Reconciling global mean and regional sea level change in projections and observations

The ability of climate models to simulate 20th century global mean sea level (GMSL) and regional sea-level change has been demonstrated. However, the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5) and Special Report on the Ocean and Cryosphere in a Changing Climate (S...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Wang, Jinping, Church, John A., Zhang, Xuebin, Chen, Xianyao
Format: Text
Language:English
Published: Nature Publishing Group UK 2021
Subjects:
Article
Ice Sheet
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7881246/
http://www.ncbi.nlm.nih.gov/pubmed/33579967
https://doi.org/10.1038/s41467-021-21265-6
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Summary:The ability of climate models to simulate 20th century global mean sea level (GMSL) and regional sea-level change has been demonstrated. However, the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5) and Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC) sea-level projections have not been rigorously evaluated with observed GMSL and coastal sea level from a global network of tide gauges as the short overlapping period (2007–2018) and natural variability make the detection of trends and accelerations challenging. Here, we critically evaluate these projections with satellite and tide-gauge observations. The observed trends from GMSL and the regional weighted mean at tide-gauge stations confirm the projections under three Representative Concentration Pathway (RCP) scenarios within 90% confidence level during 2007–2018. The central values of the observed GMSL (1993–2018) and regional weighted mean (1970–2018) accelerations are larger than projections for RCP2.6 and lie between (or even above) those for RCP4.5 and RCP8.5 over 2007–2032, but are not yet statistically different from any scenario. While the confirmation of the projection trends gives us confidence in current understanding of near future sea-level change, it leaves open questions concerning late 21(st) century non-linear accelerations from ice-sheet contributions.

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