“…Alexander and Holman (2004) confirmed the same tendency using Argus at four different sites with variable wave exposure (Noordwijk, The Netherlands; Agate Beach, Oregon, USA; Duck, North Carolina, USA; and Palm Beach, Australia). It is important to note that this is a typical forced response case, implying a sufficient time duration of the forcing factor (Stive and Reniers, 2003). For a site like Lido di Dante, where the typical duration of the observed storms was 22 h, the process may not be long enough to trigger the offshore migration of the form.…”