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. 2020 Oct 1;11:4834. doi: 10.1038/s41467-020-18424-6

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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. 6 — Four-day HYSPLIT back trajectories from the altitude of the Puy de Dôme observatory, located at the white dot. Back trajectories were calculated for every hour of sampling. Color indicates the fraction of ambient aerosol activated as depositional ice nucleating particles (INPs). Global Data Assimilation System (GDAS) data at 0.5° × 0.5° spatial resolution were used as meteorological input to calculate the back trajectories.