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. 2020 Aug 25;10:14153. doi: 10.1038/s41598-020-71055-1

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© The Author(s) 2020

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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Pronounced mean diurnal and seasonal cycles of temperature changes caused by an increase in BTF reveal a cooling effect in summer. For every month denoted as J (January), … , D (December) on the x-axis the mean diurnal cycle of the LST change induced by an 80% increase of the broad-leaved tree fraction is shown. For SEVIRI hourly mean values are available (i.e. 24 values for each month). For MODIS, observations are available at four different time steps per day which are approximately: 01:30, 10:30, 13:30 and 22:30. Confidence intervals for SEVIRI are shown in grey. Confidence intervals for the MODIS observations are denoted as black lines through the colored dots.