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. 2018 Apr 10;9:1324. doi: 10.1038/s41467-018-03732-9

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© The Author(s) 2018

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 — Identification of excess trends in marine heatwave properties globally. Shown are linear trends in a marine heatwave frequency, b marine heatwave intensity, c marine heatwave duration, d annual mean SST, e annual SST variance and f annual SST skewness from NOAA OI SST over 1982–2016. Hatching in a–c indicates the linear trend is significantly different from what is expected solely due to the rise in the annual mean SST (at the 5% level), based on the statistical climate model. Hatching in d–f indicates the linear trend is significant from zero (p < 0.05)