Japan Geoscience Union Meeting 2021

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG42] Water and sediment dynamics from land to coastal zones

Thu. Jun 3, 2021 3:30 PM - 5:00 PM Ch.11 (Zoom Room 11)

convener:Shinichiro Kida(Research Institute for Applied Mechanics, Kyushu University), Yuko Asano(The University of Tokyo), Keiko Udo(International Research Institute of Disaster Science, Tohoku University), Dai Yamazaki(Institute of Industrial Sciences, The University of Tokyo), Chairperson:Shinichiro Kida(Research Institute for Applied Mechanics, Kyushu University), Yuko Asano(The University of Tokyo), Dai Yamazaki(Institute of Industrial Sciences, The University of Tokyo), Keiko Udo(International Research Institute of Disaster Science, Tohoku University)

4:45 PM - 5:00 PM

[ACG42-12] Sediment transport and morphology change in coastal areas

*Keiko Udo1 (1.International Research Institute of Disaster Science, Tohoku University)

Keywords:coastal erosion, sediment budget, sediment size

Future sea-level rise and wave climate change are projected to further increase the coastal erosion risk in Japan, where coastal erosion has already progressed due to rapid development after 1950s. Although there have been many studies on coastal erosion, the simplest one-dimensional equilibrium beach profile model is still used for long-term projection of future coastlines because of the difficulty in estimating coastal morphology change accurately. On the other hand, the risk may decrease if the heavy rainfall frequency increases because the heavy rainfall may increase the amount of sediment supply from rivers to the coasts. Knowledge of sediment supply from rivers to the coasts has not yet been sufficient, and further knowledge needs to be obtained.
In this presentation, existing studies on the characteristics of coastal morphology change and their models, as well as existing studies on sediment dynamics in rivers and sediment supply to the coast, which have been discussed separately, are introduced, the problems of the current coastal morphology change models are summarized, and future prospects are discussed.