Trackfiend
Civil/Environmental
- Jan 10, 2008
- 128
I have modeled a channel within HEC-RAS and am currently trying to calibrate said model with given historical data. I have been given both upstream and downstream elevations and various flows over a certain time period. I've inputed the downstream w.s. elevation and am trying to match (within a certain tolerance) the computed upstream w.s. elevation to the given historical data.
The main issue that I am dealing with is for any high flow situation. I am getting unrealistic upstream w.s. elevations due to HEC-RAS vertically extending the LOB and ROB in order to contain all of the flow. I am wondering what would be the best way to model overtopping of my banks? I see that there is a lateral weir option (with split flow optimization). Would adding a lateral weir (where the low points in the channel banks are located) along with a parallel channel or storage area in order to "store" any excess water that tops the banks? Any water that tops the banks merely flows into surrounding marsh and does not reenter the channel at any point.
Any suggestions?
The main issue that I am dealing with is for any high flow situation. I am getting unrealistic upstream w.s. elevations due to HEC-RAS vertically extending the LOB and ROB in order to contain all of the flow. I am wondering what would be the best way to model overtopping of my banks? I see that there is a lateral weir option (with split flow optimization). Would adding a lateral weir (where the low points in the channel banks are located) along with a parallel channel or storage area in order to "store" any excess water that tops the banks? Any water that tops the banks merely flows into surrounding marsh and does not reenter the channel at any point.
Any suggestions?