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The storm response of three Italian mixed beaches is investigated. Two sites are located\udon the eastern side of the country (Portonovo and Sirolo) and one on the western side\ud(Marina di Pisa). Portonovo and Sirolo are two mixed sand and gravel beaches (MSG)\udwhere the storms approach from two main directions (SE and NE). Marina di Pisa is a\udcomposite mixed beach subject to storms driven by SW. Gravel nourishments were\udundertaken in recent years on the three sites. Beach evolution was monitored measuring\udthe same network of topographic profiles at a monthly to seasonal frequency. Beach\udorientation and the presence of protecting structures are the main reasons for the\uddisplacement and the accumulation of significant amount of sediments. In Marina di\udPisa storm wave tend to pile material towards the upper part of the beach with no\udrotation of the shoreline. Sirolo and Portonovo act like pocket beaches with shoreline\udrotation that occurs after each storm in a clockwise or counter-clockwise direction. The\udwider and longer beach in Sirolo allows sediment to accumulate moderately during\udstorms rather in Portonovo, given its longshore boundaries, the material tend to pile up\udin greater thickness. Periods of fair weather tend to decrease beach slope in Marina di\udPisa and to increase beach width in Sirolo. After a big storm, in Sirolo and even more in\udPortonovo, the original beach configuration can be reached only after another storm of\udsimilar energy approaches by the opposite direction of the previous one

Coarse-grained beach response after storms in three Italian sites