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Showing 1 to 5 of 5 for “"von Karman Constant"”.

  1. Fluid Dynamics and Surface Pressure Fluctuations of Two-Dimensional Turbulent Boundary Layers Over Densely Distributed Surface Roughness

    … balance approach, and the validity of the von Karman constant for rough walls was tested. Five roughness fetches were evaluated: three sandpaper roughness fetches of varying grit size and two cases of uniformly distributed hemispheres of different spacing. Optical surface profilometry was …

    vt Repository record for Fluid Dynamics and Surface Pressure Fluctuations of Two-Dimensional Turbulent Boundary Layers Over Densely Distributed Surface Roughness (opens in a new tab)

  2. Series expansion of the Modified Einstein Procedure

    … (u. = -√ghS) and assuming the value of the von Karman constant (κ) is 0.4. For point concentration measurements, the Ro is calculated by fitting the concentration profile to the measured points. Lastly, SEMEP uses the measured unit sediment discharge and Ro to determine the unit bed …

    colostate Repository record for Series expansion of the Modified Einstein Procedure (opens in a new tab)

  3. Investigation of the Influence of Temperature Inversions and Turbulence on Land-atmosphere Interactions for Rolling Terrain

    … not be achieved as the value of the estimated von Karman constant (~0.62) is not close to that of the accepted value of 0.41. The impact of the irrigated farmland near the measurement site was observed in the latent heat flux, where the advection of moisture was evident in the tower moisture …

    unr Repository record for Investigation of the Influence of Temperature Inversions and Turbulence on Land-atmosphere Interactions for Rolling Terrain (opens in a new tab)

  4. Large eddy simulation of the upper atmospheric surface layer

    The von Karmãn constant (k) and the Monin-Obukhov similarity formulation occupy very important positions in the theoretical framework of the atmospheric surface layer (ASL). Measurements, however, provide a great scatter in their estimates mainly because the requirements of neutrality (only for …

    ubc Repository record for Large eddy simulation of the upper atmospheric surface layer (opens in a new tab)

  5. Nearshore sediment dynamics in a mixed sand/mud environment

    … varying as a function of elevation (z) and the von Karman constant (κ), i.e. 𝑙ₛ = κ𝚣. Within 4-8 cm of the bed 𝑙ₛ is constant and equal to 0.06 m. β is defined as the ratio of sediment diffusivity (εₛ) to eddy viscosity (ε∫), and is commonly used as a correction factor for predictive SSC profile …

    waikato-masters Repository record for Nearshore sediment dynamics in a mixed sand/mud environment (opens in a new tab)