Ragged Roger’s Rage of Rago
20 Jul 9
South-central KS and north-central Oklahoma supercell
SHORT: On the way back from vacation in Colorado with Elke and the kids, observed a photogenic supercell over southern KS and northern OK.
LONG: Faced with a long drive back to Norman and the prospect of a day shift for me the next day, I sleepily pulled out of my in-laws’ place near Broomfield, morning sun in my face, eagerly anticipating late lunch and early dinner in SLN, and knowing that we would be bypassing the central CO and western KS storm potential along the way. We would have to depend on mesoscale accidents and luck to observe anything in the afternoon, when in central and southern KS, near the W edge of a cloud shield left behind by elevated convection early in the day.
As we proceeded E, the elevated storms kept firing across northeast and east Kansas, setting up some differential heating in an environment of favorable low level moisture and at least acceptable deep-layer shear. By the time we commenced to late lunch/early dinner at SLN, a supercell pair already had formed over southwest NEb and began charging S toward GLD — through which we had driven a few hours ago. This would include the storm that bombarded Alnado’s place with 4+ inch diameter hail and severe winds, as well as presenting him with a small tornado visible from his property.
After we cleaned out the Coyote Canyon buffet, I checked a surface map and some automated mesoanalysis data on the I-Phone, and saw a nicely defined, NW-SE boundary from near HUT-WNF, conveniently parallel to the mean wind vector, and collocated with the surface moist axis. That’s a good sign. Cu and TCu bubbled along it, seeming to be a couple hours from any serious mature storm (if ever). We headed S on I-135 in no big hurry, a small cell forming then dying on the bondary S of ICT and well S of us. As we hit Newton, the SW sky erupted with towers, and the ICT radar exploded with echoes near Kingman. A large, rather disorganized looking cluster of very high reflectivity sent a short-lived left split off toward the W side of ICT, while we cruised through town.
Given the presence of that vorticity-laden boundary and all its positive attributes (and positive SRH), we decided to wait at the Belle Plaine service area to see if a supercell could consolidate from the big convective mess, while anvil material spread in a massive shadowy umbrella across the sky overhead. Finally, it did, and we zigzagged WNW from Belle Plaine to take a look. We had a distant view under the storm at the time of the law-enforcement “rope tornado” report near Rago, and didn’t see it. Here’s a wide-angle as we approached, looking WNW from E of Perth.
The storm was moving hard right, toward the SE then SSE — a good sign for storm-relative inflow, but away from the higher SRH and moist axis along the boundary. I suspected its tornadic phase (if it ever existed) was early, brief and finished, and it would be “just” a pretty storm from here on. The storm began hammering the countryside in all directions with staccato CG bolts from the anvil, many miles ahead of the cores and vault. The sizzling CGs igniting several fires, and forced us to stay in the car most of the time until S of the OK border. Knowing it would herd us back toward I-35 and homeward, we chose to stay SE to ESE of the storm and keep observing.
The supercell developed several banded structures on both flanks (as seen from Corbin KS). This included a curious juxtaposition of near-ground smoke pooled along the forward-flank gust front, beneath a convective beaver-tail with a base, sandwiching a chamber of filtered golden light of the sunset hour (here’s that shot).
Meanwhile, with the storm bearing even more firmly equatorward, we found a stopping point S of Corbin near the border, and noticed two plumes of smoke rising into the updraft base (wide angle and zoom shots). These reminded me of the “Wicker smokenado” from the early 1980s that made national TV on Nova. Several lightning-started fires had led to a patchwork of smoke palls in all directions, including this one to the SE that formed a nice angle with the postcrepuscular storm shadow.
We reached I-35, photographing the twilight storm from the rest stop near Blackwell, as it crossed the border. Figuring this storm might not be crawling with live OKC TV trucks at this time of year (for once!), I called the OUN office to provide a field report, letting them know the storm looked flat, nontornadic, forced, and somewhat lofted atop its own outflow — despite the prominent hook and SRM couplet I was seeing on Vance AFB radar.
For once, I was not anticipating the prospective nocturnal light show. See, I performed any photographer’s dreaded blunder by forgetting my tripod on the trip. Most of the time, I improvised successfully by bracketing steadiness — rapid-fire shooting of low-light and/or high f-stop scenes in confidence that at least one shot would turn out sharply during a fortuitously steady time interval. This strategy has worked for me over and over in many other situations, but simply can’t be done with something as ephemeral as lightning.
As I drove, Elke began to marvel at the structure, which assumed the shape of twisted taffy, brilliantly illuminated by foreground lightning. Photos or not, we had to get off I-35 for a look! By the time we got back off the interstate, the storm’s sparking was becoming less frequent anyway, its structures flatter again, which made the challenge even harder.
Bring it on: I stand ready to face any challenge. Somehow, using the top of the car and some hand and finger contortions, I did get off a couple of decent lightning shots, including this one. It’s not as spectacular as some stuff I saw elsewhere from the western supercell, but I’m satisfied to have done the best I could under the circumstances.
The western supercell N of END tempted us, but it was getting late (after 10 p.m.), and I had that day shift the next morning to deal with. Tired from the extensive drive and from the trip as a whole, we simply headed back home, content and thankful to have seen and intercepted a rotating storm in late July. This made the sixth straight month I witnessed a supercell in the state of Oklahoma. How strange is that?
