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• W3204322017 abstract "Using three independent ice-flow models and several satellite-based datasets, we assess the importance of correctly capturing ice-shelf breakup, shelf thinning, and reduction in basal traction from ungrounding in reproducing observed speed-up and thinning of Thwaites Glacier between 1995 and 2015. We run several transient numerical simulations applying these three perturbations individually. Our results show that ocean-induced ice-shelf thinning generates most of the observed grounding line retreat, inland speed-up, and mass loss, in agreement with previous work. We improve the agreement with observed inland speed-up and thinning by prescribing changes in ice-shelf geometry and a reduction in basal traction over areas that became ungrounded since 1995, suggesting that shelf breakups and thinning-induced reduction in basal traction play a critical role on Thwaites's dynamics, as pointed out by previous studies. These findings suggest that modeling Thwaites's future requires reliable ocean-induced melt estimates in models that respond accurately to downstream perturbations." @default.
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• W3204322017 date "2021-10-19" @default.
• W3204322017 modified "2023-10-08" @default.
• W3204322017 title "Drivers of Change of Thwaites Glacier, West Antarctica, Between 1995 and 2015" @default.
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• W3204322017 doi "https://doi.org/10.1029/2021gl093102" @default.
• W3204322017 hasPublicationYear "2021" @default.
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