Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 424-427 |
| Number of pages | 4 |
| Journal | Nature Climate Change |
| Volume | 3 |
| Issue number | 4 |
| Early online date | 6 Jan 2013 |
| DOIs | |
| Publication status | Published - Apr 2013 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
Research Groups and Themes
- Bristol Glaciology Centre
Keywords
- CLIMATE-CHANGE
- GLACIER
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