“…This may be explained by the assumption that climate sensitivity of plants is greater towards both the dry and cold ends of ecological gradients because climate stress there becomes increasingly limiting to the point that potential distribution limits are expressed due to total growth cessation (Brown, Stevens, & Kaufman, ; Fritts, ; Normand et al., ). Based on multisite dendroecological studies, drought has emerged as a general driver of growth for beech across Europe (Dittmar, Zech, & Elling, ; Hacket‐Pain, Cavin, Friend, & Jump, ; Hacket‐Pain, Lageard, & Thomas, ; Jump, Hunt, & Peñuelas, ; Knutzen, Dulamsuren, Meier, & Leuschner, ; Lebourgeois, Bréda, Ulrich, & Granier, ), though drought sensitivity has been indicated to increase towards drier sites along continental or elevational gradients (Jump et al., ; Roibu, Popa, Kirchhefer, & Palaghianu, ; Scharnweber et al., ). However, this observation might be biased due to research focusing on the southern to south‐eastern dry parts of the distribution range (Dittmar et al., ; Roibu et al., ), on countries at the southern dry distribution margin (Jump et al., ; Lebourgeois et al., ), and on gradients from the central distribution range to its southern edge (Hacket‐Pain et al., ).…”