http://www.cnr.it/ontology/cnr/individuo/prodotto/ID49792
Global change and relative sea level rise at Venice: what impact in term of flooding (Articolo in rivista)
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- Label
- Global change and relative sea level rise at Venice: what impact in term of flooding (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00382-009-0617-5 (literal)
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- Carbognin L; Teatini P; Tomasin A; Tosi L (literal)
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- ISI Web of Science (WOS) (literal)
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- Institute of Marine Sciences, National Research Council, Castello 1364/a, 30122 Venice, Italy;
Department of Mathematical Methods and Models for Scientific Applications, University of Padova, via Trieste 63, 35121 Padua, Italy;
University Ca' Foscari in Venice, Dorsoduro 2137, 30123 Venice, Italy. (literal)
- Titolo
- Global change and relative sea level rise at Venice: what impact in term of flooding (literal)
- Abstract
- Relative sea level rise (RSLR) due to climate
change and geodynamics represents the main threat for the
survival of Venice, emerging today only 90 cm above the
Northern Adriatic mean sea level (msl). The 25 cm RSLR
occurred over the 20th century, consisting of about 12 cm of
land subsidence and 13 cm of sea level rise, has increased
the flood frequency by more than seven times with severe
damages to the urban heritage. Reasonable forecasts of the
RSLR expected to the century end must be investigated to
assess the suitability of the Mo.S.E. project planned for the
city safeguarding, i.e., the closure of the lagoon inlets by
mobile barriers. Here we consider three RSLR scenarios as
resulting from the past sea level rise recorded in the Northern
Adriatic Sea, the IPCC mid-range A1B scenario, and the
expected land subsidence. Available sea level measurements
show that more than 5 decades are required to compute a
meaningful eustatic trend, due to pseudo-cyclic 7-8 year
long fluctuations. The period from 1890 to 2007 is characterized
by an average rate of 0.12 ± 0.01 cm/year. We
demonstrate that linear regression is the most suitable model
to represent the eustatic process over these 117 year. Concerning
subsidence, at present Venice is sinking due to
natural causes at 0.05 cm/year. The RSLR is expected to
range between 17 and 53 cm by 2100, and its repercussions
in terms of flooding frequency are associated here to each
scenario. In particular, the frequency of tides higher than
110 cm, i.e., the value above which the gates would close the
lagoon to the sea, will increase from the nowadays 4 times
per year to a range between 20 and 250. These projections
provide a large spread of possible conditions concerning the
survival of Venice, from a moderate nuisance to an intolerable
aggression. Hence, complementary solutions to
Mo.S.E. may well be investigated. (literal)
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