The State and Fate of Himalayan Glaciers

American Association for the Advancement of Science (AAAS) - Tập 336 Số 6079 - Trang 310-314 - 2012
Tobias Bolch1,2, Anil V. Kulkarni3, Andreas Kääb4, Christian Huggel5, Frank Paul6, J. Graham Cogley7, Holger Frey5, Jeffrey S. Kargel8, Koji Fujita9, M. Scheel5, Samjwal Ratna Bajracharya10, Markus Stoffel5,11
1Department of Geography University of Zurich, 8057 Zürich, Switzerland
2Institute for Cartography, Technische Universität Dresden, 01069 Dresden, Germany.
3Divecha Center for Climate Change, Indian Institute of Science, Bangalore 560 012, India.
4Department of Geosciences, University of Oslo, 0316 Oslo, Norway
5Institute for Environmental Sciences, University of Geneva, 1227 Geneva, Switzerland.
6Department of Geography, University of Zurich, 8057 Zurich,#N#Switzerland
7Department of Geography, Trent University, Peterborough, Ontario, Canada K9J 7B8
8Department of Hydrology and Water Resources, University of Arizona, Tucson, AZ 85721 USA
9Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
10International Centre for Integrated Mountain Development (ICIMOD), Kathmandu, Nepal
11Institute of Geological Sciences, University of Bern, 3012 Bern, Switzerland

Tóm tắt

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.

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