Fig. 4
From: Does elevation-dependent warming hold true above 5000 m elevation? Lessons from the Tibetan Plateau
Distribution of WRF simulated a surface air temperature linear trends, b SWE linear trends, c surface latent heat flux changes, d sensible heat flux changes, and e surface net radiation changes. (f-–j) Are the same as (a–e) but for ERA-Interim in 1983–2011. Grid cells for elevations above 5000 m are labeled as pluses. Kalakunlun (NW) and Tanggula (SE) ranges are marked as black
