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. 2023 Aug 22;14:4643. doi: 10.1038/s41467-023-40112-4

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© The Author(s) 2023

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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 5 — a, d 5-day running average of daily maximum temperature (Tx5day) anomalies of average temperature over (a) Greater Chicago (84–90°W, 38–42°N) and (d) Greater Paris (1–7°E, 47–51°N) for (black line) the period 1950–2021 in ERA5, (light red) three unperturbed events and (dark red) five maximum boosted members for each event. b, e Tx5day anomaly patterns and (c, f) 500hPa geopotential height anomaly during the hottest 5-day period in the maximum boosted model member shown in (a) and (d), respectively (see other events in Fig. S10).