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Research Article

Coastal sea level rise with warming above 2 °C

Svetlana Jevrejeva, Luke P. Jackson, Riccardo E. M. Riva, Aslak Grinsted, and John C. Moore
  1. aNational Oceanography Centre, Liverpool L3 5DA, United Kingdom;
  2. bProgramme for Economic Modelling, Nuffield College, University of Oxford, Oxford OX1 1NF, United Kingdom;
  3. cDepartment Geoscience and Remote Sensing, Delft University of Technology, 2628CN Delft, The Netherlands;
  4. dClimate Institute, Delft University of Technology, 2628CN Delft, The Netherlands;
  5. eCentre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, DK-2100 Copenhagen, Denmark;
  6. fJoint Center for Global Change Studies, College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China;
  7. gArctic Centre, University of Lapland, FI-96101 Rovaniemi, Finland

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PNAS November 22, 2016 113 (47) 13342-13347; first published November 7, 2016; https://doi.org/10.1073/pnas.1605312113
Svetlana Jevrejeva
aNational Oceanography Centre, Liverpool L3 5DA, United Kingdom;
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  • For correspondence: sveta@noc.ac.uk john.moore.bnu@gmail.com
Luke P. Jackson
aNational Oceanography Centre, Liverpool L3 5DA, United Kingdom;
bProgramme for Economic Modelling, Nuffield College, University of Oxford, Oxford OX1 1NF, United Kingdom;
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Riccardo E. M. Riva
cDepartment Geoscience and Remote Sensing, Delft University of Technology, 2628CN Delft, The Netherlands;
dClimate Institute, Delft University of Technology, 2628CN Delft, The Netherlands;
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Aslak Grinsted
eCentre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, DK-2100 Copenhagen, Denmark;
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John C. Moore
fJoint Center for Global Change Studies, College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China;
gArctic Centre, University of Lapland, FI-96101 Rovaniemi, Finland
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  • For correspondence: sveta@noc.ac.uk john.moore.bnu@gmail.com
  1. Edited by Anny Cazenave, Centre National d'Etudes Spatiales, Toulouse, France, and approved October 3, 2016 (received for review April 1, 2016)

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Significance

Warming of 2 °C will lead to an average global ocean rise of 20 cm, but more than 90% of coastal areas will experience greater rises. If warming continues above 2 °C, then, by 2100, sea level will be rising faster than at any time during human civilization, and 80% of the global coastline is expected to exceed the 95th percentile upper limit of 1.8 m for mean global ocean sea level rise. Coastal communities, notably rapidly expanding cities in the developing world; small island states; United Nations Educational, Scientific and Cultural Organization Cultural World Heritage sites; and vulnerable tropical coastal ecosystems will have a very limited time after midcentury to adapt to these rises.

Abstract

Two degrees of global warming above the preindustrial level is widely suggested as an appropriate threshold beyond which climate change risks become unacceptably high. This “2 °C” threshold is likely to be reached between 2040 and 2050 for both Representative Concentration Pathway (RCP) 8.5 and 4.5. Resulting sea level rises will not be globally uniform, due to ocean dynamical processes and changes in gravity associated with water mass redistribution. Here we provide probabilistic sea level rise projections for the global coastline with warming above the 2 °C goal. By 2040, with a 2 °C warming under the RCP8.5 scenario, more than 90% of coastal areas will experience sea level rise exceeding the global estimate of 0.2 m, with up to 0.4 m expected along the Atlantic coast of North America and Norway. With a 5 °C rise by 2100, sea level will rise rapidly, reaching 0.9 m (median), and 80% of the coastline will exceed the global sea level rise at the 95th percentile upper limit of 1.8 m. Under RCP8.5, by 2100, New York may expect rises of 1.09 m, Guangzhou may expect rises of 0.91 m, and Lagos may expect rises of 0.90 m, with the 95th percentile upper limit of 2.24 m, 1.93 m, and 1.92 m, respectively. The coastal communities of rapidly expanding cities in the developing world, and vulnerable tropical coastal ecosystems, will have a very limited time after midcentury to adapt to sea level rises unprecedented since the dawn of the Bronze Age.

  • 2° warming
  • coastal sea level rise
  • probabilistic sea level projections
  • regional sea level rise

Footnotes

  • ↵1To whom correspondence may be addressed. Email: sveta{at}noc.ac.uk or john.moore.bnu{at}gmail.com.
  • Author contributions: S.J. designed research; L.P.J. performed research; R.E.M.R. and A.G. contributed new reagents/analytic tools; S.J. and L.P.J. analyzed data; and S.J., L.P.J., R.E.M.R., A.G., and J.C.M. wrote the paper.

  • The authors declare no conflict of interest.

  • This article is a PNAS Direct Submission.

  • This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1605312113/-/DCSupplemental.

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Coastal sea level rise with warming above 2 °C
Svetlana Jevrejeva, Luke P. Jackson, Riccardo E. M. Riva, Aslak Grinsted, John C. Moore
Proceedings of the National Academy of Sciences Nov 2016, 113 (47) 13342-13347; DOI: 10.1073/pnas.1605312113

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Coastal sea level rise with warming above 2 °C
Svetlana Jevrejeva, Luke P. Jackson, Riccardo E. M. Riva, Aslak Grinsted, John C. Moore
Proceedings of the National Academy of Sciences Nov 2016, 113 (47) 13342-13347; DOI: 10.1073/pnas.1605312113
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Proceedings of the National Academy of Sciences: 113 (47)
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