Proglacial lakes drive ice flow decoupling between Himalayan glacier accumulation and ablation zones
This study reveals that the rapid expansion of proglacial lakes across the Himalaya has driven a post-2021 decoupling of ice flow, causing acceleration in the ablation zones of 66% of studied lake-terminating glaciers that overcomes thinning-induced deceleration, thereby necessitating the integration of localized topographic and lake-driven factors into predictive models for water security and flood risk management.