May 20, 2017
Statistics
Summary
Warm front setup in ne IL/nw IN. Targeted Champaign for afternoon low topped supercells with tornado potential. Tracked cell from Hoopeston, IL northeast noting photogenic elephant trunk tornado south of Wolcott, IN. Pursued additional cells until dusk possibly noting brief spin-up south of Monticello.
Crew and Equipment
Chase partners: Anton Seimon, Tracie Seimon, John Allen, Rose Allen. Equipment: Sony FDR-AX100, GoPro 4.
Video
Details
“General feeling is that today is a complex scenario where interactions with the stationary front are going to be key to getting sufficient shear for supercells and increasing tornado potential (SPC has 2% - and based on how crappy their higher probs have been over the past week I like those odds). Deterministic guidance paints the best instability into northern IN, but the complicating factor is the approaching MCS from the west that is currently heading toward the Indiana border. How the models handle this in terms of CAMs differs substantially, with NAM proceeding with a more optimistic dissipation, contrasting HRRRs persistence at least in the southern half of the domain. Given the terrain and favorable environment space, the 12Z HRRR solution certainly looks more in favor of what we are after with a few discrete supercells on the lifting front/ahead of any line west of Indianapolis. HRRR has been trending somewhat westward however and does seem to have a good handle on this mornings MCS. Thus I suggest for an initial target Champaign, IL with adjustments as needed once details become more clear.”
It took several minutes to organize and really get going, but several miles south of Remington, IN as we approached I-65, it was soon quite obvious that a significant cone funnel was hanging beneath the storm. The condensation was reaching for the ground.
6:46 PM
Keep in mind that times on the log remain in Central Daylight Time, even though we had crossed into Eastern in Indiana midway through the chase.
“The joint Duck-Woodchuck survey this morning was highly successful. We first stopped at our filming site, where John and Tracie used photos to determine our various positions yesterday with very high precision. Next, we drove 2 miles to the N-S road serving the farm with the prominent metal silos seen in line with the tornado. We noted that the farmhouse and trees out front appeared to be undamaged, but corn stubble strewn across the front lawn caught our attention. We pulled in the driveway and were greeted by the homeowners, Dawn and Trent Becket, who then walked us around to the back of the house where things got much more interesting. Dawn was home and unaware of the advancing vortex until wind and a freight train sound caught her attention, just as things began to fly around. Among other things we observed: large, heavy trailers were dragged bodily sideways; a motorboat with outboard engine mounted was thrown several meters and flipped over; a shed was destroyed; a broken 2-4 was impaled almost a meter into a plowed field; shingles were stripped from the farmhouse roof, and various objects from the back yard were thrown into the nearby fields. Overall, however, the house itself and most vegetation around it — including plants in flower — came through in good condition. The south side of the house was speckled with corn stubble, with many pieces wedged into seams and rafters. An old van was pushed sideways such that corn stubble and roofing shingles were wedged tightly beneath its tires.
An astonishing find on the southern margin of the property, immediately southwest of the southernmost silo, was a fully equipped and still-functioning Davis weather station! This is operated by the owner of the farmlands surrounding the house, whom Trent called to find out if we could obtain the observations during the tornado passage. John is going to follow up on this.
