about
Committed sea-level rise for the next century from Greenland ice sheet dynamics during the past decade.Enhanced basal lubrication and the contribution of the Greenland ice sheet to future sea-level rise.Effect of uncertainty in surface mass balance–elevation feedback on projections of the future sea level contribution of the Greenland ice sheetProbabilistic parameterisation of the surface mass balance–elevation feedback in regional climate model simulations of the Greenland ice sheetIce-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project)Insights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project I: AntarcticaInsights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project II: GreenlandBenchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP–HOM)Dynamic patterns of ice stream flow in a 3-D higher-order ice sheet model with plastic bed and simplified hydrologyFeedbacks between coupled subglacial hydrology and glacier dynamicsA Parallel Computational Model for Three-Dimensional, Thermo-Mechanical Stokes Flow Simulations of Glaciers and Ice SheetsFuture climate warming increases Greenland ice sheet surface mass balance variabilityManufactured solutions and the verification of three-dimensional Stokes ice-sheet modelsA parallel high-order accurate finite element nonlinear Stokes ice sheet model and benchmark experimentsFrom the front
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հետազոտող
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Stephen F. Price
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Stephen F. Price
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0000-0001-6878-2553