“…bioclimatic envelope modelling, bioclimatic variables, climate change, growth forms, land surface temperature, microclimate, mountains, soil temperature, species distribution modelling Moreover, many organisms (particularly small-stature plants, certain types of insects and soil microbes) experience temperatures at ground or sub-surface level, which can differ greatly from ambient air temperatures that are usually measured at 2 m above the soil surface (Aalto et al, 2018;Körner & Hiltbrunner, 2018;Poorter et al, 2016). Especially in high-latitude and high-elevation regions, snow cover, for example, acts as an insulator, thereby strongly decoupling soil and air temperatures (Pauli, Zuckerberg, Whiteman, & Porter, 2013;Poorter et al, 2016;Thompson, Zuckerberg, Porter, & Pauli, 2018), and biophysical processes owing to vegetation cover may also decouple upper atmospheric conditions from boundary layer conditions (Geiger, 1950).…”