Stream temperature is one of the most critical factors controlling aquatic ecosystem health.
Practitioners and researchers from a range of fields, including biology, ecology, hydrology …

Fifty years of hyporheic zone research have shown the important role played by the
hyporheic zone as an interface between groundwater and surface waters. However, it is only …

Previously regarded as the passive drains of watersheds, over the past 50 years, rivers have
progressively been recognized as being actively connected with off‐channel environments …

The hyporheic zone, defined by shallow subsurface pathways through river beds and banks
beginning and ending at the river, is an integral and unique component of fluvial systems. It …

Beaver dams affect hydrologic processes, channel complexity, and stream temperature in
part by inundating riparian areas, influencing groundwater–surface water interactions, and …

Hyporheic flow in streams has typically been studied separately from geomorphic
processes. We investigated interactions between bed mobility and dynamic hyporheic …

Despite decades of research, we lack an accurate framework to predict and manage
hydrologic exchange in the river corridor and the associated ecosystem services and …

Recent advances in fluorometry have led to increased use of rhodamine WT as a tracer in
streams and rivers. In light of this increased use, a review of the dye's behavior in freshwater …

Due to its simplicity, adaptability, and accessibility, the transient storage model has become
one of the most widely used tools to investigate transport and exchange processes in …

Improved predictions of hyporheic exchange based on easily measured physical variables
are needed to improve assessment of solute transport and reaction processes in …