2020
DOI: 10.1007/s12210-020-00882-1
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Extreme events in Venice and in the North Adriatic Sea: 28–29 October 2018

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Cited by 15 publications
(17 citation statements)
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“…2). Only seven tidal constituents, four semidiurnal (M2, S2, N2 and K2) and three diurnal (K1, O1 and P1), give a significant contribution to the evolution of sea surface elevation in the northern Adriatic Sea, reaching a range of 1 m in the Trieste bay (Polli, 1961;Mosetti and Manca, 1972;Cushmain-Roisin et al, 2001;Orlić, 2001;Book et al, 2009) and resulting in a mixed, mainly semidiurnal tidal regime (Ferrarin et al, 2015, and references therein). The tidal form factor, consisting of the ratio of the amplitudes of the major diurnal and semidiurnal tidal constituents, reveals that the semidiurnal tidal regime (F < 1) prevails in the Adriatic Sea, although the tide maintains a diurnal character (F > 3) in the proximity of the semidiurnal amphidromic points located in the middle of central Adriatic Sea (Ursella and Gacic, 2001;Lovato et al, 2010;Ferrarin et al, 2017).…”
Section: Tidesmentioning
confidence: 99%
“…2). Only seven tidal constituents, four semidiurnal (M2, S2, N2 and K2) and three diurnal (K1, O1 and P1), give a significant contribution to the evolution of sea surface elevation in the northern Adriatic Sea, reaching a range of 1 m in the Trieste bay (Polli, 1961;Mosetti and Manca, 1972;Cushmain-Roisin et al, 2001;Orlić, 2001;Book et al, 2009) and resulting in a mixed, mainly semidiurnal tidal regime (Ferrarin et al, 2015, and references therein). The tidal form factor, consisting of the ratio of the amplitudes of the major diurnal and semidiurnal tidal constituents, reveals that the semidiurnal tidal regime (F < 1) prevails in the Adriatic Sea, although the tide maintains a diurnal character (F > 3) in the proximity of the semidiurnal amphidromic points located in the middle of central Adriatic Sea (Ursella and Gacic, 2001;Lovato et al, 2010;Ferrarin et al, 2017).…”
Section: Tidesmentioning
confidence: 99%
“…In Italy, the increasing frequency of coastal floods has been driven by an average sea level rise of 47 cm over the past 150 years [101], and sinking of the coast by natural and anthropogenic subsidence [102]. In Venice, the Italian coastal city most prone to flooding, the impacts of sea level rise are managed by mobile infrastructure called MOSE (Italian acronym for MOdulo Sperimentale Elettromeccanico) and by constructed esthetic landscapes with little impact on the environment, according to the community and local institutions [103].…”
Section: Mobile Damsmentioning
confidence: 99%
“…In October 2018 and November 2019, Venice and the North Adriatic have been exposed to extreme marine conditions (sea 140 level, waves) in turn induced by extreme weather conditions (Morucci et al, 2020). A complete list of other extreme events can be found in Lionello et al (this issue).…”
Section: The City Of Venicementioning
confidence: 99%
“…years 2012, 2014 and 2015, when a strong Bora wind was blowing (ISPRA, 2012;Coraci and Crosato, 2014). On the other hand Sirocco winds (south-easterly), blowing towards the North Adriatic Sea along the main basin axis, push water masses towards the Venice lagoon, particularly on the northern areas (Mariani et al, 2015).The combination of all these local effects 520 and climate change (Rinaldo et al, 2008) could lead to severe and disastrous storm surge events, as happened during the last two years (October 2018, November 2019; Morucci et al, 2020;AAVV, 2020).…”
Section: Local Effectsmentioning
confidence: 99%
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