May 11, 2014
Statistics
Summary
Triple point/warm front play across southeast Nebraska. Targeted Fairmont area for late afternoon tornadic supercells initiating on the triple point and riding the warm front. Intercepted severe warned supercell near Clay Center noting multivortex tornado under large bowl funnel. Escaped east trying to stay out of path and ahead of gust front. Noted gustnado interacting with updraft base near Grafton. Able to get into inflow notch north of Beaver Crossing noting later confirmed large rain wrapped tornado and satellite tornado. Chased HP gust front structure to Lincoln before heading east for home.
Crew and Equipment
Chase partners: Jennifer Brindley Ubl, Victor Gensini. Equipment: Canon 60D, Canon t2i, Canon EFS 10-22, Canon EF 50mm, Sony HDR-xr500v..
Video
Details
A triple point was forecast over southeast Nebraska, with a warm front bowing north into central Iowa and a dryline extending down into Kansas and Oklahoma. Strong instability in the warm sector and impressive shear profiles prompted the Storm Prediction Center to issue a moderate risk for tornadoes across southeast Nebraska, where storms interacting with the warm front were likely to produce tornadoes. Targeting was pretty straight forward on this chase, and we agreed to head toward Fairmont for ourinitial intercept point, where storms were forecast to fire by mid to late afternoon on the triple point. The only negatives to the setup appeared to be questions about storm mode and storm coverage. Would we be dealing with messy high precipitation supercells that were interfering with each other, or cyclical tornado machines riding the warm front? The morning convection cleared out early, setting the stage for a big afternoon supercell show.
Just before Clay Center we turned off our county highway to watch the storm. The few trees blocking our view cleared up and we were greeted by a huge bowl lowering hanging underneath the updraft base of the storm. The sight was awesomely creepy.
Victor got the updated base reflectivity scan, and the boundary was being pulled into the storm's inflow notch, a clear indication that this supercell had surface based inflow and was interacting favorably with the boundary.
Once clear of the base we stopped to watch the storm from the clear air out ahead of it. Contrast was so low we couldn’t see much of what was happening underneath. We’d have to get back into the inflow notch if we were going to see anything on this supercell.
We started stair stepping east and north on the road grid trying to keep up with the storm and get our contrast back from within the inflow notch. The storm was cycling, undergoing periods of inflow and outflow as it interacted with the frontal boundary to the south. This cyclical supercell seemed to command the environment around itself, rather than being a subject of it. North of the boundary, the hook would extend southward, and the storm’s impressive inflow would draw the boundary north. As if it were alive, the storm would then take a huge inhaling breath, impressive amounts of inflow screaming into the base. There was an eerie calm at the top of the breath, and then the storm would let it go. Huge amounts of outflow would flood out from the storm, the rear flanking gust front surging eastward at impressive speeds. The hook would undergo occlusion and then get drawn north back into the forward flank of the storm. Then the process repeated. We stepped east and north and then east and east as the RFD gust front surged and north and north as the hook occluded. The rapidly surging RFD and turn to the left was not unlike the motion we had seen on the deadly El Reno storm last year, also a monstrous HP, and we were careful to avoid getting caught in it.
Running north near Grafton to try and get into the notch once more before the RFD overtook us, Victor spotted a debris cloud in the field to our west, a smaller circulation with a tube of dust above it. We slowed the van down to a halt to watch it and make sure we were in a safe position. The clouds above the dusty circulation seemed to swirl and twist with it, another tornado. But after a few more moments of watching it, the feature seemed to lose its connection with the base of the storm, with only turbulent motion above it. Other little dust plumes kicked up beside it and we realized we were most likely watching a gustnado, a small, brief eddy that spins up in the storm’s outflow winds. The edge of the gust front hit us with a blast of inflow, but surprisingly we were also greeted by strong vertical updraft winds. Bits of gravel and grass were coming up off the ground, flying into the van up towards the storm. The gustnado was likely being directly influenced and pulled by the storm’s updraft, stretching it vertically toward the base in a kind of gustnado-landspout hybrid tornado. We didn’t count the circulation as a tornado, but it was interesting to see its interaction with the updraft. The gust front starting to overtake us. It was obvious that we weren’t going to be able to get into the notch heading north without getting blasted by the storm, so we turned around for the next east road and started stair stepping again.Then a cone tornado appeared just right of the RFD precip core. It condensed to the ground with amazing speed, probably in a couple seconds or less. It was still partially rain wrapped, but we finally had a more classic looking tornado.
The RFD region containing the large tornado was moving northeast, and while the mass was still well to our south, the forward edge was starting to get ahead of us to the east. The last thing I wanted was for this mass to overtake us, or for us to fall behind it within the core of the storm, so we escaped east out of the notch once more. We moved down the gravel as the rotating mass of rain and wind crossed behind us by about a mile or two. We cleared the core of the storm getting only a few drops of rain from the rear flank.
The massive numbers of spotters and chasers present in the region and the disorganizing, blob supercell:
Several chasers were again impacted by this storm, which in several ways was not unlike the El Reno storm with its huge rain wrapped, HP tornado. A tour van was impacted by a large sprinkler that tipped over in severe winds within the bear’s cage, and several other chasers received damage to their vehicles as power lines came down over them within the rear flanking downdraft.
Conclusion
This chase was a big success for us. Our target verified nicely and we were able to intercept a few decent tornadoes. Ultimately the HP storm made this a very difficult, dangerous even, chase, and kept the tornadoes from being more photogenic. Perhaps if the storm could have anchored to the warm front and rooted to the warm moist inflow south of it instead of transitioning between elevated, outflow dominant states between cycles north of the front, this storm might have been a more visible classic supercell. We were able to safely play the inflow notch on this storm, but we had to be on our toes to take our escape routes to avoid the RFD core with rain wrapped tornadoes and RFD gust front, which several chasers got caught in resulting in damage to their vehicles. The large rain wrapped tornado tracked from Cordova to east of Beaver Crossing, was rated EF-3 and had a maximum width of 1.5 miles, making it very large, yet difficult to see wedge tornado.
Lessons Learned
- Don't core punch the RFD on a large tornadic HP.
- Be ready to take an escape route directly away from the tornado, which does not cross its path, when playing the inflow notch on an HP.