Figure 2
From: The energy and mass balance of a continental glacier: Dongkemadi Glacier in central Tibetan Plateau
Variation of daily albedo. Red dots are in situ field observations made at AWS located at 5600 m shown on Fig. 1(c) and black line is simulations. The regression equation between observed and simulated albedo, R2, RMSE and relative error (RE) were presented. RE calculated by (RMSE/mean) *100%. The mean is of observed albedo.
