“…For example, nearly all long-term observations of precipitation are from weather stations below 3,000 m, meaning that glacierized elevations have been largely unmonitored. 13,14 As a result, precipitation amounts in these regions are poorly quantified, 15 and understanding of key processes remains limited, leading to substantial uncertainties in future projections of climate, glacier mass balance, and water resource availability. 16 Improving our knowledge of the precipitation climatology and key processes in the HKH is critical.…”