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Palabras clave – provistas por la editorial

Baltic Sea; cliff; sandy spit; beach; beach gravels; gravel grain shape; lithostatistical analysis; coastal zone dynamics; lithodynamics; beach sediment budget; coastal dynamics; beach evolution; coastal morphology; feed-back processes; Philippines; Lingayen Gulf; Suruga Bay; high-angle waves; sand spit; shoreline instability; BG model; rate of longshore sand transport; wave climate; nearshore bars; field data; cross-shore bar migration; wave conditions; wave non-linearity; storms; teleconnection patterns; Black Sea; crenulated-bay beach; hyperbolic-tangent shape; shoreline response; Boussinesq Wave model; coastal defences; extreme wave storms; tidal levels; tourist beaches; beach erosion; infrastructure damage; socioeconomic impacts; Tenerife; Canary Islands; volcanic coast; cliff instability; rock falls; Campi Flegrei; southern Italy; sea-level rise; InSAR; Magdalena River; coastal changes; subsidence; mangroves; sediment compaction; La Mancha lagoon; coastal; dynamics; DESCR framework; barrier spit; overwash; barrier migration; shoreline change; hurricane; extra-tropical storm; North Captiva Island; barrier island; Hurricane Charley; sediment transport; shoreline evolution; UAV data elaboration; coastal vulnerability assessment; CVA approach; Molise coast; Italy; morpho-sedimentological characterization; coastal system analysis and modeling; hydro-meteorological extremes; sea level rise; coastal hydrodynamics; beach erosion drivers; coastal susceptibility and risk; coastal dune and beach management; coastline defense and anthropization