After assessing the various damage indicators on the property, John assessed the state of the field of corn stubble on the west side of the road. Here he identified a very clear and extremely narrow (1-2 meter width) swath of stubble oriented to the east that lined up with the stubble strewn along the lawn in a path just north of the driveway. Putting everything together, it appears that a micro-vortex swept cyclonically across the property curving around the south and east sides of the house, causing most of the observed damage phenomena in doing so. My take is that the broader circulation would rank as EF-0, but the micro-vortex probably extended this into EF1 range. Other than this single farmstead, we did not find evidence of damage to other habitations. John and Rose did track the path upstream and downstream, and should be able to provide coordinates on estimated start and termination points. “
"Based on the damage alone, I think it would be reasonable to suggest a 75 mph intensity (there are a number of non-DI impacts here which are hard to quantify – perhaps most amusingly the 0.35 mile lofting of the steel patio chair), however the weather station has different ideas. Maximum recorded wind speed for the weather station in the 15-minute binned data (which is all we have at this stage – I’m working on getting better data if it is possible) suggests that the station was located in the outer edges of the circulation, with a high wind speed of 77.4 mph from the WSW which would be consistent with its location on the southern edge of the circulation. "
“A morning MCS persisting from the previous night’s activity moved northeastward through the potential target for Saturday. In its wake, it reinforced a weak warm front draped east to west across northern IL, IN and OH. To the southeast of this front, winds were oriented from the southeast, reflecting significant turn in wind direction with height, and thus producing enhanced helicity, particularly near the wake low-warm front interface. High 60s dew points and moderate instability combined with effective 40 knots shear, providing an environment favourable to the development of supercells, with the expectation that, as cells interacted with the boundary, they would potentially become tornadic. The SPC did not share our optimism, but extended a 2% risk for tornadoes along the warm front and south into the warm sector.
We began the day in Kingdom City MO, where it was overcast but had remained moist. Our initial target was Champaign IL, where we waited until the late afternoon hours eating strawberries and watching cumulus bubble under clearing skies. Initial cumulus was mainly a response to diurnal heating, however a couple of convective rolls oriented southwest to northeast and began to foster deeper convection.
With initial echoes developing, we moved northeast on i57 to position, then east to Rankinand onward, where we drove through the core of the immature cell to position on it’s east side. This cell exhibited a substantial degree of organisation, and shortly thereafter maintained an impressive supercell structure with a classic RFD cut. Stair stepping northeast, we positioned on this cell, awaiting its interaction with the boundary. Through a forest of wind turbines, the cell matured and underwent several occlusive cycles, before we observed a merrygoround of vortices at the cloud base associated with vorticity from the descending reflectivity core. Repositioning once again, a funnel was observed on the interface between the wall cloud and the RFD. From our vantage point approximately 2 miles away, we observed this tornado for it’s ~4.5 minute life, including damage to a farmstead before it roped out in a nearby field.
Continuing to track this cell, the environment became cluttered with a number of stronger cells which interfered with this initial storm. Dropping this cell and moving south, a weak tornado was observed southwest of Yeoman as the storm interacted with the boundary. This tornado rapidly dissipated as we drove onwards south. With convection continuing to grow upscale, we elected to continue south in attempts to intercept a cyclic tornadic supercell near Frankfort, however as we approached through the rain core, the cells began to weaken and grow upscale, and so we instead headed to dinner at Pepe’s for a little Mexican food as the sun set for the night.
Based on the successful intercept, the following morning we backtracked to the area we observed the tornado to identify exact GPS coordinates and track the damage caused. The residents whose land was impacted were kind enough to let us take photographs and answer our questions, and in interviewing them we discovered that, delightfully, not more than 15 metres from where the tornado passed, an automatic weather station was recording data. Following this very fruitful morning, team Duck headed home north.”
“Two thousand five hundred miles slogging it through the Great Plains chasing over-hyped, lackluster events. Garbage storm chasing. That was last week. It’s not just the miles. I’ll drive forever like Forrest Gump can run if the roads are good and the skies are beautiful. But this was neither. This was a grind. Hours were spent in the rain trailing behind the spray of a semi. Then it was racing east and north up the limited paved roads (the sloppy mud roads were out of the question) trying to get a glimpse of elusive needle in a haystack brief spin-up “bird fart” tornadoes. The storms were junky, grungy, grey on grey. The panoramic, epic skyscapes with “violent, long track” tornadoes were not to be found.
