The 24 August, 2011 event shared both similarities and differences with the 21 August, 2011 event.
Both were tornadic, and both had similar synoptic scale upper-level patterns. Some of the differences included the mesoscale surface pattern and the reactions of the general public, both before, during and after the events.
This time we take a proper top-down look at the setup.
On the morning of the event there is again an approaching upper level jet max, rotating around a large, long wave trough: