Academy Finds Mixed Climate Impacts on Himalayan Glaciers, Water Supplies

The eroding Rongbuk glacier in the Himalayas, in 1921 and today.

Given all the oversimplified assertions over the years about Himalayan glaciers in a warming global climate, it’s great to see a committee assembled by the National Academy of Sciences weigh in on the question with some data-based findings in a new report, “Himalayan Glaciers: Climate Change, Water Resources, and Water Security.” The bottom line — in sync with other recent analysis — is that the region is seeing a mix of changes, with glaciers growing in some places and shrinking in others and impacts on water supplies mostly inconsequential for decades to come. In most regions, monsoon patterns, population and consumption pressures and dependence on groundwater pumping will remain the dominant source of water-related risks, the report concludes. Read on for an excerpt from the news release and link to the full report, followed by related background:

Himalayan Glaciers Retreating at Accelerated Rate in Some Regions but Not Others; Consequences for Water Supply Remain Unclear, Says New Report

WASHINGTON — Glaciers in the eastern and central regions of the Himalayas appear to be retreating at accelerating rates, similar to those in other areas of the world, while glaciers in the western Himalayas are more stable and could be growing, says a new report from the National Research Council.

The report examines how changes to glaciers in the Hindu Kush-Himalayan region, which covers eight countries across Asia, could affect the area’s river systems, water supplies, and the South Asian population. The mountains in the region form the headwaters of several major river systems — including the Ganges, Mekong, Yangtze, and Yellow rivers — which serve as sources of drinking water and irrigation supplies for roughly 1.5 billion people.

The entire Himalayan climate is changing, but how climate change will impact specific places remains unclear, said the committee that wrote the report. The eastern Himalayas and Tibetan Plateau are warming, and the trend is more pronounced at higher elevations. Models suggest that desert dust and black carbon, a component of soot, could contribute to the rapid atmospheric warming, accelerated snowpack melting, and glacier retreat.

While glacier melt contributes water to the region’s rivers and streams, retreating glaciers over the next several decades are unlikely to cause significant change in water availability at lower elevations, which depend primarily on monsoon precipitation and snowmelt, the committee said. Variations in water supplies in those areas are more likely to come from extensive extraction of groundwater resources, population growth, and shifts in water-use patterns. However, if the current rate of retreat continues, high elevation areas could have altered seasonal and temporal water flow in some river basins. The effects of glacier retreat would become evident during the dry season, particularly in the west where glacial melt is more important to the river systems. Nevertheless, shifts in the location, intensity, and variability of both rain and snow will likely have a greater impact on regional water supplies than glacier retreat will. More