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Published byOsborne Boone Modified over 5 years ago
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CLIMATE CHANGE IN THE HIMALAYAN CHAIN & ITS IMPACTS
Geoffrey Boulton with Magnus Hagdorn, Nick Hulton, Hugh Sinclair, Pete Nienow School of Geosciences University of Edinburgh
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Ganges/Brahmaputra/Indus Flux: ≈ 1,200 km3/year
Ice & snowmelt Flux to Plains: ≈ 400 km3/year (mostly in the dry season) Ice & snowmelt ≈ 80-85% of Ganges dry season flow In last 30 yrs - 11% reduction in dry season flow
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Nepal transect Highest ELA Peaks 6000m envelope 5000m LIA LGM 4000m
Mean lowest winter snowline LIA - Little Ice Age LGM - Last Glacial Maximum 3000m 50km swathe mean topography 30 km 60 km
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Representative October Images
1976 1989 2000
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