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      Projections of global-scale extreme sea levels and resulting episodic coastal flooding over the 21st Century

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          Abstract

          Global models of tide, storm surge, and wave setup are used to obtain projections of episodic coastal flooding over the coming century. The models are extensively validated against tide gauge data and the impact of uncertainties and assumptions on projections estimated in detail. Global “hotspots” where there is projected to be a significant change in episodic flooding by the end of the century are identified and found to be mostly concentrated in north western Europe and Asia. Results show that for the case of, no coastal protection or adaptation, and a mean RCP8.5 scenario, there will be an increase of 48% of the world’s land area, 52% of the global population and 46% of global assets at risk of flooding by 2100. A total of 68% of the global coastal area flooded will be caused by tide and storm events with 32% due to projected regional sea level rise.

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          Future flood losses in major coastal cities

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            The rising tide: assessing the risks of climate change and human settlements in low elevation coastal zones

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              Coastal flood damage and adaptation costs under 21st century sea-level rise.

              Coastal flood damage and adaptation costs under 21st century sea-level rise are assessed on a global scale taking into account a wide range of uncertainties in continental topography data, population data, protection strategies, socioeconomic development and sea-level rise. Uncertainty in global mean and regional sea level was derived from four different climate models from the Coupled Model Intercomparison Project Phase 5, each combined with three land-ice scenarios based on the published range of contributions from ice sheets and glaciers. Without adaptation, 0.2-4.6% of global population is expected to be flooded annually in 2100 under 25-123 cm of global mean sea-level rise, with expected annual losses of 0.3-9.3% of global gross domestic product. Damages of this magnitude are very unlikely to be tolerated by society and adaptation will be widespread. The global costs of protecting the coast with dikes are significant with annual investment and maintenance costs of US$ 12-71 billion in 2100, but much smaller than the global cost of avoided damages even without accounting for indirect costs of damage to regional production supply. Flood damages by the end of this century are much more sensitive to the applied protection strategy than to variations in climate and socioeconomic scenarios as well as in physical data sources (topography and climate model). Our results emphasize the central role of long-term coastal adaptation strategies. These should also take into account that protecting large parts of the developed coast increases the risk of catastrophic consequences in the case of defense failure.
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                Author and article information

                Contributors
                ian.young@unimelb.edu.au
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                30 July 2020
                30 July 2020
                2020
                : 10
                : 11629
                Affiliations
                [1 ]ISNI 0000 0001 2179 088X, GRID grid.1008.9, Department of Infrastructure Engineering, , University of Melbourne, ; Melbourne, Australia
                [2 ]Department of Water Science and Engineering, IHE-Delft, P.O. Box 3015, 2610 DA Delft, The Netherlands
                [3 ]ISNI 0000 0000 9294 0542, GRID grid.6385.8, Harbour, Coastal and Offshore Engineering, , Deltares, ; PO Box 177, 2600 MH Delft, The Netherlands
                [4 ]ISNI 0000 0004 0399 8953, GRID grid.6214.1, Water Engineering and Management, Faculty of Engineering Technology, , University of Twente, ; PO Box 217, 7500 AE Enschede, The Netherlands
                [5 ]ISNI 0000 0004 1754 9227, GRID grid.12380.38, Institute for Environmental Studies (IVM), , Vrije Universiteit Amsterdam, ; Amsterdam, The Netherlands
                [6 ]ISNI 0000 0000 9294 0542, GRID grid.6385.8, Deltares, ; Delft, The Netherlands
                [7 ]ISNI 0000 0001 1092 7967, GRID grid.8273.e, Tyndall Centre for Climate Change Research, , University of East Anglia, ; Norwich, NR4 7TJ UK
                [8 ]GRID grid.424922.b, Global Climate Forum, ; 10829 Berlin, Germany
                [9 ]ISNI 0000 0001 2248 7639, GRID grid.7468.d, Division of Resource Economics, Albrecht Daniel Thaer-Institute and Berlin Workshop in Institutional Analysis of Social-Ecological Systems (WINS), , Humboldt-University, ; Berlin, Germany
                Article
                67736
                10.1038/s41598-020-67736-6
                7393110
                32732976
                ee02cb2f-3343-4686-836a-a20e14e19b45
                © The Author(s) 2020

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 17 February 2020
                : 15 June 2020
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                © The Author(s) 2020

                Uncategorized
                physical oceanography,climate-change impacts,projection and prediction
                Uncategorized
                physical oceanography, climate-change impacts, projection and prediction

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