A major gap in predictive capability concerning the future evolution of the ice sheets was identified in the Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change. As a consequence, it has been suggested that the AR4 estimates of future sea-level rise from this source may have been underestimated. Various approaches for addressing this problem have been tried, including semi-empirical models and conceptual studies. Here, we report a formalized pooling of expert views on uncertainties in future ice-sheet contributions using a structured elicitation approach. We find that the median estimate of such contributions is 29 cm-substantially larger than in the AR4-while the upper 95th percentile value is 84 cm, implying a conceivable risk of a sea-level rise of greater than a metre by 2100. On the critical question of whether recent ice-sheet behaviour is due to variability in the ice sheet-climate system or reflects a long-term trend, expert opinion is shown to be both very uncertain and undecided.
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Lamont Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000Lamont Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000
Siddall M.
Stocker T.F.
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Department of Earth Sciences, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, Queens RoadLamont Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000
Stocker T.F.
Clark P.U.
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Climate and Environmental Physics, Physics Institute, University of Bern, BernLamont Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000