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. 2021 Dec 8;12:7119. doi: 10.1038/s41467-021-27445-8

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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. 3 — The MNTH distribution for 2000 reflects the range of possible modeled MNTH, including tidal variability and does not include sea-level rise. MNTH distributions for 2050, 2070, and 2100 are calculated by combining the same range of modeled MNTH with a low-emissions (RCP2.6) sea-level projections with the K14⁶⁸ Antarctic Ice Sheet (AIS) contribution and DP16⁶⁰ AIS contribution. b high-emissions (RCP8.5) sea-level projections with K14⁶⁸ AIS contribution and DP16⁶⁰ AIS contribution.