2017
DOI: 10.1080/17445647.2017.1415989
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Flooding scenario for four Italian coastal plains using three relative sea level rise models

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Cited by 33 publications
(33 citation statements)
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“…Coastal anthropization started in the 1950s [46], in the following decades the E-R coast became one of the most attractive tourist destinations in Italy and an important source for the regional economy. The combined effect of subsidence, sediment supply deficit due to the marked decrease in fluvial transport, removal of the dune ridge and increased anthropic pressure, cause the E-R coastal tract to be extremely sensitive to coastal flooding due to storm surges and sea-level rise [47]. In particular, a considerable portion of the E-R coastal area is currently below sea level and this would exacerbate the impact of future sea-level rise.…”
Section: Introductionmentioning
confidence: 99%
“…Coastal anthropization started in the 1950s [46], in the following decades the E-R coast became one of the most attractive tourist destinations in Italy and an important source for the regional economy. The combined effect of subsidence, sediment supply deficit due to the marked decrease in fluvial transport, removal of the dune ridge and increased anthropic pressure, cause the E-R coastal tract to be extremely sensitive to coastal flooding due to storm surges and sea-level rise [47]. In particular, a considerable portion of the E-R coastal area is currently below sea level and this would exacerbate the impact of future sea-level rise.…”
Section: Introductionmentioning
confidence: 99%
“…Located in the central Mediterranean Sea, the Italian peninsula has more than 7,500 km of coasts, hosting around 18% of the country population (ISTAT), numerous towns and cities, industrial plants, commercial harbours and touristic activities, as well as cultural and natural heritage sites. Existing country-scale estimates of SLR up to the end of this century helps to identify the most critically exposed coastal areas of Italy (Lambeck et al 2011;Bonaduce et al 2016;Antonioli et al 2017;Marsico et al 2017). The North Adriatic coastal plain is acknowledged to be the largest and most vulnerable location to extreme coastal events due to the shape, morphology and low bathymetry of the Adriatic sea basin, which cause water level to increase relatively fast during coastal storms (Carbognin et al 2010;Ciavola and Coco 2017;Perini et al 2017).…”
Section: Area Of Studymentioning
confidence: 99%
“…Most of the peninsula shows a slow subsiding trend, although with some local variability. An estimate of VLM rates due to tectonic activity have been derived from studies conducted in Italy (Lambeck et al 2011;Antonioli et al 2017;Marsico et al 2017;Solari et al 2018). The North Adriatic coastal plain shows the most intense long-term geological subsidence rates (about 1 mm per year), increasing North to South.…”
Section: Vertical Land Movementmentioning
confidence: 99%
“…The area of study comprises the Veneto and Friuli Venezia Giulia coast, with an overall length of about 290 km, located in the NA region ( Figure 1). It includes some of the low-lying plains more vulnerable to sea-level rise in the Mediterranean region [32,33] as well as various fragile ecosystems (e.g., coastal wetlands, lagoons, deltas) and invaluable cultural and socio-economic locations (e.g., the city of Venice). The region is characterized by several subsiding areas [34] and extreme storm surge events (high tides) occasionally flooding the city of Venice [35,36].…”
Section: Study Areamentioning
confidence: 99%