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Enhanced Fujita Ratings Debate Thread

It is indubitably true that we haven't had a storm since Moore 2013 with its combination of intensity and impact on a heavily populated area. It is also true that it will happen again.
 
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Ethan Moriarty posts about Rochelle: He doubles down on EF4, and states that 200 mph was an overestimation and the true winds were about 170-180 mph. Looks like Rochelle is rapidly exiting the "universally recognized EF5 candidate" category - which is a shame because it absolutely was an EF5. Oh well.


Moriarty reminding me of the saying "an expert is a person who avoids the small errors while sweeping on to the grand fallacy"
 
Ethan Moriarty posts about Rochelle: He doubles down on EF4, and states that 200 mph was an overestimation and the true winds were about 170-180 mph. Looks like Rochelle is rapidly exiting the "universally recognized EF5 candidate" category - which is a shame because it absolutely was an EF5. Oh well.


I'm late to this.

Very strange. Perhaps he thinks he's redefining his methodology in general, but this seems less about new evidence and more about a shift in analytical philosophy. I suppose that's fine, but unless you're disregarding the EF scale's own definitions (of course, he would be FAR from the first engineer to do that), 200 MPH - or, to be more straightforward, a rating that basically said "borderline EF5" - remains well within reason for that tornado.



If memory serves me right, the house in question had anchor bolts embedded in a poured concrete basement foundation. There were no significant terrain effects or unusual topo shielding (that could explain "exaggerated damage" or whatever). IF memory serves me right, nearby objects and vehicles also sustained intense damage (again, I'm open to correction). An elevated subfloor oculd introduce some vulnerability, but the anchoring method and lack of widespread failure elsewhere in the structure don't suggest much.



The EF scale guidelines specify that devastation of a well-constructed home with anchor bolts and a basement suggest winds around 200 MPH (fitting with the EF4-5 crossover zone). That is why experts leaned toward the high end, especially because the structure was just totally eradicated. His revised estimate - 170-180?? - assumes a very significant downward adjustment *without clear new evidence.* It's a totally different interpretation. I think that's extremely conservative, to put it mildly, especially without a compelling structural reanalysis. I guess some fluid dynamics concepts have him convinced of something. But I don't think the forensic evidence, so to speak, supports that. The real-world destruction from Rochelle was extremely impressive. I don't see it as "let's reduce the estimate from high-end EF4 to almost low-end."



And, of course, that was far from the only EF4 level damage point on the tornado's path.



Moriarty does a good job overall and produces interesting content. If he's being this, IMO, unduly conservative - and, frankly, almost speculatively conservative - it really makes me wonder about the rest of the engineering type folks in the tornado rating business.



I'm not overawed by theoretical revisionism.



As for the sidewalk, I assume what he's getting at is: approximations of wind speed based solely on surface effects, like the sidewalk, might overstimate actual tornado intensity. That's probably not entirely wrong from a modeling perspective, but using that logic to downplay observed catastrophic damage is .... something. For one thing, the EF scale was supposed to be designed with boundary layer effects in mind. It doesn't just assume a straight 200 MPH wind at ground level, it interprets the effects of those winds. Second, there were multiple indicators - besides the sidewalk - of extreme winds. Third, again, this is essentially overriding the scale in a sense. I also find that sidewalk situation simply hard to explain without violent winds.

A slab of concrete flush with the soil has no structural entry points for wind to get under unless the soil itself is disturbed or the pressure gradient is high enough to, I guess, essentially excavate it. Any lift has to come from pure wind force overcoming the mass and the downward friction of earth. That's gotta be brute strength of a pressure differential or something. There was also no obvious erosion or water damage. The entire ground-level wind field seems to have been strong enough to move a large, low-profile thing against friction and gravity.



Really, I would think that since wind (in theory) decays closer to the surface, the wind must have been even stronger aloft to cause that much force at ground level.



And finally, there are some damages that fit what Fujita said for F5: extraordinary phenomena will occur. Concrete slabs being cleanly moved ... folks, that's not strong, that's EXCEPTIONAL. Downgrading that to 170 MPH using boundary-layer caveats seems like intellectual overcorrection or something.

I'd probably have fewer words if he just left it at "it was a high-end EF4" or something instead of suggesting 170-180.

Edit: please note also: I am not an engineer. I know engineers, and my Dad is one. I was trained in history and political science, and work in agriculture. But I try to think critically and learn.
 
And just you wait till you see this...


Remember when I said that I didn't fully trust Ethan Moriarty because he had "a bit too much ASCE in him"? This is what I mean by that.

Having lurked here before I became a sometime poster, one guy I really like is buckeye. He's an extremely prudential thinker about tornadoes and I highly value his thought.

