The State and Fate of Himalayan Glaciers

Author:

Bolch T.12,Kulkarni A.3,Kääb A.4,Huggel C.15,Paul F.1,Cogley J. G.6,Frey H.15,Kargel J. S.7,Fujita K.8,Scheel M.15,Bajracharya S.9,Stoffel M.510

Affiliation:

1. Department of Geography, University of Zurich, 8057 Zürich Switzerland.

2. Institute for Cartography, Technische Universität Dresden, 01069 Dresden, Germany.

3. Divecha Center for Climate Change, Indian Institute of Science, Bangalore 560 012, India.

4. Department of Geosciences, University of Oslo, 0316 Oslo, Norway.

5. Institute for Environmental Sciences, University of Geneva, 1227 Geneva, Switzerland.

6. Department of Geography, Trent University, Peterborough, Ontario, Canada K9J 7B8.

7. Department of Hydrology and Water Resources, University of Arizona, Tucson, AZ 85721, USA.

8. Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan.

9. International Centre for Integrated Mountain Development (ICIMOD), Kathmandu, Nepal.

10. Institute of Geological Sciences, University of Bern, 3012 Bern, Switzerland.

Abstract

Going More Slowly Himalayan glaciers sometimes are called the “Third Pole” because of the amount of snow and ice they contain. Despite their importance as a global water reservoir and their essential role in Asian hydrology, how their mass is changing in response to global warming is not well known. Bolch et al. (p. 310 ) review the contemporary evolution of glaciers in the Himalayan region, including those of the less well sampled region of the Karakoram to the Northwest, in order to provide a current, comprehensive picture of how they are changing. Most Himalayan glaciers are retreating at rates comparable to glaciers elsewhere in the world. In the Karakorum, on the other hand, advancing glaciers are more common.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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