Articles | Volume 19, issue 16
https://doi.org/10.5194/acp-19-10919-2019
https://doi.org/10.5194/acp-19-10919-2019
Research article
 | 
29 Aug 2019
Research article |  | 29 Aug 2019

Aerosol radiative effects with MACv2

Stefan Kinne

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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.
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