MORPHOLOGY CHANGE CAUSED BY THE 2011 GREAT TOHOKU TSUNAMI WAVE - MECHANISM OF RECENT CLOSURE AND BREACHING OF THE NANAKITA RIVER MOUTH. Coastal Engineering Proceedings, [S. l.], v. 1, n. 33, p. sediment.110, 2012. DOI: 10.9753/icce.v33.sediment.110. Disponível em: https://icce-ojs-tamu.tdl.org/icce/article/view/6790.. Acesso em: 3 jul. 2024.