Abstract

Rising sea levels increase coastal extreme events of inundation along the global coastlines. Existing hydrologic and groundwater models simulate inundation processes but simplify groundwater-surface water interactions, a key control on flood generation in coastal areas. Here we apply a coupled surface–subsurface hydrologic model to evaluate the sensitivity of shallow groundwater to sea-level rise across three watersheds in Southeast China. It was found that historical decrease of annual rainfall resulted in no changes in total water storage but lower streamflow. Sea-level rise can increase low flow and local groundwater inundation, without changes in total water storage. GIS analysis of elevation can give a first approximation of vulnerability to marine inundation. Our physics-based modeling approach helped capture the temporal dynamics of water table and improved process understanding on coastal flooding. This study provides a new insight to quantify the spatiotemporal dynamics of groundwater inundation and river floods across coastal watersheds.

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