And even he knows damn well that Vilonia was an extremely obvious EF5/F5. That's ridiculous by Moriarty. Again, I like the guy, but, as Charles Barkley would say, "Come on, man."
 
Here's some EF1 and EF2 DIs in Grinnell that infuriate me, and the "reasoning" behind them:
View attachment 43103View attachment 43104
EF2 - 116 miles-per-hour:
A more recent addition built onto the south side of the house was completely blown away along with the front (eastern) half of the original home. Trees were stripped and vehicles damaged. Images show surrounding properties that also sustained damage.
View attachment 43105View attachment 43106
EF2 - 113 miles-per-hour:
40x60 morton buiIding blown away with damage to buildings. and 20x30 ft Quonset building collapsed. 2003 manufactured home had all walls collapse. Few anchor hooks on foundation. Concrete basement. Storm doors for basement on south side were pulled up. Damage scattered in various directions.
View attachment 43107
EF1 - 110 miles-per-hour:
Garage walls imploded outward with one bolt anchor visible near the garage door. Old vehicle was inside the garage and grey truck was just south of the building prior to the tornado.

This survey angers me. And there's more images I haven't posted, some of which are arguably even worse. And pay close attention to the reasoning - they avoid any mention of the more extreme tornadic damage.
I'm reminded of a line from the Dirty Hungarian Phrasebook sketch from Monty Python

"I wish to plead incompetence, my lord."

I can only hope it WAS incompetence.
 
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I'm late to this.

Very strange. Perhaps he thinks he's redefining his methodology in general, but this seems less about new evidence and more about a shift in analytical philosophy. I suppose that's fine, but unless you're disregarding the EF scale's own definitions (of course, he would be FAR from the first engineer to do that), 200 MPH - or, to be more straightforward, a rating that basically said "borderline EF5" - remains well within reason for that tornado.



If memory serves me right, the house in question had anchor bolts embedded in a poured concrete basement foundation. There were no significant terrain effects or unusual topo shielding (that could explain "exaggerated damage" or whatever). IF memory serves me right, nearby objects and vehicles also sustained intense damage (again, I'm open to correction). An elevated subfloor oculd introduce some vulnerability, but the anchoring method and lack of widespread failure elsewhere in the structure don't suggest much.



The EF scale guidelines specify that devastation of a well-constructed home with anchor bolts and a basement suggest winds around 200 MPH (fitting with the EF4-5 crossover zone). That is why experts leaned toward the high end, especially because the structure was just totally eradicated. His revised estimate - 170-180?? - assumes a very significant downward adjustment *without clear new evidence.* It's a totally different interpretation. I think that's extremely conservative, to put it mildly, especially without a compelling structural reanalysis. I guess some fluid dynamics concepts have him convinced of something. But I don't think the forensic evidence, so to speak, supports that. The real-world destruction from Rochelle was extremely impressive. I don't see it as "let's reduce the estimate from high-end EF4 to almost low-end."



And, of course, that was far from the only EF4 level damage point on the tornado's path.



Moriarty does a good job overall and produces interesting content. If he's being this, IMO, unduly conservative - and, frankly, almost speculatively conservative - it really makes me wonder about the rest of the engineering type folks in the tornado rating business.



I'm not overawed by theoretical revisionism.



As for the sidewalk, I assume what he's getting at is: approximations of wind speed based solely on surface effects, like the sidewalk, might overstimate actual tornado intensity. That's probably not entirely wrong from a modeling perspective, but using that logic to downplay observed catastrophic damage is .... something. For one thing, the EF scale was supposed to be designed with boundary layer effects in mind. It doesn't just assume a straight 200 MPH wind at ground level, it interprets the effects of those winds. Second, there were multiple indicators - besides the sidewalk - of extreme winds. Third, again, this is essentially overriding the scale in a sense. I also find that sidewalk situation simply hard to explain without violent winds.

A slab of concrete flush with the soil has no structural entry points for wind to get under unless the soil itself is disturbed or the pressure gradient is high enough to, I guess, essentially excavate it. Any lift has to come from pure wind force overcoming the mass and the downward friction of earth. That's gotta be brute strength of a pressure differential or something. There was also no obvious erosion or water damage. The entire ground-level wind field seems to have been strong enough to move a large, low-profile thing against friction and gravity.



Really, I would think that since wind (in theory) decays closer to the surface, the wind must have been even stronger aloft to cause that much force at ground level.



And finally, there are some damages that fit what Fujita said for F5: extraordinary phenomena will occur. Concrete slabs being cleanly moved ... folks, that's not strong, that's EXCEPTIONAL. Downgrading that to 170 MPH using boundary-layer caveats seems like intellectual overcorrection or something.

I'd probably have fewer words if he just left it at "it was a high-end EF4" or something instead of suggesting 170-180.

