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Abstract

Current glaciological research highlights the profound sensitivity of glacier mass balance and ice flow dynamics to climate change, evidenced by widespread thinning and retreat. Advances in satellite remote sensing, in-situ measurements, and numerical modeling are enhancing our understanding of subglacial hydrology, basal conditions, debris cover impacts, and calving processes. These factors are crucial for accurate projections of sea-level rise and freshwater availability. Studies on mountain glaciers and Antarctic ice streams indicate significant future ice loss and potential instability, influenced by thermal regimes and basal friction. Historical reconstructions provide context for glacier sensitivity to climate forcing, while atmospheric deposition represents an additional factor influencing melt rates.

Keywords: Glacier Mass Balance脥戮 Ice Flow Dynamics脥戮 Climate Change脥戮 Sea- Level Rise脥戮 Subglacial Hydrology脥戮 Remote Sensing脥戮 Glacier Retreat脥戮 Ice Streams脥戮 Calving Processes脥戮 Glacier Albedo