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. 2019 Dec 11;9:18813. doi: 10.1038/s41598-019-55303-7

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© The Author(s) 2019

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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Remote control mechanisms for the heating over the western Mediterranean. Schematic illustrating the (a) monsoon–desert teleconnection and (b) northeastward wave energy propagation. Red (blue) shading ellipses indicate the anticyclonic (cyclonic) circulation. Black line boxes show the SASM, EASM, and Atlantic forcings. The Gill-type Rossby wave response to the SASM and EASM forcings is denoted by yellow line in (a) and the northeastward wave route emanated from the Atlantic forcing is shown as blue line in (b). The maps were created using the NCAR Command Language Version 6.4.0 (http://www.ncl.ucar.edu).