Spatial patterns of water surface topography at a river confluence

• Published in: Earth surface processes and landforms 2002-08, Vol.27 (9), p.913-928
• Main Authors: Biron, Pascale M., Richer, Antoine, Kirkbride, Alistair D., Roy, André G., Han, Sangsoo
• Format: Article
• Language: English
• Subjects: Bgi / Prodig; confluences; Earth sciences; Earth, ocean, space; Exact sciences and technology; flow structure; Freshwater; Hydrology; Hydrology. Hydrogeology; Hydrometeorology; mixing layer; numerical modelling; Physical geography; turbulence; water surface elevation
• ISSN: 0197-9337; 1096-9837
• DOI: 10.1002/esp.359

Understanding flow structures in river confluences has largely been the product of interpretations made from measured flow velocity data. Here, we turn the attention to the investigation of the patterns of both the average and standard deviations of the micro‐topography of the water surface at an asymmetrical natural discordant confluence for different flow conditions. Water surface topography is measured using a total station to survey the position of a reflector mounted on a custom‐built raft. To limit error problems related to changes in the water level, measurements are taken and analysed by cross‐stream transects where five water surface profiles are taken before moving to the next transect. Three‐dimensional numerical simulations of the flow dynamics at the field site are used to examine predicted water surface topography for a steady‐state situation. The patterns are interpreted with respect to flow structure dynamics, visual observations of boils, and bed topography. Results indicate that coherent patterns emerge at the water surface of a discordant bed confluence for different flow conditions. The zone of stagnation and the mixing layer are characterized by super‐elevation, a lateral tilt is present at the edge of the mixing layer, and a zone of super‐elevation is present on the tributary side at the downstream junction corner. The latter seems associated with periodical upwelling and is not present in the numerical simulations that do not take into account instantaneous velocity fluctuations. Planform curvature, topographic steering related to the tributary mouth bar, and turbulent structures associated with the mixing layer all play a key role in the pattern of both the average and standard deviation of the water surface topography at confluences. Copyright © 2002 John Wiley & Sons, Ltd.