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Mass loss of the Antarctic ice sheet until the year 3000 under a sustained late-21st-century climate (1) ·
Morphodynamic modelling of beach cusp formation: the role of wave forcing and sediment composition (1) ·
The importance of turbulent ocean–sea ice nutrient exchanges for simulation of ice algal biomass and production with CICE6.1 and Icepack 1.2 (1)
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