River velocity is typically greatest in the upper reaches or headwaters where the gradient is steepest. It is also highest in the center of the channel and near the surface, where there is less friction compared to the riverbed and banks.
Relationship Between Average Stream Velocities, Stream Roughness, and Stream Gradient:
Stream Gradient:Higher Gradient: Leads to higher average stream velocities due to increased gravitational force. Lower Gradient: Results in lower average velocities as the gravitational force is reduced.
Stream Roughness:Higher Roughness: Decreases average stream velocities because friction from the rough bed and banks slows down the flow. Lower Roughness: Increases average velocities as smoother channels reduce friction and allow water to flow more freely.
In summary, higher gradients and lower roughness lead to greater average stream velocities, while lower gradients and higher roughness result in slower stream velocities.