heartlandce
Civil/Environmental
- Mar 11, 2013
- 7
We're working for a City to evaluate options for regional detention to mitigate overtopping of an existing detention facility. We have a dynamic rainfall-runoff model that we're using to route runoff determined using the TR-55 method. This is a coupled 1D/2D routing model, so any discharge not conveyed in the pipe network is conveyed as overland flow or stored on the surface. If we're evaluating overall system performance, we typically use a nested frequency rainfall distribution, which is essentially an SCS Type II distribution updated with current rainfall depths from NOAA Atlas 14. This works well to evaluate pipe capacity within basins with varying times of concentration.
However, this approach produces high rainfall intensities that can overwhelm the pipes upstream in the basins, causing flooding, which could then alter the hydrograph at the proposed detention pond location as the water that couldn't be handled by the upstream pipes is potentially delivered more slowly to the detention pond location. I'm concerned that this approach could underestimate the volume required. I'm wondering if we need to look at a more gradual rainfall distribution, where the rainfall occurs at lower intensities over a longer period of time.
Am I overthinking this?
However, this approach produces high rainfall intensities that can overwhelm the pipes upstream in the basins, causing flooding, which could then alter the hydrograph at the proposed detention pond location as the water that couldn't be handled by the upstream pipes is potentially delivered more slowly to the detention pond location. I'm concerned that this approach could underestimate the volume required. I'm wondering if we need to look at a more gradual rainfall distribution, where the rainfall occurs at lower intensities over a longer period of time.
Am I overthinking this?