i have two xs in 100 meters. The flow regime is supercritical.
In first time, i interpolated between this 2 xs with a distance of 10m, then ws elevation was stable, but i had a warning : i must add xs.
So , in second time i interpolated between the 2 xs with a distance of 1m, and then results in ws elevation were very different and become instable (multiple oscilations!) Same thing with lower step.
My question is : how can i define the good interpolation’s step between xs? Is it possible that a very low interpolation’s step make oscilations in the water surface elevation?
Why do you choose a interpolation 1 or 2 m? You should estimate a distance between cross section using Samuel equation and Fread’s euatione (see manual hec).
Can you send me your model? (using File- Debug report) I think, that you have more bugs in your model (ineffective area, abrupt change of bed of channel, …)
I thought Samuel’s equation must be used in case of unsteady flow data (relation time step and xs interpolation step)?
I choose a low xs interpolation step because of warnings in cross section Output “…this may indicate the need for additional cross sections” I thought results always where best with a low step?
Oddly I don’t seem to have the rapid oscillation when I run it on my machine. However I do still have the hydraulic jump after Section 130 for your higher flow profiles.
I was looking your model and your issue is a downstream condition (steady flow, reach boundary conditions).
Why did you choose a Know WS for the downstream condition? You cann´t use one WS for all flow (10,20,50, …)!!! You should use it, when you simulate one flow a you know a WS for this flow in the downstream cross section.
Do you understand me?
I changed:
upstream condition: from 0.01 to 0.006 Normal depth
downstream condition: from Know WS to Normal depth 0.01
OK for downstream condition, thanks! (My interest is near the bridge, downstream condition is far enough).
Sorry, oscillations appears with 0.5m step interpolation, under 1 m. (it’s also depending on manning value).
In this model, measuring station is unfortunately located near the bridge on supercritical flow, that’s why i must interpolate with very low step, and i founded that oscillation problem.