Sediment Budget and Net Sediment Transport on a Coast Dominated by Waves and Offshore Currents: A Case Study on the Ishikawa Coast and Its Surrounding Areas in Japan

Abstract

This study discusses the coastal sediment budget for the Ishikawa coast using 12 years of observational datasets; it involves an understanding the local and regional sediment dynamics, the intensity of the transport processes in the region, and sediment supply from a local river. Although alongshore sediment transport and sediment budgets have been analyzed in previous studies, only a few conducted cross-shore sediment transport evaluations. The concentration of suspended sediments will be determined in this study, taking into account the influence of waves that are associated with the coastal current. The cross-shore sediment transport using sediment budget analysis indicated that the net alongshore sediment transport directions in the surf and offshore zones are opposite on the Ishikawa coast. The increase in the sediment budget of the surf zone can be attributed to the river sediment supply and longshore sediment transport inflow. Because of the significant outflow components of longshore and cross-shore sediment transports, the offshore zone budget showed a decreasing trend. A detailed sensitivity study was performed by varying the input parameters, in order to determine the possible ranges of net transport rates and sediment transport to the adjacent coasts. The results demonstrated the possibility of a clockwise residual sediment circulation. Our method can be used to analyze the alongshore sediment transport for other coasts and supplement future studies on coastal sedimentology and sediment budgets.

Impacts of sediment transported downstream from the 2015 deep‐seated landslide in Mt. Hakusan, Japan

“…The installation of the upstream Tedori River Dam also resulted in a significant reduction in the riverbed level in the Fan Top Tsurugi area (Dang et al, 2014). Further, Tedori River serves as a prime source of sediment replenishment to the coastal area (Thunyaphun et al, 2023). Notably, sediment from the Tedori River reaches as far as Chirihama Beach, situated 50 km to the east from estuary, effectively recharging sediment to the sandy beach (Sato et al, 2020).…”