Sub-regional variability in the influence of ice-contact lakes on Himalayan glaciers

• Main Authors: Scoffield, A.C., Rowan, A.V., Quincey, D.J., Carrivick, J.L., Sole, A.J., Cook, S.J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2024
• Subjects: Journal of Glaciology
• Online Access: https://eprints.whiterose.ac.uk/209145/; https://eprints.whiterose.ac.uk/209145/15/sub-regional-variability-in-the-influence-of-ice-contact-lakes-on-himalayan-glaciers.pdf

Ice-contact lakes modify glacier geometry and dynamics by shifting the majority of mass loss from the ice surface to the terminus. Lake-Terminating glaciers are known to experience greater thinning rates and higher velocities than land-Terminating glaciers, but the controls on variability in surface elevation change and ice flow between lake-Terminating glaciers in different regions remain poorly explored. We combined existing datasets of glacier velocity, surface elevation change and glacial lake area to characterise the evolution of 352 lake-Terminating and land-Terminating glaciers within three Himalayan sub-regions between 2000 and 2019. These analyses show that the influence of ice-contact lakes propagates up-glacier across only the lowermost 30% of the hypsometric distribution, even where lakes are well established. We find that ice-contact lakes only affect glacier behaviour when the lakes reach an advanced evolutionary stage; most clearly manifested in the Eastern Himalaya by statistically robust differences in glacier-wide surface elevation change between lake-Terminating (-0.68 ± 0.05 m a-1) and land-Terminating (-0.54 ± 0.04 m a-1) glaciers. These differences are driven by the presence of a greater number of well-developed ice-contact lakes in the Eastern Himalaya compared to in the Western and Central Himalaya, resulting from greater mass loss rates to date.