Quantifies how grounding-line melt parameterizations control long‑term evolution of the Wilkes Subglacial Basin and its sea‑level contribution; provides practical guidance for choosing melt schemes in projections.
Jan 1, 2024
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