Abstract
An approach to analyze high-end sea level rise is presented to provide a conceptual framework for high-end estimates as a function of time scale, thereby linking robust sea level science with stakeholder needs. Instead of developing and agreeing on a set of high-end sea level rise numbers or using an expert consultation, our effort is focused on the essential task of providing a generic conceptual framework for such discussions and demonstrating its feasibility to address this problem. In contrast, information about high-end sea level rise projections was derived previously either from a likely range emerging from the highest view of emissions in the Intergovernmental Panel on Climate Change assessment (currently the Representative Concentration Pathway 8.5 scenario) or from independent ad hoc studies and expert solicitations. Ideally, users need high-end sea level information representing the upper tail of a single joint sea level frequency distribution, which considers all plausible yet unknown emission scenarios as well as involved physical mechanisms and natural variability of sea level, but this is not possible. In the absence of such information we propose a framework that would infer the required information from explicit conditional statements (lines of evidence) in combination with upper (plausible) physical bounds. This approach acknowledges the growing uncertainty in respective estimates with increasing time scale. It also allows consideration of the various levels of risk aversion of the diverse stakeholders who make coastal policy and adaptation decisions, while maintaining scientific rigor.
Original language | English |
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Pages (from-to) | 923-938 |
Number of pages | 16 |
Journal | Earth's Future |
Volume | 7 |
Issue number | 8 |
DOIs | |
Publication status | Published - Aug 2019 |
Funding
The authors thank Robert Kopp and an anonymous reviewer for their detailed comments that helped improving the manuscript. This paper is a contribution to the Grand Challenge of Regional Sea level change and coastal impacts of the World Climate Research Programme. The content emerged from a workshop on high‐end sea level scenarios and held in Hamburg during September 2017 with partial support of the DFG‐funded Excellence Cluster CliSAP of the University Hamburg and of the DFG SPP 1889 on Sea Level Change and Society. R. W. acknowledges the ALW‐NPP program of NWO for financial support. J. C. was partially supported by the Centre for Southern Hemisphere Oceans Research, a joint research center between QNLM and CSIRO. B. P. H. acknowledges the funding from Singapore Ministry of Education Academic Research Fund Tier 2 MOE218‐T2‐1‐030. G. L. C. acknowledges ERA4CS support (grant 690462). No data are being used in this paper that would need to be made available.