09:15 〜 09:30
[AHW26-02] Effects of creek topology on salinization of coastal marsh due to storm surges
キーワード:marsh, storm surge, vertical saltwater intrusion, geomorphology, seawater intrusion, coastal resilience
Creek topology, which varies broadly across coastal marshes, affects both surface and subsurface flow and transport. In this study, we employed modeling tools to understand the role of creek networks in salt transport due to storm surges. We developed a stochastical morphodynamic model to represent three typical creek network groups: sparse, intermediate, and dense groups. We then utilized a variable-density, coupled surface-subsurface, flow and salt transport model to simulate a theoretical storm surge overwash event. Our model evaluated salinization of creek, marsh and aquifers. We examined how the presence of creek affect the extent and location of salinization by evaluating differences in salinity of surface waters and the subsurface. The salinization assessment showed that dense creek networks attenuated storm surge inundation and limited the salinization extent. The highest occurrence of opposite creek and groundwater flow directions was found in the sparse group, which delayed the salt flushing. The recovery from salinization varies nonlinearly in creek water, marsh sediments, and aquifers. Our study suggests that creek topology significantly affects the resilience of coastal marshes to saltwater intrusion, with important implications for coastal land management and ecosystem restoration.