I got a late start on the day and didn’t leave until after 5:30 pm.  By then, several weak tornadoes had been produced by storms near the TX/W OK border.  I targeted one storm that moved northeast across Custer into southeast Dewey counties.  The storm had evolved into a rotating line segment and was rather uninteresting when I came across it.  The photos here were taken near Fay.

I did come across an old farmhouse that I will have to remember for future chases:

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A rather uneventful chase that resulted in quite a few miles making a big loop to the southwest, northwest and northeast of Okarche.  Several storms formed in an area of weak instability and modest low level shear.

My first attention was with storms that formed in Caddo County, but these struggled most of their life before weakening during the late afternoon.  A couple of storms showed a bit more life in Blaine County and I worked my way up through Watonga and Hitchcock observing these.  While they were able to maintain strength longer than most, there was very little structure of interest.

By late afternoon, storms started forming near I-35 from the Kansas border southward to just north of the OKC metro.  These were the strongest of the day but once again struggled to reach severe levels.  I stopped once to observe a storm near Perry that had a lowering on the flanking line, but little in the way of motion:

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Near Guthrie, I put W.O.D. in the air to get a view of the low-topped convection with the Cimarron River in the foreground:

Simple.  Fun.  Thom and I had a fairly small target area over the southwest corner of the state and the atmosphere didn’t disappoint.  We started with a drive west to Shamrock, Texas and then south on Highway 83 to Highway 62 which led us back east into Oklahoma. While near that intersection, we watched a supercell storm gradually evolve out of a cluster of storms that formed near Memphis, Texas.

Environmental conditions favored very large hail production on the day, with only a low end chance at a tornado.   With this in mind, our plan was to stay out of the large hail – grab storm structure shots – and then drop in behind the storm to see what kind of hail we could find.  The plan worked perfectly and we didn’t become one of the many that spent the following day replacing car glass.

The supercell of interest had wonderful structure and moved at an easy to follow pace eastward across Harmon and Jackson counties.

It was after 7 pm when the storm reached the eastern side of Harmon County and we decided to let it pass us into Jackson County.  We had a north/south road that took us to Gould and we decided to use it in our hail search.

It didn’t take long to find large hail.  The swath of hail greater than 1.75″ was several miles wide.  However, our first stop was to check out wind damage that occurred 6.2 NM south of Gould:

It was at this location where we also measured hail to 2.28″:

At 2.7 NM south of Gould, we measured hail to 2.54″:

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Finally, at 2.4 NM south of Gould, we measured hail to 3.20″ (just shy of the largest, 3.33″ that I’ve ever put a caliper to):

This also stands as the largest 2019 Oklahoma hailstone as of this writing.

Another thing of note.  For whatever reason, I had never documented severe size hail in Harmon County.  It was one of the more glaring holes in my chase logs:

I think we can fill that in now….