Abstract

Abstract. The combined effect of global sea level rise and land subsidence phenomena poses a major threat to coastal settlements. Coastal flooding events are expected to grow in frequency and magnitude, increasing the potential economic losses and costs of adaptation. In Italy, a large share of the population and economic activities are located along the low-lying coastal plain of the North Adriatic coast, one of the most sensitive areas to relative sea level changes. Over the last half a century, this stretch of coast has experienced a significant rise in relative sea level, the main component of which was land subsidence; in the forthcoming decades, climate-induced sea level rise is expected to become the first driver of coastal inundation hazard. We propose an assessment of flood hazard and risk linked with extreme sea level scenarios, under both historical conditions and sea level rise projections in 2050 and 2100. We run a hydrodynamic inundation model on two pilot sites located along the North Adriatic coast of Emilia-Romagna: Rimini and Cesenatico. Here, we compare alternative extreme sea level scenarios accounting for the effect of planned and hypothetical seaside renovation projects against the historical baseline. We apply a flood damage model to estimate the potential economic damage linked to flood scenarios, and we calculate the change in expected annual damage according to changes in the relative sea level. Finally, damage reduction benefits are evaluated by means of cost–benefit analysis. Results suggest an overall profitability of the investigated projects over time, with increasing benefits due to increased probability of intense flooding in the near future.

Highlights

  • More than 700 million people live in low-lying coastal areas (McGranahan et al, 2007), and about 13 % of them are exposed to a 100-year-return-period flood event (Muis et al, 2016)

  • We develop a set of trigonometric equations based on harmonic analysis concepts to characterize the amplitude and period of tidal, storm surge and wave levels as the harmonic constituents that describe the theoretical temporal evolution of the nearshore total water level (TWL) during an ESL event

  • The flood extents corresponding to each return period (RP) scenario are shown for Rimini (Fig. 8) and Cesenatico (Fig. 9)

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Summary

Introduction

More than 700 million people live in low-lying coastal areas (McGranahan et al, 2007), and about 13 % of them are exposed to a 100-year-return-period flood event (Muis et al, 2016). According to the IPCC projections, it is very likely that, by the end of the 21st century, the SLR rate will exceed that observed in the period 1971–2010 for all Representative Concentration Pathway (RCP) scenarios (Pötner et al, 2019); yet the local sea level can have strong regional variability, with some places experiencing significant deviations from the global mean change (Stocker et al, 2013). This is worrisome in regions where small changes in the mean sea level (MSL) can drastically change the frequency of extreme sea level (ESL) events, leading to situations where a 100-year event may occur several times per year by 2100

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