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. 2022 Nov 23;13:7202. doi: 10.1038/s41467-022-34944-9

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© The Author(s) 2022

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. 4 — Difference in (a) zonal mean SOA increase and (b) accumulation mode SOA column increase between CRI-Strat 2 (CS2_Δ) and Strat-Trop (ST_Δ). Radiative forcing from the change in the aerosol direct radiative effect (IRF_DRE) for (c) ST_Δ and (d) CS2_Δ. Percentage change in vertically averaged cloud droplet number concentration (CDNC) concentration (e) ST_Δ and (f) CS2_Δ and radiative forcing due to change in CDNC (ERF_CDNC) for (g) ST_∆ and (h) CS2_∆ calculated using the offline approach of³⁴ (Methods). Values in titles are global mean forcing (c, d) and CDNC change (e, f). Non-hatched regions in (c–h) show areas where the change is statistically significant (95% confidence).