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.
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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- Aerosol effects on clouds are concealed by natural cloud heterogeneity and satellite retrieval errors A. Arola et al. 10.1038/s41467-022-34948-5
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- 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
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- Wind, Rain, and the Closed to Open Cell Transition in Subtropical Marine Stratocumulus R. Eastman et al. 10.1029/2022JD036795
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- Opportunistic experiments to constrain aerosol effective radiative forcing M. Christensen et al. 10.5194/acp-22-641-2022
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- 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: 20 Nov 2024
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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