Aquanty
HGS RESEARCH HIGHLIGHT – Impact of River Morphology on River–Groundwater Exchange in Braided River Systems
Wöhling, T., Kraft, M., & Di Ciacca, A., (2026). Impact of River Morphology on River–Groundwater Exchange in Braided River Systems. Groundwater. doi.org/10.1111/gwat.70092
CLICK HERE TO READ THE ARTICLE.
“Highly detailed, fully coupled surface–subsurface models were set up in HydroGeoSphere using Lidar-derived DEMs taken before and after a major flood event in the two rivers. Apart from the river bathymetry, the two model variants of each site are otherwise identical, which allows investigating for the first time the change of both the net groundwater exchange fluxes and their spatial patterns due to naturally occurring shifts in riverbed morphology. This study addresses the following research question: Do river–groundwater interaction rates in braided rivers change as a result of changes in riverbed morphology? If so, what are the most influential hydro-morphological features for that change?”— Thomas Wöhling. et al., 2026 ♦
Fig 1. Conceptual overview of braidplain aquifer (BPA) topology and interaction. Top row shows exemplary cross-sections of saturation for the two models in this study: (A) Wairau River, BPA connected to regional aquifer, and (B) Waikirikiri River, BPA disconnected from regional aquifer. Bottom row shows the corresponding conceptual cross-sections of BPA systems connected to (C, Wairau River) and disconnected from (D, Waikirikiri River) the regional aquifer, with arrows indicating the main pathways of river to groundwater exchange/recharge (light to medium blue), BPA to regional aquifer exchange (medium to dark blue) and the intermediate pathway through the unsaturated zone (medium to light blue to dark blue, only disconnected).
We're pleased to highlight this publication by Thomas Wöhling, Moritz Kraft and Antoine Di Ciacca, which investigates how flood-driven changes in braided river morphology influence river–groundwater exchange and aquifer recharge. Using HydroGeoSphere (HGS), the researchers developed fully coupled surface water–groundwater models of two braided river systems in New Zealand to isolate the effects of changing riverbed morphology before and after major flood events. The study demonstrates that morphological changes alone can significantly alter both recharge to shallow braidplain aquifers and subsequent recharge to regional groundwater systems.
Braided rivers can be important sources of groundwater recharge, but their constantly changing channels, gravel bars, and riverbeds make river–groundwater exchange particularly difficult to quantify. Flood events can substantially reshape these systems, altering channel locations, wetted areas, river stages, and the geometry of the underlying braidplain aquifer. Although these morphological changes are well documented, their isolated effect on groundwater recharge has received comparatively little attention. Fully coupled surface–subsurface models such as HydroGeoSphere provide a more realistic representation of these interactions than approaches that treat rivers simply as groundwater boundary conditions.
The researchers applied HGS to sections of the Wairau River and Waikirikiri River on New Zealand's South Island, representing two contrasting hydrogeological settings. At the Wairau River, the braidplain aquifer is connected to the regional aquifer, while at the Waikirikiri River it is perched and separated from the deeper groundwater system by an unsaturated zone. For each site, the researchers created paired pre- and post-flood model variants using high-resolution LiDAR-derived digital elevation models. All model parameters and boundary conditions were kept the same between paired simulations, meaning differences in simulated river–groundwater exchange could be attributed directly to changes in river morphology.
♦Fig 3. Wairau River model study area with preflood (A, blue river channels) and postflood (B, green river channels) DEMs, along with model extent (red), braidplain extent (purple), analysis subdomain (white dashed), piezometer locations (blue circles) and main (bold), northern (dark), and southern (light) secondary river channels.
The simulations revealed contrasting responses at the two rivers. Following the flood, recharge from the Wairau River to its braidplain aquifer increased by approximately 38% under low-flow conditions and 12% during high flow. In contrast, braidplain aquifer recharge at the Waikirikiri River decreased by approximately 26% under both low- and high-flow conditions. Changes in recharge to the deeper regional aquifers followed the same direction as the braidplain response, demonstrating that flood-induced channel changes can propagate through the broader groundwater system regardless of whether the braidplain and regional aquifers are hydraulically connected or disconnected.
Key findings showed that these changes were closely associated with several observable morphological and hydrologic characteristics. Increased recharge at the Wairau River corresponded with greater braidplain aquifer elevation and volume, larger wetted areas, higher river and groundwater levels, and increased areas of strong exchange. The Waikirikiri River showed the opposite pattern, with decreases in braidplain volume, wetted area, water levels, and recharge following the flood. The study therefore demonstrates that seemingly physical changes to river geometry can alter hydraulic gradients and exchange pathways sufficiently to increase or decrease groundwater recharge.
♦Fig 5. Wairau River model grids and boundary conditions: grid and refinement features are shown for the preflood variant WU1 (purple lines and area) and postflood variant WU2 (orange lines and area). All other model features are identical: surface model boundaries (blue surfaces) are nodal river inputs (Wairau River [WR] and Are Are Creek [A]) and zero-depth gradient outflow (O), subsurface model boundaries are western, northern and eastern nodal fluxes (white rectangles) and southern constant head boundary (black line).
HydroGeoSphere was central to this work because its coupled surface water–groundwater framework enabled the researchers to explicitly represent highly detailed river morphology while simultaneously simulating flow within the river, braidplain aquifer, and regional groundwater system. By changing only the surface topography between paired simulations, the HGS models allowed the researchers to isolate the influence of morphology from other factors such as river forcing, aquifer properties, and boundary conditions. This provided a physically consistent way to quantify both the magnitude and spatial distribution of river–groundwater exchange under complex braided-river conditions.
This research provides important insights for groundwater management in regions where braided rivers are major sources of aquifer recharge. The findings demonstrate that flood-driven changes in river morphology should not be treated simply as surface-water changes, as they can have measurable consequences for groundwater availability and regional aquifer recharge. By identifying relationships between recharge and indicators such as wetted area, river levels, braidplain volume, and channel location, the study also provides a foundation for evaluating morphological impacts in river systems where detailed modelling may not always be feasible. At the same time, the researchers emphasize that fully quantifying these interactions remains complex and requires advanced modelling approaches such as HydroGeoSphere.
Abstract:
Braided river systems are an important source for groundwater recharge, but their complex morphology makes river–groundwater exchange fluxes difficult to estimate. Their river channel morphology changes frequently after floods, which has effects on recharge rates that have rarely been studied in the past. This work aims to isolate the effects of changes in braided river morphology on groundwater recharge for two sections of the Wairau River and Waikirikiri River in New Zealand. For each study site, two different river morphology variants of a fully coupled surface water–groundwater model utilizing high-resolution DEMs of river bathymetry before and after a major flood event were set up while keeping parameterization and boundary conditions the same. The models demonstrate that flood-induced morphology changes in braided river systems alter groundwater recharge. We identify features, both simulated and observed, that explain the direction of change. Features that increase groundwater recharge are a larger braidplain aquifer extent and volume, larger wetted area and, specifically, an increase of areas with high exchange rates in locations of larger gradients between braidplain aquifer and regional aquifer. These factors influence groundwater recharge independent of connection (Wairau River) or disconnection (Waikirikiri River) of the system to the regional aquifer, albeit with different magnitudes. An extension of our research to other braided rivers is needed to more broadly generalize our findings.
CLICK HERE TO READ THE ARTICLE.