D. S. Mueller C. R. Wagner 2001 <p>The quantification of current patterns is an essential component of a Water Quality Analysis Simulation Program (WASP) application in a riverine environment. The U.S. Geological Survey (USGS) provided a field validated two-dimensional Resource Management Associates-2 (RMA-2) hydrodynamic model capable of quantifying the steady-flowpatterns in the Ohio River extending from river mile 590 to 630 for the Ohio River Valley Water Sanitation Commission (ORSANCO) water-quality modeling efforts on that reach. Because of the hydrodynamic complexities induced by McAlpine Locks and Dam (Ohio River mile 607), the model was split into two segments: an upstream reach, which extended from the dam upstream to the upper terminus of the study reach at Ohio River mile 590; and a downstream reach, which extended from the dam downstream to a lower terminus at Ohio River mile 636. </p><p>The model was calibrated to a low-flow hydraulic survey (approximately 35,000 cubic feet per second (ft³/s)) and verified with data collected during a high-flow survey (approximately 390,000 ft³/s). The model calibration and validation process included matching water-surface elevations at 10 locations and velocity profiles at 30 cross sections throughout the study reach. Based on the calibration and validation results, the model is a representative simulation of the Ohio River steady-flow patterns below discharges of approximately 400,000 ft³/s.</p> application/pdf 10.3133/wri014091 en U.S. Geological Survey Calibration and validation of a two-dimensional hydrodynamic model of the Ohio River, Jefferson County, Kentucky reports