Sediment Model Conditions
Source: County of Santa Clara
Additional scenarios were developed for the sediment model to expand the understanding of the sediment characteristics of the Pajaro River. The sediment model used the hydrology model results as one of several variables. Other variables included stream flow data, hydraulic roughness of the channel, and sediment data. Comparison between the current peak discharges shows the effects of varying stream flow. Increasing the channel hydraulic roughness simulates additional vegetation and impacts the velocity and water depth in the channel, which increases sediment deposition. The other conditions are developed based on an increase or decrease in actual sediment load which could result from changes in upstream land use, in stream gravel mining, incision and erosion of upstream channels, and reservoir construction.