Uncertainties in Long-Term Twenty-First Century Process-Based Coastal Sea-Level Projections

Review (2019)
Authors

Roderik S.W. van de Wal (Universiteit Utrecht)

X Zhang (Centre for Southern Hemisphere Oceans Research (CSHOR))

S. Minobe (Hokkaido University)

S. Jevrejeva (National Oceanography Center, Centre for Climate Research Singapore)

REM Riva (TU Delft - Physical and Space Geodesy)

C. Little (Atmospheric and Environmental Research, Inc.)

K. Richter (University of Innsbruck)

Matthew D. Palmer (Met Office)

Research Group
Physical and Space Geodesy
Copyright
© 2019 R. S.W. van de Wal, X. Zhang, S. Minobe, S. Jevrejeva, R.E.M. Riva, C. Little, K. Richter, M. D. Palmer
To reference this document use:
https://doi.org/10.1007/s10712-019-09575-3
More Info
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Publication Year
2019
Language
English
Copyright
© 2019 R. S.W. van de Wal, X. Zhang, S. Minobe, S. Jevrejeva, R.E.M. Riva, C. Little, K. Richter, M. D. Palmer
Research Group
Physical and Space Geodesy
Issue number
6
Volume number
40
Pages (from-to)
1655-1671
DOI:
https://doi.org/10.1007/s10712-019-09575-3
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Abstract

Many processes affect sea level near the coast. In this paper, we discuss the major uncertainties in coastal sea-level projections from a process-based perspective, at different spatial and temporal scales, and provide an outlook on how these uncertainties may be reduced. Uncertainty in centennial global sea-level rise is dominated by the ice sheet contributions. Geographical variations in projected sea-level change arise mainly from dynamical patterns in the ocean response and other geophysical processes. Finally, the uncertainties in the short-duration extreme sea-level events are controlled by near coastal processes, storms and tides.