Fig. 2
From: Does elevation-dependent warming hold true above 5000 m elevation? Lessons from the Tibetan Plateau
a Histogram of elevation in 500 m interval and hypsometric curve for the Tibetan Plateau (over 2000 m) based on the 0.5-degree resolution elevation and observation stations. Solid lines represent the number and the percentage of cells/stations below a given threshold. b Topography of 0.5-degree resolution grid cells over the TP (shades) and locations of stations and grid cells with elevations at 2000–3000 m: stations in dots and grid cells in pentagons
