Hi fellow modellers,
have been puzzled with this problem for a couple of days. I have a 2D model of an area with a dam (with 2 gates) in the middle of this area. I made a time series of opening for these 2 gates. After the model run (with no instabilities and converge problems). I found that there is a negative flow at one of the gates. Due to these negative flow values, the problem gate was sending water from downstream to upstream, even though the water from the model Upstream boundary condition did not reach the dam yet.
Interestingly raising the Gate invert (from 368 meters to 370 meters) did not result in negative flow. I chose 370 because the second gate had an invert of 370 meters. I checked that the elevation of HW and TW Cells, they are not higher than the invert elevation, I’ve given. I don’t wanna leave the invert at 370 meters, because the real elevation is 368.
Does anyone have an idea how this could be solved?
I can not understand how the invert is resulting in negative flow. Or to put it this way, how can invert create water in HEC-RAS?
Hope someone has an answer for this