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. 2023 Feb 20;16(3):210–216. doi: 10.1038/s41561-023-01126-1

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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 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. 2 — Panels (a–d) as in Fig. 1. Panels (e–h) depict remotely generated T', advective T', adiabatic T' and diabatic T', respectively. The quantities have been computed by integrating Equation (1) along the respective trajectories between t_g and t_e, whereby t_e is the first trajectory time step during which the respective air parcel was located closer than 500 km to its final position x(t_X). Panels (i–l) show locally (that is, less than 500 km distance) generated T', advective T', adiabatic T' and diabatic T', respectively, computed as the difference between the top minus middle row. Panel (m) shows area weighted averages over the heat wave region (black line in panels a–l) for total T' and its contributions (that is, quantities shown in the top row) in red, as well as remotely and locally produced T' and its contributions (that is, quantities in the middle and bottom row, respectively) in blue and brown, respectively.