On the importance of river hydrodynamics in simulating groundwater levels and baseflows

• Published in: Hydrological processes Vol. 34; no. 8; pp. 1754 - 1767
• Main Authors: Quan, Tran Quoc, Meert, Pieter, Huysmans, Marijke, Willems, Patrick
• Format: Journal Article
• Language: English
• Published: Hoboken, USA John Wiley & Sons, Inc 15.04.2020; Wiley Subscription Services, Inc
• Subjects: Aquifers; Catchment area; Catchments; Components; Computational fluid dynamics; Computer simulation; Elevation; Fluid flow; Fluid mechanics; Groundwater; Groundwater discharge; Groundwater levels; groundwater model; Groundwater runoff; Hydrodynamics; Hydrologic models; Hydrology; integrated modelling; Mathematical models; Outlets; Performance evaluation; Resource management; River beds; River discharge; River flow; river hydrodynamics; River stages; Riverbeds; Rivers; Runoff; Statistical models; Subsurface runoff; Surface runoff; Water discharge; Water management; Water resources; Water resources management; Water table
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.13667

Research to date affirmed the key role of stream–aquifer interactions in integrated water resources management. The importance of river hydrodynamics on the spatial and temporal behaviour of groundwater was, however, not yet fully investigated. In contrast to the common approach where topography‐based estimates of riverbed elevation may lead to inappropriate discretization and constant river stages, this study couples a fully hydrodynamic and one‐dimensional river model to a two‐dimensional catchment hydrological model. The surface and subsurface runoff, groundwater, and river components are integrated into a single modelling framework. The coupled model was applied to a medium sized catchment in Belgium with three model setups, in which the level of detail of representation of river hydrodynamics varies. Further model iterations were carried out for the most exhaustive setup to assess the importance of the bi‐directional interactions between model components. Results show that higher details of river hydrodynamics help to improve the simulation of time‐averaged groundwater levels. However, the impacts were not that clear for the time‐varying groundwater levels. Moreover, visual and statistical model performance evaluation indicates a strong enhancement of the coupled models compared to the output from the hydrological model with respect to river discharge observations at catchment outlet and at internal stations. It also reveals the impact of river hydrodynamics on groundwater discharges when the most detailed setting delivered the highest performance among the three coupled models.