Quantifying reductions in streamflow due to groundwater pumping (‘streamflow depletion') is essential for conjunctive management of groundwater and surface water resources. Analytical models are widely used to estimate streamflow depletion but …
Permafrost thaw due to climate warming modifies hydrological processes by increasing hydrological connectivity between aquifers and surface water bodies and increasing groundwater storage. While previous studies have documented arctic river baseflow …
As Andean glaciers rapidly retreat due to climate change, the balance of groundwater and glacial meltwater contributions to stream discharge in tropical, proglacial watersheds will change, potentially increasing vulnerability of water resources. The …