A more widespread severe weather event unfolded the next afternoon, on the 10th, as an unseasonably deep upper-level trof ejected east into the Ohio Valley amidst a very warm and tropically-moist airmass that had settled into the region. With unseasonably wind fields collocated with a seasonably unstable atmosphere, the environment was primed for widespread severe storms. Several linear clusters tracked east through the local area during the afternoon and evening, bringing with it widespread swaths of damaging wind and numerous observed reports of winds in the 50-65 MPH range. There were likely instances of even higher wind that were not directly sampled. The storms produced over 50 reports of wind damage throughout the local area.
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