Articles | Volume 22, issue 5
https://doi.org/10.5194/acp-22-3303-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-22-3303-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Mar 2022
Research article |
| 14 Mar 2022
| 14 Mar 2022
Quantifying albedo susceptibility biases in shallow clouds
National Oceanic and Atmospheric Administration (NOAA), Chemical Sciences Laboratory, Boulder, Colorado, USA
Tom Goren
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Takanobu Yamaguchi
National Oceanic and Atmospheric Administration (NOAA), Chemical Sciences Laboratory, Boulder, Colorado, USA
Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado, USA
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Cited
15 citations as recorded by crossref.
- Daytime variation in the aerosol indirect effect for warm marine boundary layer clouds in the eastern North Atlantic S. Qiu et al. 10.5194/acp-24-2913-2024
- Can general circulation models (GCMs) represent cloud liquid water path adjustments to aerosol–cloud interactions? J. Mülmenstädt et al. 10.5194/acp-24-13633-2024
- Frontiers in Satellite‐Based Estimates of Cloud‐Mediated Aerosol Forcing D. Rosenfeld et al. 10.1029/2022RG000799
- Spatial Aggregation of Satellite Observations Leads to an Overestimation of the Radiative Forcing due to Aerosol‐Cloud Interactions T. Goren et al. 10.1029/2023GL105282
- Machine-Learning Based Analysis of Liquid Water Path Adjustments to Aerosol Perturbations in Marine Boundary Layer Clouds Using Satellite Observations L. Zipfel et al. 10.3390/atmos13040586
- Impacts of Mesoscale Cloud Organization on Aerosol‐Induced Cloud Water Adjustment and Cloud Brightness X. Zhou & G. Feingold 10.1029/2023GL103417
- Addressing the difficulties in quantifying droplet number response to aerosol from satellite observations H. Jia et al. 10.5194/acp-22-7353-2022
- Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
- General circulation models simulate negative liquid water path–droplet number correlations, but anthropogenic aerosols still increase simulated liquid water path J. Mülmenstädt et al. 10.5194/acp-24-7331-2024
- Evaluation of liquid cloud albedo susceptibility in E3SM using coupled eastern North Atlantic surface and satellite retrievals A. Varble et al. 10.5194/acp-23-13523-2023
- Model analysis of biases in the satellite-diagnosed aerosol effect on the cloud liquid water path H. Kokkola et al. 10.5194/acp-25-1533-2025
- Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions J. Zhang & G. Feingold 10.5194/acp-23-1073-2023
- Effects of intermittent aerosol forcing on the stratocumulus-to-cumulus transition P. Prabhakaran et al. 10.5194/acp-24-1919-2024
- Decreasing aerosols increase the European summer diurnal temperature range C. Roesch et al. 10.1038/s41612-025-00922-3
- Global observations of aerosol indirect effects from marine liquid clouds C. Wall et al. 10.5194/acp-23-13125-2023
15 citations as recorded by crossref.
- Daytime variation in the aerosol indirect effect for warm marine boundary layer clouds in the eastern North Atlantic S. Qiu et al. 10.5194/acp-24-2913-2024
- Can general circulation models (GCMs) represent cloud liquid water path adjustments to aerosol–cloud interactions? J. Mülmenstädt et al. 10.5194/acp-24-13633-2024
- Frontiers in Satellite‐Based Estimates of Cloud‐Mediated Aerosol Forcing D. Rosenfeld et al. 10.1029/2022RG000799
- Spatial Aggregation of Satellite Observations Leads to an Overestimation of the Radiative Forcing due to Aerosol‐Cloud Interactions T. Goren et al. 10.1029/2023GL105282
- Machine-Learning Based Analysis of Liquid Water Path Adjustments to Aerosol Perturbations in Marine Boundary Layer Clouds Using Satellite Observations L. Zipfel et al. 10.3390/atmos13040586
- Impacts of Mesoscale Cloud Organization on Aerosol‐Induced Cloud Water Adjustment and Cloud Brightness X. Zhou & G. Feingold 10.1029/2023GL103417
- Addressing the difficulties in quantifying droplet number response to aerosol from satellite observations H. Jia et al. 10.5194/acp-22-7353-2022
- Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
- General circulation models simulate negative liquid water path–droplet number correlations, but anthropogenic aerosols still increase simulated liquid water path J. Mülmenstädt et al. 10.5194/acp-24-7331-2024
- Evaluation of liquid cloud albedo susceptibility in E3SM using coupled eastern North Atlantic surface and satellite retrievals A. Varble et al. 10.5194/acp-23-13523-2023
- Model analysis of biases in the satellite-diagnosed aerosol effect on the cloud liquid water path H. Kokkola et al. 10.5194/acp-25-1533-2025
- Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions J. Zhang & G. Feingold 10.5194/acp-23-1073-2023
- Effects of intermittent aerosol forcing on the stratocumulus-to-cumulus transition P. Prabhakaran et al. 10.5194/acp-24-1919-2024
- Decreasing aerosols increase the European summer diurnal temperature range C. Roesch et al. 10.1038/s41612-025-00922-3
- Global observations of aerosol indirect effects from marine liquid clouds C. Wall et al. 10.5194/acp-23-13125-2023
Latest update: 21 Feb 2025
Short summary
The evaluation of radiative forcing associated with aerosol–cloud interactions remains a significant source of uncertainty in future climate projections. Using high-resolution numerical model output, we mimic typical satellite retrieval methodologies to show that data aggregation can introduce significant error (hundreds of percent) in the cloud albedo susceptibility metric. Spatial aggregation errors tend to be countered by temporal aggregation errors.
The evaluation of radiative forcing associated with aerosol–cloud interactions remains a...
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