%0 journal article %@ 0894-8755 %A Breil, M., Rechid, D., Davin, E., de Noblet-Ducoudré, N., Katragkou, E., Cardoso, R., Hoffmann, P., Jach, L., Soares, P., Sofiadis, G., Strada, S., Strandberg, G., Tölle, M., Warrach-Sagi, K. %D 2020 %J Journal of Climate %N 21 %P 9159-9179 %R doi:10.1175/JCLI-D-19-0624.1 %T The Opposing Effects of Reforestation and Afforestation on the Diurnal Temperature Cycle at the Surface and in the Lowest Atmospheric Model Level in the European Summer %U https://doi.org/10.1175/JCLI-D-19-0624.1 21 %X First, an in-depth analysis of one ensemble member (CCLM-VEG3D) is carried out, to reveal the complex process chain caused by such land use changes (LUCs). Based on these findings, the whole ensemble is analyzed and principle biophysical effects of re/af-forestation are derived. Results show that the diurnal temperature range is reduced at the surface (top of the vegetation) with re/af-forestation. Most RCMs simulate colder surface temperatures (Tsurf) during the day and warmer Tsurf during the night. Thus, for the first time, the principle temperature interrelations found in observation-based studies in the mid-latitudes could be reproduced within a model intercomparison study. On the contrary, the diurnal temperature range in the lowest atmospheric model level (Tair) is increased with re/af-forestation. This opposing temperature response is mainly caused by the higher surface roughness of forest, enhancing the turbulent heat exchange. Furthermore, these opposing temperature responses demonstrate that the use of the diagnostic 2 m temperature (weighted interpolation between Tsurf and Tair) has a limited potential to assess the effects of re/af-forestation. Thus, studies about the biophysical impacts of LUCs should investigate the whole near-surface temperature profile.