Articles | Volume 21, issue 8
https://doi.org/10.5194/acp-21-6093-2021
© Author(s) 2021. 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-21-6093-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
26 Apr 2021
Research article | Highlight paper |
| 26 Apr 2021
| 26 Apr 2021
Observing the timescales of aerosol–cloud interactions in snapshot satellite images
Edward Gryspeerdt
CORRESPONDING AUTHOR
Space and Atmospheric Physics Group, Imperial College London, London, UK
Tom Goren
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Tristan W. P. Smith
UCL Energy Institute, University College London, London, UK
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Cited
26 citations as recorded by crossref.
- Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
- Liquid Containing Clouds at the North Slope of Alaska Demonstrate Sensitivity to Local Industrial Aerosol Emissions M. Maahn et al. 10.1029/2021GL094307
- Finding the invisible traces of shipping in marine clouds 10.1038/d41586-022-03026-7
- Exploring Satellite-Derived Relationships between Cloud Droplet Number Concentration and Liquid Water Path Using a Large-Domain Large-Eddy Simulation S. Dipu et al. 10.16993/tellusb.27
- Microphysical, macrophysical, and radiative responses of subtropical marine clouds to aerosol injections J. Chun et al. 10.5194/acp-23-1345-2023
- Observing short-timescale cloud development to constrain aerosol–cloud interactions E. Gryspeerdt et al. 10.5194/acp-22-11727-2022
- Weak liquid water path response in ship tracks A. Tippett et al. 10.5194/acp-24-13269-2024
- Opportunistic experiments to constrain aerosol effective radiative forcing M. Christensen et al. 10.5194/acp-22-641-2022
- Invisible ship tracks show large cloud sensitivity to aerosol P. Manshausen et al. 10.1038/s41586-022-05122-0
- A competition–species model for water vapour-aerosol-cloud-rain interactions F. Mascaut et al. 10.1016/j.atmosres.2022.106588
- Assessing the potential efficacy of marine cloud brightening for cooling Earth using a simple heuristic model R. Wood 10.5194/acp-21-14507-2021
- Rapid saturation of cloud water adjustments to shipping emissions P. Manshausen et al. 10.5194/acp-23-12545-2023
- Investigating the development of clouds within marine cold-air outbreaks R. Murray-Watson et al. 10.5194/acp-23-9365-2023
- 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
- 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
- Strong Anthropogenic Cloud Perturbations Can Persist for Multiple Days V. Toll & J. Rahu 10.1029/2022JD038146
- Perspectives on shipping emissions and their impacts on the surface ocean and lower atmosphere: An environmental-social-economic dimension Z. Shi et al. 10.1525/elementa.2023.00052
- Observational evidence of strong forcing from aerosol effect on low cloud coverage T. Yuan et al. 10.1126/sciadv.adh7716
- Diurnal Evolution of Cloud Water Responses to Aerosols J. Rahu et al. 10.1029/2021JD035091
- A Competition–Species Model for Water Vapour-Aerosol-Cloud-Rain Interactions F. Mascaut et al. 10.2139/ssrn.4197632
- Uncertainty in aerosol–cloud radiative forcing is driven by clean conditions E. Gryspeerdt et al. 10.5194/acp-23-4115-2023
- 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
- Albedo susceptibility of northeastern Pacific stratocumulus: the role of covarying meteorological conditions J. Zhang et al. 10.5194/acp-22-861-2022
- Observational evidence and mechanisms of aerosol effects on precipitation C. Zhao et al. 10.1016/j.scib.2024.03.014
- Physical science research needed to evaluate the viability and risks of marine cloud brightening G. Feingold et al. 10.1126/sciadv.adi8594
- A cloud-by-cloud approach for studying aerosol–cloud interaction in satellite observations F. Alexandri et al. 10.5194/amt-17-1739-2024
26 citations as recorded by crossref.
- Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
- Liquid Containing Clouds at the North Slope of Alaska Demonstrate Sensitivity to Local Industrial Aerosol Emissions M. Maahn et al. 10.1029/2021GL094307
- Finding the invisible traces of shipping in marine clouds 10.1038/d41586-022-03026-7
- Exploring Satellite-Derived Relationships between Cloud Droplet Number Concentration and Liquid Water Path Using a Large-Domain Large-Eddy Simulation S. Dipu et al. 10.16993/tellusb.27
- Microphysical, macrophysical, and radiative responses of subtropical marine clouds to aerosol injections J. Chun et al. 10.5194/acp-23-1345-2023
- Observing short-timescale cloud development to constrain aerosol–cloud interactions E. Gryspeerdt et al. 10.5194/acp-22-11727-2022
- Weak liquid water path response in ship tracks A. Tippett et al. 10.5194/acp-24-13269-2024
- Opportunistic experiments to constrain aerosol effective radiative forcing M. Christensen et al. 10.5194/acp-22-641-2022
- Invisible ship tracks show large cloud sensitivity to aerosol P. Manshausen et al. 10.1038/s41586-022-05122-0
- A competition–species model for water vapour-aerosol-cloud-rain interactions F. Mascaut et al. 10.1016/j.atmosres.2022.106588
- Assessing the potential efficacy of marine cloud brightening for cooling Earth using a simple heuristic model R. Wood 10.5194/acp-21-14507-2021
- Rapid saturation of cloud water adjustments to shipping emissions P. Manshausen et al. 10.5194/acp-23-12545-2023
- Investigating the development of clouds within marine cold-air outbreaks R. Murray-Watson et al. 10.5194/acp-23-9365-2023
- 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
- 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
- Strong Anthropogenic Cloud Perturbations Can Persist for Multiple Days V. Toll & J. Rahu 10.1029/2022JD038146
- Perspectives on shipping emissions and their impacts on the surface ocean and lower atmosphere: An environmental-social-economic dimension Z. Shi et al. 10.1525/elementa.2023.00052
- Observational evidence of strong forcing from aerosol effect on low cloud coverage T. Yuan et al. 10.1126/sciadv.adh7716
- Diurnal Evolution of Cloud Water Responses to Aerosols J. Rahu et al. 10.1029/2021JD035091
- A Competition–Species Model for Water Vapour-Aerosol-Cloud-Rain Interactions F. Mascaut et al. 10.2139/ssrn.4197632
- Uncertainty in aerosol–cloud radiative forcing is driven by clean conditions E. Gryspeerdt et al. 10.5194/acp-23-4115-2023
- 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
- Albedo susceptibility of northeastern Pacific stratocumulus: the role of covarying meteorological conditions J. Zhang et al. 10.5194/acp-22-861-2022
- Observational evidence and mechanisms of aerosol effects on precipitation C. Zhao et al. 10.1016/j.scib.2024.03.014
- Physical science research needed to evaluate the viability and risks of marine cloud brightening G. Feingold et al. 10.1126/sciadv.adi8594
- A cloud-by-cloud approach for studying aerosol–cloud interaction in satellite observations F. Alexandri et al. 10.5194/amt-17-1739-2024
Latest update: 08 Mar 2025
Short summary
Cloud responses to aerosol are time-sensitive, but this development is rarely observed. This study uses isolated aerosol perturbations from ships to measure this development and shows that macrophysical (width, cloud fraction, detectability) and microphysical (droplet number) properties of ship tracks vary strongly with time since emission, background cloud and meteorological state. This temporal development should be considered when constraining aerosol–cloud interactions with observations.
Cloud responses to aerosol are time-sensitive, but this development is rarely observed. This...
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