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Person

Bruce C Call

Interdisciplinary Physical Scientist and Geographer

Columbia Environmental Research Center

Email: bcall@usgs.gov
Office Phone: 573-875-5399
ORCID: 0000-0001-9064-2231

Location
CERC - R1 Research Building
4200 New Haven Road
Columbia , MO 65201
US

Supervisor: Caroline M Elliott
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The consists of longitudinal water surface profiles collected in a 10-km reach of the Missouri River at Sheepnose Bend downstream from Lexington, Missouri. Water surface elevation profiles were generated from data collected by USGS staff from the Columbia Environmental Research Center during multibeam sonar surveys of the channel bed in 2019, 2020, and 2021.
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The dataset contains data collected with an acoustic Doppler current profiler (ADCP) for a reach of the Missouri River at Sheepnose Bend downstream from Lexington, Missouri. Velocity data was collected using a TeleDyne Marine RD Instruments (Poway, California) Rio Grande Workhorse 600 kilohertz ADCP on June 4, 2020. Positioning used a Trimble Real-Time-Kinematic Global Navigation Satellite System. This data release consists of one shapefile with depth-averaged velocity magnitude and direction data and 40 text files that contain processed ascii velocity data exported from WinRIver II, Teledyne Marine RD Insturments (Poway, California) ADCP software.
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This dataset contains two- and quasi-three-dimensional hydrodynamic model outputs from the Flow and Sediment Transport with Morphologic Evolution of CHannels (FaSTMECH) hydrodynamic model in the open-source binary Visualization Toolkit (VTK) format (https://vtk.org/). The simulations were run at flows in the range of 185-635 cms at increments of 30 cms. This set of flow conditions pertains to the base lateral eddy viscosity scenario referred to as LEVx1 in Call et al., 2023. Files can be opened using the open-source software program Paraview: (https://www.paraview.org/).
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These two datasets contain metrics from hydrodynamic and particle tracking simulations for two sub-reaches of the Upper Missouri River near Wolf Point, MT. The upstream reach is referred to as the “upper” reach while the downstream reach is referred to as the “lower” reach. Simulations were performed for 16 flows in the range of 185-635 cms at increments of 30 cms.
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This dataset consists of a point shapefile with depth, velocity magnitude, XY velocity vector components, and vector angles from outputs of a two-dimensional hydrodynamic model of the Missouri River at Searcys Bend near Huntsdale, Missouri. The model was run at a discharge of 1,291 cubic meters per second (m3/s) to reflect average flow conditions on September 16, 2021, as measured by the U.S. Geological Survey’s Missouri River gaging station at Boonville, Missouri (USGS Gage 06909000). The simulation was run using the Flow and Sediment Transport with Morphologic Evolution of CHannels (FaSTMECH) hydrodynamic model within the International River Interface Cooperative (iRIC) software package (www.i-ric.org). Required...
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