Fig. 6: Schematic figure of possible mechanisms responsible for robust elevation-dependent warming over the Tibetan Plateau at GW1.5 and GW2.
From: Recent frontiers of climate changes in East Asia at global warming of 1.5°C and 2°C
SR and LR indicate shortwave radiation and longwave radiation fluxes, respectively. It is adapted from Fig. 10 of You et al. (2019).
