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  • and obstacle Reynolds number, especially when morphometric variables were combined. Further validation, calibration and extension of this approach will help to adequately asses the influence of obstacles in the fluvial environment on micro- and meso-scale
  • 2012
  • The aim of this paper is to explore the interaction between bedform steered flow and bifurcation dynamics. The AA. present the predicted flow dynamics from the application of a Reynolds-averaged Navier–Stokes (RANS) model to a series of bifurcation
  • 2012
  • are used. Two distinct boundary layers (near the bed and in the vicinity of the ice cover, near the water surface) are clearly identified, each being characterized by high turbulent intensity levels. Detailed profile measurements of Reynolds stresses
  • 2012