Research news on stream discharge

Stream discharge, within hydrologic and fluvial geomorphology topics, refers to the volumetric flow rate of water moving through a stream or river cross section per unit time, typically expressed in cubic meters per second (m³/s). It is quantified as the product of cross-sectional area and mean flow velocity, and is highly variable in space and time due to precipitation, evapotranspiration, groundwater inputs, and human regulation. Stream discharge governs sediment transport capacity, channel morphology, nutrient and contaminant fluxes, and aquatic habitat conditions, and is a central variable in watershed modeling, flood frequency analysis, and water-resources management.

Drought dries major European rivers to record lows

Vast tracts of many of Europe's largest rivers, including the Rhine, Rhone and Danube, have slowed to a trickle never before recorded in July, data from a European climate observatory showed Monday.

How tides and river water combine to amplify floods

Ocean tides push upstream along coastal rivers, in some cases reaching hundreds of kilometers (hundreds of miles) inland. These inland stretches are known as tidal rivers, and they're the scene of complex interactions between ...

Breaking down the force of water in the Texas floods

Over just two hours, the Guadalupe River at Comfort, Texas, rose from hip-height to three stories tall, sending water weighing as much as the Empire State building downstream roughly every minute it remained at its crest.