Edit: please note also: I am not an engineer. I know engineers, and my Dad is one. I was trained in history and political science, and work in agriculture. But I try to think critically and learn.
Regarding winds decaying closer to the surface, some new research shows this might not actually be the case, although the sample size of 0m AGL recorded winds is pretty laughable.

edit: forgot to link the survey https://journals.ametsoc.org/view/journals/mwre/152/8/MWR-D-23-0242.1.xml
 
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In the anniversary of the Joplin tornado, I did a reflection of the type of tornadoes we've gotten since then, as well as Moore 2013. I think it's clear that the NWS is saving the EF5 for catastrophic tornadoes in semi highly populated areas such as Jopin and Moore. This is due to highly populated areas having better built homes/structures, compared to cities such as Rolling Fork and Mayfield, where the population is only a few thousand, and instead have the opposite.

I also looked back on RadarScope at the radar signatures that Joplin and Moore had, and I cannot remember seeing more violent signatues on radar around a heavy populated area.

Joplin 2011

1000002196.jpg

This is the radar signature from the Joplin tornado as it went over the city. That is one of the most violent signatures I have ever seen on radar, especially directly over a heavy populated area. It is no wonder why the tornado was able to do such catastrophic damage to the city of Joplin.
1000002201.jpg

Moore 2013

1000002199.jpg
1000002200.jpg
This is the radar signature of the Moore OK tornado from 2013. This storm had probably one of the biggest debris balls I have ever seen on a storm, calculating around 2.5 - 3 miles wide. This is crazy, especially because Moore is about 10-15 miles away from the radar beam. It is no wonder why this storm was able to produce catastrophic damage to the city.
1000002197.jpg

I truly believe that we will not see another EF5 tornado again unless we have another Moore or Joplin type event, such as a devastating tornado hitting a highly populated (50,000+) city head on, producing catastrophic damage.
 
The tree damage and scouring from this outbreak is seriously something else. Very impressive

Edit: I'd be interested in knowing more about the soil composition of Kentucky. How deep are the roots of grasses there? Hopefully someone studies those damage tracks beyond assigning a rating.
 
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In the anniversary of the Joplin tornado, I did a reflection of the type of tornadoes we've gotten since then, as well as Moore 2013. I think it's clear that the NWS is saving the EF5 for catastrophic tornadoes in semi highly populated areas such as Jopin and Moore. This is due to highly populated areas having better built homes/structures, compared to cities such as Rolling Fork and Mayfield, where the population is only a few thousand, and instead have the opposite.

I also looked back on RadarScope at the radar signatures that Joplin and Moore had, and I cannot remember seeing more violent signatues on radar around a heavy populated area.

Joplin 2011

View attachment 43121

This is the radar signature from the Joplin tornado as it went over the city. That is one of the most violent signatures I have ever seen on radar, especially directly over a heavy populated area. It is no wonder why the tornado was able to do such catastrophic damage to the city of Joplin.
View attachment 43122

Moore 2013

View attachment 43124
View attachment 43125
This is the radar signature of the Moore OK tornado from 2013. This storm had probably one of the biggest debris balls I have ever seen on a storm, calculating around 2.5 - 3 miles wide. This is crazy, especially because Moore is about 10-15 miles away from the radar beam. It is no wonder why this storm was able to produce catastrophic damage to the city.
View attachment 43126

I truly believe that we will not see another EF5 tornado again unless we have another Moore or Joplin type event, such as a devastating tornado hitting a highly populated (50,000+) city head on, producing catastrophic damage.
To be fair, that same year, many of the super outbreak storms didn't hit populated areas (rainesville) and still got the rating
 
To be fair, that same year, many of the super outbreak storms didn't hit populated areas (rainesville) and still got the rating
I think part of that reason is because they couldn't spend much time to really study them, including how the houses were built, because of how many tornadoes spawned. I also don't think WFO's were as strict with the EF5 rating as they are now. That's also why I believe NWS offices are saving that rating for when they hit highly populated areas and produce catastrophic damage like Moore and Joplin experienced.
 
I think part of that reason is because they couldn't spend much time to really study them, including how the houses were built, because of how many tornadoes spawned. I also don't think WFO's were as strict with the EF5 rating as they are now. That's also why I believe NWS offices are saving that rating for when they hit highly populated areas and produce catastrophic damage like Moore and Joplin experienced.
2011 probably just set our standards too high. There were also tornadoes in 2011 that got screwed (New Wren, Goldsby etc)
 
My cynical self is wondering if the higher end EF4s we've seen in these outbreaks were given their ratings simply for model/forecast verification, and all the other tornadoes are rated with the typical scrutiny. Does anyone know how the analogs pulled with soundings are classified? What is the threshold between the "tornado"(red) and "PDS tornado" (pink) labels?

It's probably pointless conjecture, but I'm still curious.
 
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