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Coupled ice shelf-ocean modeling and complex grounding line retreat from a seabed ridge : COUPLED ICE SHELF-OCEAN MODELING

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Journal of Geophysical Research: Earth Surface

Wiley-Blackwell

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      Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling

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        Acceleration of Jakobshavn Isbræ triggered by warm subsurface ocean waters

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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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            Author and article information

            Journal
            Journal of Geophysical Research: Earth Surface
            J. Geophys. Res. Earth Surf.
            Wiley-Blackwell
            21699003
            May 2016
            May 2016
            : 121
            : 5
            : 865-880
            10.1002/2015JF003791
            © 2016

            http://doi.wiley.com/10.1002/tdm_license_1.1

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