Fig. 3: Processes contributing to Tibetan Plateau warming in boreal summer.
From: Asynchronicity of deglacial permafrost thawing controlled by millennial-scale climate variability
a–h Decomposition of a surface temperature difference between the North Atlantic hosing experiment (GFWF) and the equilibrated glacial control simulation (GCTL) into seven individual processes due to b surface albedo, c water vapor, d cloud, e surface sensible heat flux, f surface latent heat flux, g atmospheric heat transport, and h surface dynamics (i.e., land and oceanic surface energy transport). The Tibetan Plateau caves and the Siberian Caves are marked by red stars and blue circles, respectively. (Map produced by NCL Version 6.6.2, https://doi.org/10.5065/D6WD3XH5)87.
