Abstract
Abstract. Sea level observations made in the Venice Lagoon between 1751 and 1792 have been recovered, consisting of two time series of daily data on high and low waters in Venice and Chioggia. From comparisons with modern observations, the quality of the 18th century data appears to be good enough to allow a useful analysis. A composite time series of daily mean sea level is obtained by merging the 18th century data and 1872–2004 observations in Venice Punta della Salute. The absence of reliable information on vertical references prevents the connection of the two 18th century time series with each other and with modern observations. However, daily sea level anomalies relative to the mean sea level enable us to recognize storm surge events that appear to occur more frequently in the second half of the 18th century than in the late 19th and 20th centuries, particularly during the 1751–1769 period. The record-breaking storm surge of 4 November 1966 turns out to be a remarkable event even in comparison to the events extracted from the 18th century time series. Further work is required to fill the gap between the old and modern observations.
Highlights
The coastal communities in the north Adriatic region and in the Venice Lagoon have always been sensitive to sea level variations, the occurrence of storm surges and related floods, locally known as acqua alta
Regular and still ongoing sea level monitoring in the north Adriatic started in the second half of the 19th century, and the time series provide long-term and accurate information about mean sea level (MSL) variability and storm surge frequency and intensity that has been exploited by several authors
The main aim of this paper is to describe the analysis of a time series of daily sea level data useful to study the storm surge frequency in the Venice Lagoon since 1751
Summary
The coastal communities in the north Adriatic region and in the Venice Lagoon have always been sensitive to sea level variations, the occurrence of storm surges and related floods, locally known as acqua alta (high water). Storm surges in the north Adriatic are the result of synoptic atmospheric forcing variability, and they are generally induced by southerly wind (sirocco) associated with cyclones over the western or central Mediterranean. The interaction of the sirocco flow with the orography surrounding the northern Adriatic can result in a north-easterly wind flow (Bora) that produces an additional sea level increase in the lagoon, at its south-western end (Camuffo, 1981). The earliest quantitative observations of sea level height seem to have been made in Venice by Francesco Rinuccini in 1638 on Galileo Galilei’s request by means of a pole (Rinuccini, 1966)
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