Articles | Volume 23, issue 2
https://doi.org/10.5194/acp-23-1073-2023
© Author(s) 2023. 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-23-1073-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO, USA
Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, USA
Graham Feingold
Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, USA
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14 citations as recorded by crossref.
- Radiative forcing from the 2020 shipping fuel regulation is large but hard to detect J. Zhang et al. 10.1038/s43247-024-01911-9
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- 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
- “Cooling credits” are not a viable climate solution M. Diamond et al. 10.1007/s10584-023-03561-w
- Present-day correlations are insufficient to predict cloud albedo change by anthropogenic aerosols in E3SM v2 N. Mahfouz et al. 10.5194/acp-24-7253-2024
- Global observations of aerosol indirect effects from marine liquid clouds C. Wall et al. 10.5194/acp-23-13125-2023
- Physical science research needed to evaluate the viability and risks of marine cloud brightening G. Feingold et al. 10.1126/sciadv.adi8594
1 citations as recorded by crossref.
Latest update: 31 Mar 2025
Short summary
Using observations from space, we show maps of potential brightness changes in marine warm clouds in response to increases in cloud droplet concentrations. The environmental and aerosol conditions in which these clouds reside covary differently in each ocean basin, leading to distinct evolutions of cloud brightness changes. This work stresses the central importance of the covariability between meteorology and aerosol for scaling up the radiative response of cloud brightness changes.
Using observations from space, we show maps of potential brightness changes in marine warm...
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