Subglacial water flow strengthens ice–ocean interactions and substantially increases Antarctica’s projected contribution to future sea‑level rise; results highlight the need to include hydrology in projections.
Jan 1, 2025
Open-borehole observations and 3D/1D Elmer/Ice simulations reveal a near‑isothermal basal marine‑ice layer and strong basal temperature gradients; we quantify how basal mass balance patterns control shelf rheology and dynamics.
Jan 1, 2022