Figure 3
From: Irrigation and warming drive the decreases in surface albedo over High Mountain Asia
Dominant drivers of the surface albedo changes. (a) map of the dominant drivers of the surface albedo changes (i.e., the variable with the highest unique information). (b–m) Temporal variations of the unique, synergistic, and redundant information of leaf area index, soil moisture, and snow cover about the visible white-sky surface albedo of 16 zones (basin names are indicated in Fig. 1c and subregions c4). Note that y-axis is a stacked graph and is not cumulative.
