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. 2021 Jan 12;12:277. doi: 10.1038/s41467-020-20482-9

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© The Author(s) 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 5 — a default CAM5.4 biomass burning (BB) radiative effect due to aerosol-radiation interactions (RE_ari), b the difference in RE_ari due to changes in BB black carbon refractive index (CAM_ BCRI – CAM5.4), c the difference in RE_ari due to increasing BB aerosol size (CAM_Dg160 – CAM5.4), d the difference in RE_ari due to treating fresh BB aerosol as externally mixed (CAM_EMIX – CAM5.4), e the difference in RE_ari due to all of the previous changes (CAM_ALL – CAM5.4), and f the RE_ari of BB with all of the previous changes (CAM_ALL). Hatching indicates regions where the change over the ensemble years is significant to the 0.05 level. Note difference in color bars.