MORPHOLOGY CHANGE CAUSED BY THE 2011 GREAT TOHOKU TSUNAMI WAVE – MECHANISM OF RECENT CLOSURE AND BREACHING OF THE NANAKITA RIVER MOUTH

Proceedings of the International Conference on Coastal Engineering

Ryutaro Hirao¹  Keiko Udo¹  Xuan Tinh Nguyen¹  Akira Mano¹  Hitoshi Tanaka¹  Eko Pradjoko¹ 

关键词: Nanakita River;    Tohoku Tsunami;    Great Tohoku Earthquake;    Morphology Change;    Erosion;    Breaching;   

DOI  :  10.9753/icce.v33.sediment.110

学科分类：建筑学

来源: Coastal Engineering Research Council

【 摘 要 】

The 2011 Great Tohoku Earthquake and Tsunami in March had caused a lot of damages to people and infrastructure in Japan. With a giant tsunami height plus the subsidence due to earthquakes have destroyed most o f the nearshore constructions and coastal zone areas. According to measured data from the survey group (Mori et al. 2011); maximum tsunamiwave height measured at the Nanakita area is about 14m. This Tsunami made the topography of this region changed drastically. Many breaching places occurred along the coast and river mouth. This study will focus on investigating the mechanisms of sediment transport and hydrodynamics leading to the river mouth was closedin about five months after the event and then breached in a different location during the river flood.

【 授权许可】

Unknown