Northwest of Great Bend, Kansas we got what I thought for sure would be our best catch of the week: a tiny squiggly line tornado that lasted seconds. The storm had screaming inflow, but it was chill you to the bone cold. It was north of the warm front and stuck behind the lead storm’s gust front, sucking its rain and hail cooled exhaust. I would have bet money that the storm with its laminar inflow streamers and fuzzy black gust front was elevated and wouldn’t produce a tornado. And then it started kicking up several of these small vortices. They were low contrast and lasted seconds, and then we had to flee to get out of the way of the storm. The tornado itself wasn’t the amazing thing. It’s that this cold, gusty, striated beast was producing a tornado at all. It made me think that everything I know about storms and tornadoes is wrong. One of the inflow streamers this storm was sucking up must have had some buoyancy to it. Like a portion of the inflow was warm and not ice cold. Maybe it was latched onto the lead storm’s gust front and we just happened to be north of it at our position. Maybe there was enough buoyancy leftover in the parcels the storm was recycling through its RFD while we felt it sucking stable inflow. Maybe the massive inflow and outflow interfaces were producing so much vorticity the storm was just forcing up tornadic vortices despite the expected thermodynamics not being there. I don’t know, but it totally surprised me. And I should have been happy with that catch. But a brief wisp of a “tornado” doesn’t do it for me and I felt like our high risk, tornado outbreak chase had busted.
Two more days of chasing and we were still trying the warm front for some reason. The next day across Missouri was just utter rubbish with weak watery updrafts with no discernible structure. Adding insult to injury, parts of Kansas we just left were producing photogenic tornadoes in marginal conditions on the back end of the system.
So let’s play the warm front yet again, and this time do it in Indiana, on the fringe of our chase domain, where few chasers would even bother in even more marginal conditions. That’s a great idea, right? It felt like desperation at this point: chasing sloppy seconds across the Midwest on a marginal, 2% day. We were going to see some low topped convection congeal into an MCS and then go home. I could see it coming.
But instead it was the dream we had been waiting for. Convective rolls started to bubble over. We watched from a park in Champaign, IL as the lead tower rocketed up with a pileas cap and we were after it. Despite appearing as little more than a 50 dbz shower blip on the radar, our storm steadily organized into a classic supercell with wall clouds sporting lengthy tail clouds and RFD clear slots. We stair stepped the storm on Indiana’s road grid, a mix of gravel and pavement. It wasn’t quite as nice as the all paved Illinois grid, but compared to Kansas and Oklahoma it was a dream come true. We could cherry pick our position. No watch but the tornado warning had 28 minutes of lead time. Carousel rain curtains, the base wrapped up, nub funnel and then the tornado condensed. It was textbook. We saw maybe 5 other chasers the entire day. I didn’t think our final desperate play on a 2% Indiana day would upstage 15% hatched of Caprock magic and 30% hatched of Kansas outbreak, but it did.
The tornado danced around one farm, sweeping back and forth like a tamer version of the Wizard of Oz rope. You can make out one of the buildings in the foreground. A woman was home, but was oblivious to her lawn equipment and pieces of outbuilding being tossed about until she finally heard the train like roar. She and her house were fine, fortunately. The tornado will likely be rated EF0 or EF1. But it was a beaut. DNA strand like helical spirals twirled around the hollow tube funnel as the tornado danced for several minutes. And then poof, it was gone.
I don't understand the weather or know when the best time to chase is. But I'll keep trying for little moments like these.”
Conclusion
What had started as one of our lowest expectations storm chases ended with one of our most photogenic catches. The Wolcott, IN tornado was rated EF0 having done minimal structural damage except to outbuildings. It’s narrow path width missed most nearby buildings, which was fortunate for all involved, but still offered us a possible candidate event for our research project. I wish we had been a bit closer during the tornado intercept, but our positioning made for great backlighting and the Sony camcorders performed well even at full zoom.
Lessons Learned
- Don’t give up after a string of busts, as the next chase could make it all worth it, even if it has the lowest chances.