While I agree with the overall message he’s attempting to convey, El Reno 2013 and Hollister 2024 aren’t great examples for conveying how misapplied the scale is. El Reno 2013 IMO is very overrated in its intensity to the general public outside of some impressive vehicle damage, and I haven’t seen a single image from Hollister 2024 that even remotely points to a significant EF2+ tornado. Extremely violent tornadoes are fully capable of incredible damage to the ground and trees, and neither of those two did such a thing (El Reno 2013 did have like, one tree that was debarked impressively though). Hollister 2024 literally did nothing substantial on the ground at all, it wasn’t even close to being a violent tornado.
Better examples for this argument are Grinnell and Lake City from this year, and Matador. All three of these inflicted violent damage without a doubt in my mind (Matador arguably inflicted full on EF5 damage for Pete’s sake) yet they were rated EF3. Sterling City potentially reached violent status as well, but I question the validity of that statement TBH.
Sterling city I argue had Ef5 winds, the contextuals weren’t as bad as Matador but were definitely “low end Ef5”.
Regarding Hollister/El Reno 2013, there has been many tornadoes that had deceitfully strong TVS but end up doing comparatively unimpressive damage at the surface.
In reality, tornadoes (particularly wedges) fail to develop a violent core, the vast majority of times a wedge just contains meso vortices; which can be strong in their own right (El Reno 2013 and Greenfield for example).
But due to the nature of meso vortices, the extreme velocities they achieve are simply too brief to do any real damage, which is why many tornadoes on radar look extreme on velocity but DOD is far less despite the fact.
Wedge tornadoes like Smithville, Bridge creek, Bassfield, Piedmont, (just to name a few) are examples of wedges that do contain a violent core, (which I would think looks like a secondary stove pipe shaped column hidden inside the main condensation funnel, that does the extreme damage).
It’s no coincidence that in violent wedges, the area of extreme damage looks like it occurred from a separate smaller tornado inside of the broad damage swath.
A lot of tornadoes that exhibit ef5 level damage look relatively “unimpressive” on radar velocities even while in close proximity, and even ones that do fail to match or surpass other TVS on weaker tornadoes.
This also isn’t a coincidence, violent cores likely do have weaker max wind velocities compared to meso vortices, but unlike those, violent cores are much larger in size and more importantly, last more than a second.