascale Earth System Model version 3 (E3SMv3). The ensemble perturbs 25 cloud, convection, and aerosol parameters, spanning diverse cloud behavior. The default simulation and many ensemble members capture observed responses to most controlling factors, but not to surface temperature advection, revealing a structural deficiency in processes linking stratocumulus to advection. Many members also overestimate cloud fraction and radiative responses to inversion strength, free‐tropospheric humidity, and sulfate aerosol optical depth. Differences in mean cloud optical depth substantially modify the radiative impact of similar cloud fraction changes, showing that the mean cloud state strongly regulates stratocumulus radiative sensitivity. Across the ensemble, conversion of cloud water to rain controls mean optical depth, identifying autoconversion as a key microphysical control on stratocumulus radiative sensitivity.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-10-18
DOI
https://doi.org/10.1029/2026gl125263
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
0.00

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Cloud Controlling Factor Analysis Reveals E3SMv3 Structural Bias and Mean State Controls on Stratocumulus Radiative Sensitivity

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Cloud Controlling Factor Analysis Reveals E3SMv3 Structural Bias and Mean State Controls on Stratocumulus Radiative Sensitivity

Timothy A. Myers, Jacqueline M Nugent, Daniel Thompson McCoy, Travis Aerenson, Mark D. Zelinka, Hunter Brown
article en

Abstract

Abstract We investigate marine stratocumulus cloud radiative sensitivity to meteorological and aerosol controlling factors in a perturbed parameter ensemble of the Energy Exascale Earth System Model version 3 (E3SMv3). The ensemble perturbs 25 cloud, convection, and aerosol parameters, spanning diverse cloud behavior. The default simulation and many ensemble members capture observed responses to most controlling factors, but not to surface temperature advection, revealing a structural deficiency in processes linking stratocumulus to advection. Many members also overestimate cloud fraction and radiative responses to inversion strength, free‐tropospheric humidity, and sulfate aerosol optical depth. Differences in mean cloud optical depth substantially modify the radiative impact of similar cloud fraction changes, showing that the mean cloud state strongly regulates stratocumulus radiative sensitivity. Across the ensemble, conversion of cloud water to rain controls mean optical depth, identifying autoconversion as a key microphysical control on stratocumulus radiative sensitivity.

Geophysical Research LettersVol. 53(20)
Lawrence Livermore National Laboratory (US), University of Wyoming (US)
U.S. Department of Energy, Office of Science, Biological and Environmental Research, Office of Experimental Program to Stimulate Competitive Research, Lawrence Livermore National Laboratory
Climate action
Openalex Percentile: Top 25%
Atmospheric aerosols and clouds
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