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 …

Climate change is expected to increase regional and global air temperatures and
significantly alter precipitation regimes. These projected changes in meteorological …

Human activities and climate change threaten coldwater organisms in freshwater
ecosystems by causing rivers and streams to warm, increasing the intensity and frequency of …

Lake eutrophication is a large and growing problem in many parts of the world, commonly
due to anthropogenic sources of nutrients. Improved quantification of nutrient inputs is …

Cold groundwater discharge to streams and rivers can provide critical thermal refuge for
threatened salmonids and other aquatic species during warm summer periods. Climate …

Groundwater has a predictable thermal signature that can be used to locate discrete zones
of discharge to surface water. As climate warms, surface water with strong groundwater …

Over the last 37 years, particular interest has been directed towards exploring the
characteristics of the optical environment for sensing, giving rise to what would now be one …

More than 75 years after its introduction, the seepage meter remains the only device for
directly quantifying exchange across the sediment-water interface between groundwater …

Stream temperature is a key habitat variable controlling all physical and biological river
processes. In light of the threat of climate change to fluvial environments, growing …