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The State and Fate of Himalayan Glaciers

Tobias BolchDepartment of Geography, University of Zurich, 8057 Zürich SwitzerlandAnil V. KulkarniDivecha Center for Climate Change, Indian Institute of Science, Bangalore 560 012, IndiaAndreas KääbDepartment of Geosciences, University of Oslo, 0316 Oslo, NorwayChristian HuggelDepartment of Geography, University of Zurich, 8057 Zürich SwitzerlandF. PaulDepartment of Geography, University of Zurich, 8057 Zürich SwitzerlandJ. Graham CogleyDepartment of Geography, Trent University, Peterborough, Ontario, Canada K9J 7B8Holger FreyDepartment of Geography, University of Zurich, 8057 Zürich SwitzerlandJeffrey S. KargelDepartment of Hydrology and Water Resources, University of Arizona, Tucson, AZ 85721, USAKoji FujitaGraduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, JapanM. ScheelDepartment of Geography, University of Zurich, 8057 Zürich SwitzerlandSamjwal Ratna BajracharyaInternational Centre for Integrated Mountain Development (ICIMOD), Kathmandu, NepalMarkus StoffelInstitute for Environmental Sciences, University of Geneva, 1227 Geneva, Switzerland
2012en
ABI

Аннотация

Himalayan glaciers are a focus of public and scientific debate. Prevailing uncertainties are of major concern because some projections of their future have serious implications for water resources. Most Himalayan glaciers are losing mass at rates similar to glaciers elsewhere, except for emerging indications of stability or mass gain in the Karakoram. A poor understanding of the processes affecting them, combined with the diversity of climatic conditions and the extremes of topographical relief within the region, makes projections speculative. Nevertheless, it is unlikely that dramatic changes in total runoff will occur soon, although continuing shrinkage outside the Karakoram will increase the seasonality of runoff, affect irrigation and hydropower, and alter hazards.

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