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. 2021 Nov 30;12:6765. doi: 10.1038/s41467-021-27031-y

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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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Fig. 5 — Inter-model dependence of snowfall and rainfall to a, d, g, j surface air temperature, b, e, h, k Open water and c, f, i, l vertically integrated moisture flux (VIMF) changes at the end of the century relative to the start of the century for a–c December–February (DJF), d–f March–May (MAM), g–i June–August (JJA), j–l September–November (SON). Each dot represents a model from CMIP6 and each x represents a model from CMIP5. The stars represent the multi-model means for either CMIP6 and CMIP5 snowfall/rainfall in the same colours as their representative individual members. The line of best fit is calculated using a 1D polynomial.