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And thrice for those above 160 cm.
The project should significantly reduce the effects of "exceptional high waters" (but not those of lesser, yet detrimental, tidal events) by completing the installation of 79 separate 300-ton flaps hinged on the seabed between the lagoon and the Adriatic sea.
Grado and, trieste, but much less often and to a lesser degree.
3 The creation of the industrial area of Porto Marghera, which lies immediately behind Venice, amplified the effects of high waters for two reasons: first, the land upon which the area is built was created by filling large parts of the lagoon where smaller islands.Comune di partouche poker scope Venezia (ed.).A b c d e Giordani Soika,.Venice's "Tide Monitoring and Forecast Center" evaluates that the city has lost 23 cm in its elevation since 1897, 1 the year of reference, 12 of which are attributable to natural causes (9 because of eustasy, 3 because of subsidence 13 are due to the additional.2 Should meteorological conditions (such as a strong scirocco wind blowing north along the major axis of the Adriatic basin) hamper the natural outflow of excess tidal water, high waters of greater magnitude can be expected in Venice.
In the 15th century, high tides were recorded in 14, on May 11, 1428, and on October 10, 1430, as well as in 14On November 10, 1442, the water is reported to have risen "four feet above the usual".
References edit Miozzi, Eugenio (1969).
Finally, in the decades before the installation of the marigraphs, high waters are recorded to have occurred on December 5, 1839, as well as in 1848 (140 cm) and 1867 (153 cm).
Exceptional high waters since 1923 edit The levels reached by high waters, engraved on the walls of Ca' Farsetti, Venice's City Hall.
The phenomenon occurs mainly between autumn and spring, when the astronomical tides are reinforced by the prevailing seasonal winds that hamper the usual reflux.
A b "Città di Venezia - Il contributo meteorologico".The main winds involved are the sirocco, which blows northbound along the Adriatic Sea, and the bora, which has a specific local effect due to the shape and location of the Venetian lagoon.For example: In Acqua Alta (1996 book 5, acqua alta is an important plot point, as the title suggests.13 Modern Era edit High waters were recorded on May 29, 1511; in 1517; on October 16, 1521; on October 3 and, again, on December 20, 1535.Rapporti Preliminari della Commissione di studio dei provvedimenti per la conservazione e difesa della laguna e della città di Venezia (in Italian).Introduction to Previsioni di Marea nell'Alto Adriatico (in Italian Venice, issue 29 of year 29, by Stefano Fracon Stravisi, Franco: Caratteristiche meteorologiche e climatiche del Golfo di Trieste Archived at the Wayback Machine., Università degli Studi di Trieste, Dipartimento di Scienze della Terra.




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