River‐groundwater interactions are at the core of a wide range of major contemporary
challenges, including the provision of high‐quality drinking water in sufficient quantities, the …

River–aquifer exchange is highly spatially variable. For this reason, methods that estimate
river gain or loss over small scales cannot be easily extrapolated to provide flux estimates …

Bioclogging in rivers can detrimentally impact aquifer recharge. This is particularly so in dry
regions, where losing rivers are common, and where disconnection between surface water …

Biofilm‐induced dynamic evolution of streambed permeability commonly concurs with the
transition from connection to disconnection between surface water and groundwater in arid …

The physics of disconnection between interrelated surface and groundwater has evolved
considerably in recent years, especially since conjunctive use of water resources is …

Prolonged exposure to human induced-stressors can profoundly modify the natural
trajectory of ecosystems. Predicting how ecosystems respond under stress requires …

Transmission losses from the beds of ephemeral streams are thought to be a widespread
mechanism of groundwater recharge in arid and semi‐arid regions and support a range of …

Ephemeral and intermittent flow in dryland stream channels infiltrates into sediments,
replenishes groundwater resources and underpins riparian ecosystems. However, the …

Numerical models with spatially-varying head as top boundary conditions were used in
previous studies to understand topography-driven groundwater flow. The head boundary …

Interactions between groundwater and surface water sustain groundwater-dependent
ecosystems and regulate river temperature and biogeochemical cycles, amongst many other …