Landscapes receive water from precipitation and then transport, store, mix, and release it,
both downward to streams and upward to vegetation. How they do this shapes floods …

Processes that drive variability in catchment solute sourcing, transformation, and transport
can be investigated using concentration–discharge (C–Q) relationships. These relationships …

Hypoxia in coastal waters and lakes is widely recognized as a detrimental environmental
issue, yet we lack a comparable understanding of hypoxia in rivers. We investigated controls …

The analysis of concentration‐discharge (C‐Q) relationships from low‐frequency
observations is commonly used to assess solute sources, mobilization, and reactive …

Abstract The Upper Mississippi River Basin is the largest source of reactive nitrogen (N) to
the Gulf of Mexico. Concentration‐discharge (C‐Q) relationships offer a means to …

Stream dissolved oxygen (DO) dynamics are an outcome of metabolic activity and
subsequently regulate ecosystem functions such as in‐stream solute and sediment …

Deoxygenation of aquatic ecosystems is a key feature of the Anthropocene. Studies are
increasingly reporting low oxygen conditions in rivers and headwater streams even in the …

The temporal structures of gross primary production (GPP) and ecosystem respiration (ER)
vary across time scales in response to complex interactions among dynamic drivers (eg …

The rapid development of novel technologies to obtain high‐frequency observations has
provided new possibilities to observe and understand carbon cycling in inland waters. This …

Dissolved organic carbon (DOC) influences stream nitrogen (N) dynamics by regulating the
nutrient demand of heterotrophic microbes and mediating their interactions with nitrifiers …