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. 2020 Oct 12;7:335. doi: 10.1038/s41597-020-00663-3

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© The Author(s) 2020

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. 3 — Maps of trend, variability, and signal to noise ratio (SNR) for temperature during periods of extreme global warming in the ocean and on land (≥90^th percentile from pre-industrial conditions). Maps of centennial trend (a), inter-annual variability (b), and SNR (c). Rows represent rapid global warming events at different time periods/climate scenarios. Past = Bølling–Allerød (14.7-14.2k B.P.⁶⁹); Historical = 1850 C.E.–2005 C.E.; RCP 2.6 & 4.5 = Representative Concentration Pathways 2.6 and 4.5 for 2001 C.E.–2100 C.E. Maps of the past and historical conditions are mean estimates for overlapping century windows during the relevant periods.