Foremost I would like to know what happens to 1D/2D flow error. The minimum flow tolerance in my model is 50 cfs, with up to 10 iterations. I have 1D/2D flow errors from 51 cfs to as much as 200 cfs. Is mass being conserved? The manual does not say, where minimum flow tolerance is described.
The purpose of the model is to evaluate flood extent and elevation in a small low gradient valley. The watershed extends east from a saddle point in the valley, through a marshy meadow that was ditched around 1900 (s ≈ 0.0015), to a natural channel (s ≈ 0.025) and a downstream confluence with a larger creek where a gauge was located.
The hydraulic model extends from near the saddle point east to the larger confluence. The 2D area is at the head of the model and extends as far as the steeper natural channel. The 1D model extends from downstream at the confluence with the larger stream up the natural channel to the 2D area, and about 4000 feet into the 2D area. Changes to channel characteristics or culverts are being considered in the upstream reach of the 1D model. See geometry detail below.
There are eight lateral weirs along each bank of the water course connecting the 1D and 2D areas. They essentially span the entire length of the lateral interfaces, with consideration given to cell, cross section, and culvert locations. The terrain is fairly uniform, without many obvious high spots where flow exchange would not occur. Some of the lateral structures are several hundred feet long. Should I have made them shorter and more numerous? That may allow me to set the minimum flow tolerance lower.
Using HEC RAS 5.0.3