I was looking at archive from RadarScope. It costs like $15 per month for the Pro version, but I only upgrade before a good event then cancel the next month. That's cool that thomp2mp found a site that offers it for free.
It looks like there were broadly rotating supercells out ahead of the main downdraft / wind-shift line that was moving south. The data shows rotation passing over the area, but it looks like its mostly ahead of the downdraft where the damaging winds are shown coming from the north. Was there two different events, one from the south, then another from the north? The exact time would be helpful.
I think if there was a tornado in your area it was probably a shallow gust-nado type that the radar might not detect. The way the line was absorbing rotating elements definitely gave the wind a boost in some areas. The Williamston and Comstock Park tornadoes were both a result of downdraft-dominant segments catching up to and absorbing supercells. I normally think cell mergers are not helpful for tornado formation, but in this case it looks like they caused a temporary boost. The mergers did limit the track lengths though, thankfully. There probably was enough shear and overall energy for a major long track tornado if a more discrete cell had formed somewhere and remained separate.