Nature Climate Change, 9 February 2026
This study addresses emerging and cascading changes facing global mountain ecosystems from glacier loss, highlighting the damaging impact of such loss on diverse socio-ecological sectors and adaptation needs. Mountains provide both surface water and groundwater critical for downstream regions, especially in dry and semi-arid regions where billions of people rely on seasonal upstream flows. Rising temperatures increase glacier mass loss, initially triggering faster meltwater runoff but gradually reducing it over time as the ice volume shrinks. This shift causes runoff to peak earlier in the year and diminishes late-summer flows, weakening the natural buffering that sustains rivers during dry periods. Snow is also increasingly falling as rain in many regions, leading to earlier and more unpredictable runoff. At the same time, groundwater levels in several major mountain ranges are projected to decline, further reducing base flow and the resilience of river systems. These changes have direct consequences for downstream water availability, heightening competition for natural resources, intensifying drought impacts, and reducing low streamflows. Collectively, these trends underscore the far-reaching consequences of changing mountain water systems for downstream populations, reinforcing the urgency of transition from fossil fuel use.
By Science Writing Intern Haily Landrigan, Global Outreach Director Amy Imdieke, and ICCI Director Pam Pearson.
Published 2 月. 13, 2026 Updated 2 月. 13, 2026 10:34 下午
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