none2nopubblicazione presente in: http://journals.tdl.org/icce/index.php/icce/issue/view/361/showToc Rivista indicizzata su SCOPUS ma non ancora presente nel database sito del convegno http://www.icce2012.com/The main parameter for the assessment of coastal vulnerability and sediment transport is the wave run-up on the beach, defining the limit of maximum flooding, but also hydrodynamic properties in the Swash Zone (SZ) are trivial for the comprehension of hydro-morphodynamic processes. Several studies have been carried out on the SZ but few literature is still available on the run-up and on SZ flows on beaches protected by Low Crested Structures (LCSs), where flow motion is driven by a combination of low frequency infra-gravity w...