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Long-term variability of storm surge frequency in the Venice Lagoon: an update thanks to 18th century sea level observations

机译:威尼斯泻湖风暴潮频率的长期变化:18世纪海平面观测资料的更新

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摘要

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.
机译:已恢复了1751年至1792年之间在威尼斯泻湖中进行的海平面观测,其中包括威尼斯和基奥贾的两个高低水位每日数据的时间序列。通过与现代观测结果进行比较,可以看出18世纪数据的质量足以进行有用的分析。通过将18世纪的数据和1872-2004年在威尼斯蓬塔·萨鲁特的观测资料合并,得出每日平均海平面的综合时间序列。在垂直参考资料上缺乏可靠的信息会阻止两个18世纪时间序列彼此之间以及与现代观测之间的联系。但是,相对于平均海平面而言,每天的海平面异常使我们能够认识到,在18世纪下半叶比在19世纪和20世纪后期,特别是在1751-1769年期间,更经常发生风暴潮事件。 1966年11月4日创纪录的风暴潮与18世纪时间序列中提取的事件相比,确实是一个了不起的事件。需要进一步的工作来填补旧的和现代的观测之间的空白。

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