Abstract
Microseisms are used to estimate significant sea wave heights (Hs) in different parts of the world and also during extreme events (e.g., typhoons and hurricanes), as they are generated by the effect of sea waves on the sea bottom and are strictly related to the wave height. On 29 October 2018, an exceptional sea storm event (the Adrian storm) occurred in the Ligurian Sea (NW Mediterranean Sea), producing severe damage to coastal constructions and infrastructures. However, the microseism measured at seismic stations located near the coast did not show equivalent high energy, thus resulting in a severe underestimation of the Hs predicted. In the present study, the Adrian storm was compared to other sea storms that have occurred in the Ligurian Sea in recent decades. The aim of this paper is to statistically examine the distinctive peculiarities of the Adrian storm in order to find new parameters to insert in the empirical models used in the procedure recently implemented for monitoring of Hs through microseism recordings in the Ligurian Sea, improving the effectiveness in Hs estimates in cases of extreme events that do not produce high-energy microseisms. The results show that the additional parameters to be taken into account into the predictive model are the atmospheric pressure gradient and the wind intensity. A correction term is finally proposed and applied to the predictive model to significantly reduce the Hs underestimation.
Highlights
Sea wave height is one of the most relevant sea parameters to the monitoring and protection of coastal areas and to mitigation of marine risk associated with the occurrence of strong sea storm events
From microseism recordings s during strong marine events, four significant sea storms that occurred in the Ligurian Sea during stronginmarine events, four2012 significant seawere storms that occurred in the Ligurian
Following the methods described above, the sea wave parameters and atmospheric pressure data were analysed for the five sea storms considered in this study
Summary
Sea wave height is one of the most relevant sea parameters to the monitoring and protection of coastal areas and to mitigation of marine risk associated with the occurrence of strong sea storm events. The study of the wave characteristics, such as wave period, wavelength, significant wave height, and return period of sea storm, is essential for the design of offshore and coastal infrastructures, such as oil platforms, wind farms, breakwaters and artificial reefs, and for their conservation [1,2]. Wave buoys are typically very expensive and problematic, especially regarding their installation and maintenance. They usually provide discontinuous data (e.g., due to temporary damage) with poor spatial resolution (due to the low density of monitoring stations in sea areas).
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