Mountains are often referred to as water towers of the world, supplying fresh water to ecosystems and millions of people downstream. Specifically, snow and glacier melt are important elements in the water balance of mountain regions, supplying water during warmer and drier months of the year. However, little is known about how glacier melt partitions between reaching rivers directly or infiltrating below the surface to recharge deeper groundwater. Understanding this is critical in the face of climate change.
Glacier-Groundwater – Still Largely Ignored in the Mountain Water Cycle
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