Skip to main content
. 2018 Feb 20;45(4):2047–2054. doi: 10.1002/2017GL076158

Figure 3.

Figure 3

Moisture sources for Kunlun Shan summer snowfall. Fractions of the snowfall that originates from a certain grid point for summers that have 2010‐level irrigation applied (a), and the difference in amount of moisture originated from a certain pixel for the ΔHIST case (b), and the ΔDEC case (c).