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 …

Hydrologic connectivity is the linkage of separate regions of a catchment via water flow.
Knowledge of hillslope–stream connectivity (both at the surface and in the subsurface) is …

Global quantitative estimations of ecosystem functions are vital. Among those, ecosystem
respiration and photosynthesis contribute to carbon cycling and energy flow to food webs …

Downstream flow in rivers is repeatedly delayed by hydrologic exchange with off‐channel
storage zones where biogeochemical processing occurs. We present a dimensionless …

Headwater stream networks expand and contract in response to changes in stream
discharge. The changes in the extent of the stream network are also controlled by geologic …

Rainfall–groundwater interactions are complex and can depend upon a variety of hydro-
geological and geographical conditions and can commonly present high nonlinearity. This …

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

Abstract Groundwater–surface-water (GW-SW) interactions in streams are difficult to quantify
because of heterogeneity in hydraulic and reactive processes across a range of spatial and …

Hydrologic exchange fluxes (HEFs) vary significantly along river corridors due to
spatiotemporal changes in discharge and geomorphology. This variability results in the …

Examining the evolution of groundwater flow patterns is critical to understanding the
hydrological cycle and plays an important role in the sustainable management of water …