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Upper limit for sea level projections by 2100

 

S Jevrejeva¹, A Grinsted² and J C Moore^3,4

 

1 National Oceanography Centre, Liverpool, UK

2 Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark

3 State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Global Change and Earth System Science, Beijing Normal University, Beijing, People's Republic of China

4 Arctic Centre, University of Lapland, Rovaniemi, Finland

 

ABSTRACT

We construct the probability density function of global sea level at 2100, estimating that sea level rises larger than 180 cm are less than 5% probable. An upper limit for global sea level rise of 190 cm is assembled by summing the highest estimates of individual sea level rise components simulated by process based models with the RCP8.5 scenario. The agreement between the methods may suggest more confidence than is warranted since large uncertainties remain due to the lack of scenario-dependent projections from ice sheet dynamical models, particularly for mass loss from marine-based fast flowing outlet glaciers in Antarctica. This leads to an intrinsically hard to quantify fat tail in the probability distribution for global mean sea level rise. Thus our low probability upper limit of sea level projections cannot be considered definitive. Nevertheless, our upper limit of 180 cm for sea level rise by 2100 is based on both expert opinion and process studies and hence indicates that other lines of evidence are needed to justify a larger sea level rise this century.

 

KEY WORDS: sea level rise, high end projections, climate change

 

PUBLISHED BY: Environmental Research Letters, 2014, 9 (10): 10.1088/1748-9326/9/10/104008

 

SOURCE:  http://iopscience.iop.org/1748-9326/9/10/104008