Where Qover is the overflow discharge, Lw is the overflow length, C is the discharge coefficient and C=3.0 is used, H is the head over the overflow elevation.
Note: The volume of water that overflows out of the manhole (or catchbasin with no attached downstream gutter) is lost from the system and is accounted for in the "total overflow volume" portion of the mass balance as seen in the Calculation Summary. If you need to store the overflow in the above-surface terrain, you would need to use one of the surface storage options, as explained in the article in the "See also" section below.
(b) Explicit dynamic solver (SWMM)
When using the Explicit (SWMM) solver, it truncates (limits) the node water elevation at the ground (rim) level and overflow is determined by the total inflows minus the total outflows which is based on the enforced node elevation.
Therefore, the SWMM solver will not allow the node water elevation to rise above the rim/ground and the Implicit solver has the node water elevation normally slightly above the ground. As a result, the SWMM solver normally calculates a little more overflow than the Implicit solver.
Both dynamic solvers will handle concurrence of overflow and storage above the ground.
Note: The volume of water that overflows out of the manhole (or catchbasin with no attached downstream gutter) is lost from the system and is accounted for in the "total overflow volume" portion of the mass balance as seen in the Calculation Summary or the Hydraulic Reviewer found under the Analysis Tab. Just select the catch-basin tab and run to see the overflow volume. If you need to store the overflow in the above-surface terrain, you would need to use one of the surface storage options, as explained in the article in the "See also" section below.