Abstract

Decision-making in the area of coastal adaptation is facing major challenges due to ambiguity (i.e., deep uncertainty) pertaining to the selection of a probability model for sea level rise (SLR) projections. Possibility distributions are mathematical tools that address this type of uncertainty since they bound all the plausible probability models that are consistent with the available data. In the present study, SLR uncertainties are represented by a possibility distribution constrained by likely ranges provided in the IPCC Fifth Assessment Report and by a review of high-end scenarios. On this basis, we propose a framework combining probabilities and possibilities to evaluate how SLR uncertainties accumulate with other sources of uncertainties, such as future greenhouse gas emissions, upper bounds of future sea level changes, the regional variability of sea level changes, the vertical ground motion, and the contributions of extremes and wave effects. We apply the framework to evaluate the probability of coastal flooding by the year 2100 at a local, low-lying coastal French urban area on the Mediterranean coast. We show that when adaptation is limited to maintaining current defenses, the level of ambiguity is too large to precisely assign a probability model to future flooding. Raising the coastal walls by 85 cm creates a safety margin that may not be considered sufficient by local stakeholders. A sensitivity analysis highlights the key role of deep uncertainties pertaining to global SLR and of the statistical uncertainty related to extremes. The ranking of uncertainties strongly depends on the decision-maker’s attitude to risk (e.g., neutral, averse), which highlights the need for research combining advanced mathematical theories of uncertainties with decision analytics and social science.

Highlights

  • Adaptation to future coastal flooding requires testing different adaptation pathways against different potential futures (Ranger et al 2013; Haasnoot et al 2013)

  • This approach is justified in the Mediterranean region because (1) the complexity of processes taking place in the Mediterranean Sea prevents us from using published regional sea level projections in this area (Calafat et al 2012; Adloff et al 2018); (2) the published likely ranges for different regions only slightly differ from the likely ranges of global 2100 Sea level rise (SLR) projections; and (3) HE scenarios that are considered in the possibility approach (Sect. 3) rely on estimates of Antarctic melting, which remain highly imprecise today

  • While the available data justify the selection of a unique cumulative probability distribution function (CDF) for extremes and wave effects, this is not the case for the global sea level rise (GSLR), the RSLR, and the Vertical ground motion (VGM), which are represented by possibility distributions

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Summary

Introduction

Adaptation to future coastal flooding requires testing different adaptation pathways against different potential futures (Ranger et al 2013; Haasnoot et al 2013). These methods are termed extraprobabilistic because they avoid the selection of a single CDF by bounding all the possible ones that are consistent with the available data/information The feasibility of these approaches has been discussed for climate change impact assessments (e.g., Kriegler and Held 2005) and more recently for global SLR projections (Ben Abdallah et al 2014; Le Cozannet et al 2017). The concept using possibility distributions (Dubois and Prade 1988) for global projections based on the likely ranges from the IPCC Fifth Assessment Report (AR5) (Church et al 2013) and on assumptions on high-end (HE) scenarios On this basis, the present study goes a step further by presenting a framework for local flooding impact assessments, which combines both possibilities and probabilities to address the whole spectrum of uncertainties in addition to deep uncertainties in SLR prediction (from global to local scales).

Case study
Construction of possibility distributions
Method
Application
Uncertainty of the GSLR possibility distribution
Integrating risk aversion
Influence of the different uncertainty sources
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