Date: Sept. 12, 2012
FOR IMMEDIATE RELEASE
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.
Melting of glacial ice could play an important role in maintaining water security during times of drought or similar climate extremes, the committee noted. During the 2003 European drought, glacial melt contributions to the Danube River in August were about three times greater than the 100-year average. Water stored as glacial ice could serve as the Himalayan region's hydrologic "insurance," adding to streams and rivers when it is most needed. Although retreating glaciers would provide more meltwater in the short term, the loss of glacier "insurance" could become problematic over the long term.
Water resources management and provision of clean water and sanitation are already a challenge in the region, and the changes in climate and water availability warrant small-scale adaptations with effective, flexible management that can adjust to the conditions, the committee concluded. Current efforts that focus on natural hazard and disaster reduction in the region could offer useful lessons when considering and addressing the potential for impacts resulting from glacial retreat and changes in snowmelt processes in the region.
Many basins in the region are "water-stressed" due to both social changes and environmental factors, and this stress is projected to intensify with large forecasted population growth, the committee concluded. Climate change could exacerbate this stress in the future.
Although the history of international river disputes suggests that cooperation is a more likely outcome than violent conflict in this region, social conditions could change. Therefore, modifications in water supplies could play an increasing role in political tensions, especially if existing water management institutions do not evolve to take better account of the region's social, economic, and ecological complexities, the committee said.
The National Research Council, the operating arm of the National Academy of Sciences and National Academy of Engineering, is an independent, nonprofit institution that provides science and technology advice under a congressional charter granted to the NAS in 1863. A committee roster follows.
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Pre-publication copies of Himalayan Glaciers: Climate Change, Water Resources, and Water Security are available from the National Academies Press; tel. 202-334-3313 or 1-800-624-6242 or on the Internet at http://www.nap.edu. Reporters may obtain a copy from the Office of News and Public Information (contacts listed above).
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NATIONAL RESEARCH COUNCIL
Division on Earth and Life Studies
Board on Atmospheric Sciences and Climate
Water Science and Technology Board
Division of Behavioral and Social Sciences and Education
Committee on Population
Committee on Himalayan Glaciers, Climate Change, and Implications for Downstream Populations
Henry J. Vaux Jr. (chair)
Professor Emeritus of Resource Economics
University of California at Berkeley and Riverside
El Cerrito, Calif.
Acting Associate Director
Institute for Demographic Research, and
Baruch School of Public Affairs
City University of New York
New York City
Edward R. Cook
Associate Research Scientist
Tree Ring Research Laboratory
Lamont-Doherty Geological Observatory
William K. Lau
Laboratory for Atmospheres
NASA Goddard Space Flight Center
Center for International Earth Sciences Information Network
Elizabeth L. Malone
Staff Scientist IV
Joint Global Change Research Institute
College Park, Md.
The Nature Conservancy
NASA Goddard Institute for Space Studies
New York City
Lonnie G. Thompson*
Distinguished University Professor
Byrd Polar Research Center
Ohio State University
James L. Wescoat Jr.
Aga Khan Program for Islamic Architecture
School of Architecture and Planning
Massachusetts Institute of Technology
Mark W. Williams
University of Colorado
RESEARCH COUNCIL STAFF
* Member, National Academy of Sciences