Glaciohydrology of the Himalaya-Karakoram

Author:

Azam Mohd. Farooq1ORCID,Kargel Jeffrey S.2,Shea Joseph M.3ORCID,Nepal Santosh4ORCID,Haritashya Umesh K.5ORCID,Srivastava Smriti1ORCID,Maussion Fabien6ORCID,Qazi Nuzhat7,Chevallier Pierre8ORCID,Dimri A. P.9ORCID,Kulkarni Anil V.10ORCID,Cogley J. Graham,Bahuguna Ishmohan11

Affiliation:

1. Discipline of Civil Engineering, Indian Institute of Technology Indore, Simrol 453552, India.

2. Planetary Science Institute, Tucson, AZ, USA.

3. Geography Program, University of Northern British Columbia, Prince George, BC V2N 4Z9, Canada.

4. International Centre for Integrated Mountain Development, Kathmandu, Nepal.

5. Department of Geology and Environmental Geosciences, University of Dayton, Dayton, OH 45469, USA.

6. Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innsbruck, Austria.

7. National Institute of Hydrology, Roorkee, India.

8. Hydrosciences Laboratory (CNRS, IRD, University of Montpellier), CC 57, 34090 Montpellier, France.

9. School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, India.

10. Indian Institute of Science, Divecha Center for Climate Change, Bangalore, India.

11. Space Application Centre, Ahmadabad, India.

Abstract

Waters of high Asia How the rivers of the Himalaya-Karakoram region of Asia respond to climate change is critical for the billion-plus people who depend on the water that they provide. In a review, Azam et al . discuss recent progress in understanding the importance of glacier and snow melt in the hydrological budget there, which is driven largely by advances in remote sensing and modeling. Observational data remain sparse and challenging to collect. —HJS

Funder

Department of Science and Technology, Ministry of Science and Technology

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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