TY - JOUR
T1 - Extreme sea levels at different global warming levels
AU - Tebaldi, Claudia
AU - Ranasinghe, Roshanka
AU - Vousdoukas, Michalis
AU - Rasmussen, D. J.
AU - Vega-Westhoff, Ben
AU - Kirezci, Ebru
AU - Kopp, Robert E.
AU - Sriver, Ryan
AU - Mentaschi, Lorenzo
N1 - Funding Information:
C.T.’s work was supported by the Multisector Dynamics program area of the US Department of Energy, Office of Science, Office of Biological and Environmental Research as part of the multi-programme, collaborative Integrated Coastal Modeling (ICoM) and by US Environmental Protection Agency, under Interagency Agreement DW-089-92459801. R.R. is supported by the AXA Research fund and the Deltares Strategic Research Programme ‘Natural Hazards’. Data and code supporting this paper were archived with the support of the MultiSector Dynamics-Living, Intuitive, Value-adding Environment (MSD-LIVE) project.
Publisher Copyright:
© 2021, The Author(s).
PY - 2021/9
Y1 - 2021/9
N2 - The Paris agreement focused global climate mitigation policy on limiting global warming to 1.5 or 2 °C above pre-industrial levels. Consequently, projections of hazards and risk are increasingly framed in terms of global warming levels rather than emission scenarios. Here, we use a multimethod approach to describe changes in extreme sea levels driven by changes in mean sea level associated with a wide range of global warming levels, from 1.5 to 5 °C, and for a large number of locations, providing uniform coverage over most of the world’s coastlines. We estimate that by 2100 ~50% of the 7,000+ locations considered will experience the present-day 100-yr extreme-sea-level event at least once a year, even under 1.5 °C of warming, and often well before the end of the century. The tropics appear more sensitive than the Northern high latitudes, where some locations do not see this frequency change even for the highest global warming levels.
AB - The Paris agreement focused global climate mitigation policy on limiting global warming to 1.5 or 2 °C above pre-industrial levels. Consequently, projections of hazards and risk are increasingly framed in terms of global warming levels rather than emission scenarios. Here, we use a multimethod approach to describe changes in extreme sea levels driven by changes in mean sea level associated with a wide range of global warming levels, from 1.5 to 5 °C, and for a large number of locations, providing uniform coverage over most of the world’s coastlines. We estimate that by 2100 ~50% of the 7,000+ locations considered will experience the present-day 100-yr extreme-sea-level event at least once a year, even under 1.5 °C of warming, and often well before the end of the century. The tropics appear more sensitive than the Northern high latitudes, where some locations do not see this frequency change even for the highest global warming levels.
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U2 - 10.1038/s41558-021-01127-1
DO - 10.1038/s41558-021-01127-1
M3 - Article
AN - SCOPUS:85113967406
SN - 1758-678X
VL - 11
SP - 746
EP - 751
JO - Nature Climate Change
JF - Nature Climate Change
IS - 9
ER -