Fig. 3
From: Does elevation-dependent warming hold true above 5000 m elevation? Lessons from the Tibetan Plateau
Mean (lines) and median (stars) linear trends of simulated anneal mean a vertical averaged tropospheric water vapor, b vertical averaged tropospheric diabatic heating releasing, c snow-water equivalent, d snowfall, e precipitation, and f albedo in April vs. elevation bands with 500 m width for ERA-Interim and WRF simulation in 1983–2011. Spread is indicated with 25 and 75% percentiles in shades
