Abstract

Rising sea levels increase the probability of future coastal flooding. Many decision-makers use risk analyses to inform the design of sea-level rise (SLR) adaptation strategies. These analyses are often silent on potentially relevant uncertainties. For example, some previous risk analyses use the expected, best, or large quantile (i.e., 90%) estimate of future SLR. Here, we use a case study to quantify and illustrate how neglecting SLR uncertainties can bias risk projections. Specifically, we focus on the future 100-yr (1% annual exceedance probability) coastal flood height (storm surge including SLR) in the year 2100 in the San Francisco Bay area. We find that accounting for uncertainty in future SLR increases the return level (the height associated with a probability of occurrence) by half a meter from roughly 2.2 to 2.7 m, compared to using the mean sea-level projection. Accounting for this uncertainty also changes the shape of the relationship between the return period (the inverse probability that an event of interest will occur) and the return level. For instance, incorporating uncertainties shortens the return period associated with the 2.2 m return level from a 100-yr to roughly a 7-yr return period (∼15% probability). Additionally, accounting for this uncertainty doubles the area at risk of flooding (the area to be flooded under a certain height; e.g., the 100-yr flood height) in San Francisco. These results indicate that the method of accounting for future SLR can have considerable impacts on the design of flood risk management strategies.

Highlights

  • The warming climate is causing sea levels to rise around the globe [1,2,3,4]

  • If sea level is assumed to rise by the mean estimate or the 90% estimate in 2100, the 100-yr flood height would increase to a return level of roughly 2.2 m or 2.5 m, respectively (Fig 3 and S2 Fig)

  • We show how accounting for sea-level rise uncertainty can increase the area at risk of flooding and can increase the probability of flood occurrence

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Summary

Introduction

The warming climate is causing sea levels to rise around the globe [1,2,3,4]. Settlements and ecosystems in low-lying coastal areas become more vulnerable to flooding. About 10% of the world’s population resides within 10 meters of present-day sea level [5] and about 40 million people are exposed to a 100-yr ( known as the 1-in-100 year or 1% annual exceedance probability) storm surge [6]. Rising sea levels drive hazards for transportation and energy facilities, tourism, agriculture, and human lives [7].

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