If the vertical diffusion is controlled solely by the local array properties, then Eq. In a step canopy with constant stem diameter over depth, CD ad is constant in each half of the canopy, implying constant Dz within each layer Eq. When a varies with height above the bed z see Fig. Then the evolution of the cloud can be evaluated by alternately applying Eq. To characterize the mean-shear dispersion, we must first characterize the velocity variation over depth.

## Redtuu. Shop by category.

If the vertical diffusion is controlled solely by the local array properties, then Eq. In a step canopy with constant stem diameter over depth, CD ad is constant in each half of the canopy, implying constant Dz within each layer Eq. When a varies with height above the bed z see Fig. Then the evolution of the cloud can be evaluated by alternately applying Eq. To characterize the mean-shear dispersion, we must first characterize the velocity variation over depth.

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