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. 2021 Mar 31;592(7852):65–69. doi: 10.1038/s41586-021-03325-5

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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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Extended Data Fig. 3 — a, b, Change in the 95th percentile between the distributions of de-seasoned and de-trended temperature (a) and VPD (b) between CTL and experiment A ( $Δ Q_{95} = Q_{95}^{ExpA} - Q_{95}^{CTL}$ ). The median ΔQ₉₅ of all four models is reported. Suppressing non-seasonal soil moisture variability in experiment A reduces temperature and VPD extremes, demonstrating the role of LAC.