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      Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

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          Bedmap2: improved ice bed, surface and thickness datasets for Antarctica

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            Marine ice sheet collapse potentially under way for the Thwaites Glacier Basin, West Antarctica.

            Resting atop a deep marine basin, the West Antarctic Ice Sheet has long been considered prone to instability. Using a numerical model, we investigated the sensitivity of Thwaites Glacier to ocean melt and whether its unstable retreat is already under way. Our model reproduces observed losses when forced with ocean melt comparable to estimates. Simulated losses are moderate ( 1 mm per year of sea-level rise) collapse in the different simulations within the range of 200 to 900 years. Copyright © 2014, American Association for the Advancement of Science.
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              Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011

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                Author and article information

                Journal
                Nature Geoscience
                Nat. Geosci.
                Springer Science and Business Media LLC
                1752-0894
                1752-0908
                December 12 2019
                Article
                10.1038/s41561-019-0510-8
                7cc88c3f-7cee-4e34-b251-13215aed37a9
                © 2019

                http://www.springer.com/tdm

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