Articles | Volume 20, issue 6
https://doi.org/10.5194/acp-20-3609-2020
© Author(s) 2020. 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-20-3609-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
26 Mar 2020
Research article | Highlight paper |
| 26 Mar 2020
| 26 Mar 2020
Deconvolution of boundary layer depth and aerosol constraints on cloud water path in subtropical stratocumulus decks
Anna Possner
CORRESPONDING AUTHOR
Institute for Atmospheric and Environmental Sciences, Goethe University, Frankfurt am Main, Germany
Ryan Eastman
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
Frida Bender
Department of Meteorology and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Franziska Glassmeier
Department of Environmental Sciences, Wageningen University, Wageningen, the Netherlands
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34 citations as recorded by crossref.
- Factors affecting precipitation formation and precipitation susceptibility of marine stratocumulus with variable above- and below-cloud aerosol concentrations over the Southeast Atlantic S. Gupta et al. 10.5194/acp-22-2769-2022
- Investigating the sign of stratocumulus adjustments to aerosols in the ICON global storm-resolving model E. Fons et al. 10.5194/acp-24-8653-2024
- Objectively combining climate sensitivity evidence N. Lewis 10.1007/s00382-022-06468-x
- A new method for diagnosing effective radiative forcing from aerosol–cloud interactions in climate models B. Duran et al. 10.5194/acp-25-2123-2025
- Impacts of Mesoscale Cloud Organization on Aerosol‐Induced Cloud Water Adjustment and Cloud Brightness X. Zhou & G. Feingold 10.1029/2023GL103417
- Rapid saturation of cloud water adjustments to shipping emissions P. Manshausen et al. 10.5194/acp-23-12545-2023
- Machine learning reveals climate forcing from aerosols is dominated by increased cloud cover Y. Chen et al. 10.1038/s41561-022-00991-6
- The CLoud–Aerosol–Radiation Interaction and Forcing: Year 2017 (CLARIFY-2017) measurement campaign J. Haywood et al. 10.5194/acp-21-1049-2021
- A survey of radiative and physical properties of North Atlantic mesoscale cloud morphologies from multiple identification methodologies R. Eastman et al. 10.5194/acp-24-6613-2024
- Weak liquid water path response in ship tracks A. Tippett et al. 10.5194/acp-24-13269-2024
- The impact of aerosol on cloud water: a heuristic perspective F. Hoffmann et al. 10.5194/acp-24-13403-2024
- Aerosol effects on clouds are concealed by natural cloud heterogeneity and satellite retrieval errors A. Arola et al. 10.1038/s41467-022-34948-5
- The Radiative and Cloud Responses to Sea Salt Aerosol Engineering in GFDL Models N. Mahfouz et al. 10.1029/2022GL102340
- Cloud water adjustments to aerosol perturbations are buffered by solar heating in non-precipitating marine stratocumuli J. Zhang et al. 10.5194/acp-24-10425-2024
- Environmental and Internal Controls on Lagrangian Transitions from Closed Cell Mesoscale Cellular Convection over Subtropical Oceans R. Eastman et al. 10.1175/JAS-D-20-0277.1
- Assessing the potential efficacy of marine cloud brightening for cooling Earth using a simple heuristic model R. Wood 10.5194/acp-21-14507-2021
- Global observations of aerosol indirect effects from marine liquid clouds C. Wall et al. 10.5194/acp-23-13125-2023
- Observing short-timescale cloud development to constrain aerosol–cloud interactions E. Gryspeerdt et al. 10.5194/acp-22-11727-2022
- Co-variability drives the inverted-V sensitivity between liquid water path and droplet concentrations T. Goren et al. 10.5194/acp-25-3413-2025
- Finding the invisible traces of shipping in marine clouds 10.1038/d41586-022-03026-7
- 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
- Albedo susceptibility of northeastern Pacific stratocumulus: the role of covarying meteorological conditions J. Zhang et al. 10.5194/acp-22-861-2022
- Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions J. Zhang & G. Feingold 10.5194/acp-23-1073-2023
- Wind, Rain, and the Closed to Open Cell Transition in Subtropical Marine Stratocumulus R. Eastman et al. 10.1029/2022JD036795
- Microphysical, macrophysical, and radiative responses of subtropical marine clouds to aerosol injections J. Chun et al. 10.5194/acp-23-1345-2023
- Sampling Bias From Satellite Retrieval Failures of Cloud Properties and Its Implications for Aerosol‐Cloud Interactions G. Choudhury & T. Goren 10.1029/2025GL115429
- 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
- Invisible ship tracks show large cloud sensitivity to aerosol P. Manshausen et al. 10.1038/s41586-022-05122-0
- Opportunistic experiments to constrain aerosol effective radiative forcing M. Christensen et al. 10.5194/acp-22-641-2022
- Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
- Physical science research needed to evaluate the viability and risks of marine cloud brightening G. Feingold et al. 10.1126/sciadv.adi8594
- 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
- Aerosol-cloud-climate cooling overestimated by ship-track data F. Glassmeier et al. 10.1126/science.abd3980
- The Impact of Resolving Subkilometer Processes on Aerosol‐Cloud Interactions of Low‐Level Clouds in Global Model Simulations C. Terai et al. 10.1029/2020MS002274
Latest update: 31 May 2025
Short summary
Cloud water content and the number of droplets inside clouds covary with boundary layer depth. This covariation may amplify the change in water content due to a change in droplet number inferred from long-term observations. Taking this into account shows that the change in water content for increased droplet number in observations and high-resolution simulations agrees in shallow boundary layers. Meanwhile, deep boundary layers are under-sampled in process-scale simulations and observations.
Cloud water content and the number of droplets inside clouds covary with boundary layer depth....
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