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. 2017 Sep 7;7:10783. doi: 10.1038/s41598-017-11285-y

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© The Author(s) 2017

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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CMIP5 winter precipitation changes versus (a) changes in dry day and (b) extreme precipitation day frequency average over the Mediterranean-climate grids (stippled region shown in Fig. 1a) by 2060–2089, relative to the historical period 1960–1989, using the RCP8.5 forcing scenario over the five global Mediterranean-climate regions. Black line indicates the regression line (and correlation, Corr) corresponding to all CMIP5 models. Figure was plotted using NCAR Command Language Version 6.3.0 (NCL; ref. 31).

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