Articles | Volume 19, issue 16
https://doi.org/10.5194/acp-19-10919-2019
© Author(s) 2019. 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-19-10919-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Aerosol radiative effects with MACv2
Stefan Kinne
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Hamburg, Germany
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Latest update: 16 Aug 2024
Short summary
Global distributions of aerosol radiative effects are calculated using aerosol properties of the MACv2 climatology and a satellite-retrieval-based relationship for the first indirect effect. Present-day climate cooling by anthropogenic aerosol is likely within a −0.7 to −1.6 W m−2 range – with a best estimate at −1.0 W m−2. Only about 1/3 of this TOA cooling is contributed by direct effects, which are more variable (even in sign) and stronger near pollution source regions than indirect effects.
Global distributions of aerosol radiative effects are calculated using aerosol properties of the...
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