Research news on surface-water level

Surface-water level refers to the elevation or height of free water surfaces in rivers, lakes, reservoirs, wetlands, or other surface-water bodies relative to a defined vertical datum or local reference point. It is a fundamental hydrologic state variable controlling hydraulic gradients, flow directions, storage volume, and exchange with groundwater and the atmosphere. Surface-water level is monitored using gauges, pressure transducers, radar or ultrasonic sensors, and remote sensing, and is used to derive stage–discharge relationships, flood frequency statistics, and water-balance components. Temporal variability in surface-water level reflects the integrated effects of precipitation, evapotranspiration, inflows, outflows, regulation, and anthropogenic withdrawals.

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.

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