Fig. 4: Sensitivity of temperature offset to canopy cover loss in montane forests in Africa.
From: Deforestation reduces microclimate buffering of African montane forests

Panel (a–c) show the sensitivity of the change in maximum air temperature offset between microclimate air temperature (Tmicro) and mesoclimate air temperature (Tmeso) (Toffset = Tmicro – Tmeso; ΔToffset = Toffset(2022) – Toffset(2003)) to canopy cover loss from 2003 to 2022 in Mount Bale (Ethiopia), Mount Kilimanjaro (Tanzania), and the Taita Hills (Kenya) respectively. A cubic spline regression is fitted (red lines) with a 95% confidence interval (blue shading) based on generalized additive modeling.