Two-Way Coupling of the National Water Model (NWM) and Semi-Implicit Cross-Scale Hydroscience Integrated System Model (SCHISM) for Enhanced Coastal Discharge Predictions

Author:

Zhang Hongyuan1ORCID,Shen Dongliang2,Bao Shaowu1ORCID,Len Pietrafesa13

Affiliation:

1. Department of Marine Science, Coastal Carolina University, Conway, SC 29526, USA

2. Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

3. Department of Marine, Earth, Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA

Abstract

This study addresses the limitations of and the common challenges faced by one-dimensional river-routing methods in hydrological models, including the National Water Model (NWM), in accurately representing coastal regions. We developed a two-way coupling between the NWM and the Semi-implicit Cross-scale Hydroscience Integrated System Model (SCHISM). The approach demonstrated improvements in modeling coastal river dynamics, particularly during extreme events like Hurricane Matthew. The coupled model successfully captured tidal influences, storm surge effects, and complex river–river interactions that the standalone NWM missed. The approach revealed more accurate representations of peak discharge timing and magnitude as well as water storage and release in coastal floodplains. However, we also identified challenges in reconciling variable representations between hydrological and hydraulic models. This work not only enhances the understanding of coastal–riverine interactions but also provides valuable insights for the development of next-generation hydrological models. The improved modeling capabilities have implications for flood forecasting, coastal management, and climate change adaptation in vulnerable coastal areas.

Funder

National Oceanic and Atmospheric Administration

Publisher

MDPI AG

Reference31 articles.

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2. Pietrafesa, L.J., Zhang, H., Bao, S., Gayes, P.T., and Hallstrom, J.O. (2019). Coastal Flooding and Inundation and Inland Flooding due to Downstream Blocking. J. Mar. Sci. Eng., 7.

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