2012
DOI: 10.9753/icce.v33.management.77
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An Early Warning System for the on-Line Prediction of Coastal Storm Risk on the Italian Coastline

Abstract: The ability to predict the imminent arrival of coastal storm risks is a valuable tool for civil protection agencies in order to prepare themselves and, if needs be, execute the appropriate hazard-reduction measures. In this study we present a prototype Early Warning System (EWS) for coastal storm risk on the Emilia-Romagna coastline in Northern Italy. This EWS is run by executing a chain of numerical models (SWAN, ROMS and XBeach) daily, with the final output transformed into a format suitable for decision mak… Show more

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Cited by 16 publications
(17 citation statements)
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“…The survey continued for a week following the passage 5 of the storm. The coastal landscape in Emilia-Romagna is generally comprised of low-lying sandy beaches with limited topographically elevated areas usually in the form of either relict beach ridges or artificial embankments (Armaroli et al, 2012). The shore is comprised of alternating spaces of natural areas with native dunes and intermixed with more prevalent urbanized areas with tourist facilities and coastal protection structures (i.e.…”
Section: Regional Settingsmentioning
confidence: 99%
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“…The survey continued for a week following the passage 5 of the storm. The coastal landscape in Emilia-Romagna is generally comprised of low-lying sandy beaches with limited topographically elevated areas usually in the form of either relict beach ridges or artificial embankments (Armaroli et al, 2012). The shore is comprised of alternating spaces of natural areas with native dunes and intermixed with more prevalent urbanized areas with tourist facilities and coastal protection structures (i.e.…”
Section: Regional Settingsmentioning
confidence: 99%
“…The exposure to coastal flooding is high, especially in the Ferrara and Ravenna provinces, where some elevations are below Mean Sea Level 15 (MSL), (Perini et al, 2010), and several defense structures (groins, breakwaters, etc.) have been built along the coast in the hope that beach retreat would cease (Armaroli et al, 2012).This problem has been exacerbated over the last few decades by land subsidence, which has been caused mostly by groundwater and gas extraction activities (Teatini et al, 2005;Taramelli et al, 2015). The subsequent vulnerability of local beaches to storm events led to the development of an Early Warning System (EWS), in the framework of the EU FP7 MICORE project (www.micore.eu), with the objective to predict the imminent arrival 20 of a storm as a tool to be used by civil protection agencies and local communities Harley et al, 2012;Harley et al, 2016).…”
Section: Regional Settingsmentioning
confidence: 99%
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“…The E-R coastal plain can be considered a low-energy environment with significant wave height H sig = 0.4 m (period T peak = 4 s) and a semidiurnal and micro-tidal regime, with an average maximum excursion of 0.7-0.8 m (IDROSER S.p.A., 1996;Harley et al, 2012). Wind waves are characterised by a significant height, with H sig = 3.3 m for 1-year return period (Armaroli et al, 2009), which is most frequently associated with the Bora weather conditions blowing from the east-northeast sectors.…”
Section: Coastal Stormsmentioning
confidence: 99%