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      Feasibility of ice sheet conservation using seabed anchored curtains

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      PNAS Nexus
      Oxford University Press

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          Abstract

          Sea level rise is expected to be rapid and extremely damaging to coastal communities and infrastructure, with unavoidable losses and coastal protection costs in the tens of billions per year. Retreat of the Thwaites and Pine Island Glaciers is likely already in an unstable regime as their oceanic fronts are ablated by deep intruding layers of relatively warm seawater. Warm water can be blocked from reaching the grounding line by thin flexible buoyant curtains anchored to the seabed. The consequent reduction in ice shelf melting could result in increased ice sheet buttressing as the shelf makes contact with seabed highs. Flexible curtains are less costly than solid artificial barriers, more robust against iceberg collisions, and easier to repair or remove in the event of unforeseen side effects. We illustrate the technical viability of this approach by considering curtain design concepts that should withstand oceanographic forces, and feasible methods of installation. Suitable materials are commonly available. Installation of a seabed curtain in temperate ocean waters would be entirely within the capabilities of existing offshore and deep ocean construction techniques. Installing in polar waters presents severe challenges from icebergs, harsh weather, and brief working seasons, which can however, be overcome with present-day technology. An 80 km long curtain installed in 600 m deep waters on alluvial sediments could help stabilize Pine Island and Thwaites glaciers over the next few centuries at much lower cost ($40–80 billion + $1–2 billion/yr maintenance) than the global coastline protection (∼$40 billion/yr) needed due to their collapse.

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          Most cited references40

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          A reconciled estimate of ice-sheet mass balance.

          We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets using common geographical regions, time intervals, and models of surface mass balance and glacial isostatic adjustment to estimate the mass balance of Earth's polar ice sheets. We find that there is good agreement between different satellite methods--especially in Greenland and West Antarctica--and that combining satellite data sets leads to greater certainty. Between 1992 and 2011, the ice sheets of Greenland, East Antarctica, West Antarctica, and the Antarctic Peninsula changed in mass by -142 ± 49, +14 ± 43, -65 ± 26, and -20 ± 14 gigatonnes year(-1), respectively. Since 1992, the polar ice sheets have contributed, on average, 0.59 ± 0.20 millimeter year(-1) to the rate of global sea-level rise.
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            Ice sheet grounding line dynamics: Steady states, stability, and hysteresis

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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

                Contributors
                Role: Editor
                Journal
                PNAS Nexus
                PNAS Nexus
                pnasnexus
                PNAS Nexus
                Oxford University Press (US )
                2752-6542
                March 2023
                28 March 2023
                28 March 2023
                : 2
                : 3
                : pgad053
                Affiliations
                Adjunct, Clean Energy Research Centre, University of British Columbia , 2329 West Mall, Vancouver BC V6T 1Z4, Canada
                College of Global Change and Earth Systems Science, Beijing Normal University , 19 Xinjiekouwai St, Haidian District, Beijing 100875, China
                Glaciology Section, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung , Bremerhaven, Germany
                College of Global Change and Earth Systems Science, Beijing Normal University , 19 Xinjiekouwai St, Haidian District, Beijing 100875, China
                Arctic Center, University of Lapland , Pohjoisranta 4, 96200 Rovaniemi, Finland
                Author notes
                To whom correspondence should be addressed: Email: john.moore.bnu@ 123456gmail.com

                Competing Interest: The authors declare no competing interest.

                Article
                pgad053
                10.1093/pnasnexus/pgad053
                10062297
                2b7efe85-c88a-4876-aeb8-36c265721863
                © The Author(s) 2023. Published by Oxford University Press on behalf of National Academy of Sciences.

                This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.

                History
                : 26 August 2022
                : 08 February 2023
                : 13 February 2023
                : 28 March 2023
                Page count
                Pages: 8
                Funding
                Funded by: National Key Science Program for Global Change Research;
                Award ID: 2015CB953600
                Funded by: Finnish Academy COLD Consortium;
                Award ID: 322430
                Categories
                Physical Sciences and Engineering
                Environmental Sciences
                AcademicSubjects/MED00010
                AcademicSubjects/SCI00010
                AcademicSubjects/SOC00010

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