Spring 2009’s Fantastic Grand Finale
17 Jun 9
Northeast KS and South-central Nebraska
SHORT: Outstanding. Two chase days in one. Intercepted stack-o-plates tornadic supercell between Belleville-Seneca KS but missed Marysville tornado(es). Long drive W and N for several tornadoes and spectacular supercell from Buffalo County NE to near York, including 17-minute dusty tornado near Aurora. Let tornado get close enough to hear then backed off. Aurora and GRI got very lucky w/timing of occlusion cycles.
LONG:
Looking at morning data and maps from our lodging in CNK, the forecast scenario looked so clear to me on this day, it almost was frightening in its own right. Play a diurnally cooking frontal zone across south-central Nebraska, with strong heating and frontal lift likely to breach the cap and fire at least a supercell or two before sunset in an environment of very impressive moisture and large low level hodographs. It seemed simple enough: Leisurely wander up toward that nearby target area — say, to HSI, eat a good lunch, and and wait for additional clues and/or storm initiation. And so we did. Then a lyin’, cheatin’, seductive storm intercepted us, temporarily stole our hearts, and almost kept us from our true date with the true love of supercellular splendor.
This really was two fine storm intercept days in one, the first beginning before noon!
Early Elevated Supercell in North Kansas
We left our rooms around 1100 CDT, headed N toward Belleville, intending to grab some fuel and proceed to HSI. DF, Ross and the big dogs were going to get some grub, then meet us somewhere along the way. As we headed N on US-81, still in the forenoon hour, big towers appeared to our NW! They were not far away, and W of Belleville. No problem, mon! We could get a drive-by look at some early, elevated storms around noon, be under their shade to keep the car cool, and if lucky, maybe see some hail.
At our vantage a couple miles W of Belleville, two updrafts initially appeared, and also appeared very elevated, with the typically rippled, undulating character of warm-advection clouds, inflow obviously off the surface. But the left one (quickly lowered toward a laminar feature developing beneath and became dominant. On one hand I was somewhat excited to witness the curious spectacle of what could become an elevated supercell; they’re typically very hard to see unimpeded by intervening low clouds and precip common to such regimes. On the other, I already was starting to get concerned that this strengthening storm could last long enough to become surface based, that it would be in a good shear and buoyancy environment if it did, and that under such a scenario, I would have to make a critical decision (influencing the chase fate of four chasers and two pooches) between this “sucker storm” right in our laps and the actual forecast area farther NW for late afternoon.
Such serious contemplations got interrupted momentarily by the diesel-roaring, slow-moving fanfare of a wide load caravan crawling E down US-36. What on Earth was the wide load, anyway? If anyone can identify specifically enough this curious, round little stone structure and its former function, I’ve got a Dublin Dr Pepper for you.
[Edit: It's a 120-year old stone smokehouse, being moved from its place of construction to the county historical museum. See the comment below. I owe Elke a Dublin, not that she'll consume it. 
]
A few hours later we would see the truck and structure later parked at an abandoned fuel station E of Belleville, while racing back W.
Meanwhile, the laminar band’s top rose and conjoined to the lowering midlevel cloud base, which itself flared into a banded formation. The process looked like building a supercell structure piece by piece, out of an erector set made of play-doh. Elke said, “it sure was fun watching that storm assemble itself.” It was still laminar, still smooth and fuzzy and a tad rubbery in form, but visually and on radar, a bonafide, elevated supercell. As it improved, potentially moving into very well heated and moist air, it also started moving east — away from our late-afternoon target zone!
Figuring we got an early start, and a couple hours’ diversion wouldn’t throw us off track, we headed E of Belleville to watch the storm for awhile. It evolved rather quickly from a pretty but obviously not surface-based storm…
Oh Crap…Not-So-Elevated Supercell Anymore!
..into something not quite so obviously elevated with a rapidly evolving, low-hanging wall cloud rooted in the destabilizing boundary layer, as seen in wide angle from N of Morrowville (and as seen with and by DF). Great. This storm was taking us ever farther off on its diversion, and we were letting it.
The previously pictured mesocyclone died to our NW, and the storm appeared to grow rather high based and disorganized. We began to let it go at Morrowville shortly after 1330 CDT, in plenty of time to get back into our original target area. As the storm got off to our ENE and E, however, and almost out of clear sight, it “jumped flanks” eastward, a new and lower base developed with a wall cloud (distant zoom view looking E), it turned farther rightward and quickly organized into an obviously surface-based supercell on radar. Rats! Decision time…and a tornado warning helped to seal the decision. Maybe we did have time to get back in front of it briefly for another look.
We headed E toward Marysville, hearing of tornado reports just NNW and N of town. By the time we entered the W side of town, about 10 minutes after he last report, an old, back-thrown occlusion was evident off to our N, while the storm jumped flanks again and was spreading a precip-filled RFD from the new mesocyclone across the countryside to our NE. By the time we got ahead of the storm again, W of Seneca, it was very beautifully chambered and lit — but sucking cold air. We measured temps in the low 70s and upper 60s in the inflow, where they had been in the mid 80s before. A fine line could be seen in reflectivity imagery, arching NW from another, newer supercell well to our SE that was headed toward the STJ area. That outflow boundary still was spreading SW and W, while our storm had crossed it and was getting elevated again, this time for good. [I strongly believe the storm briefly became surface based and produced the short-lived tornado(es) as it interacted with the boundary N of Marysville). Time to go!
Westward Recovery to Nebraska and...Tornadoes!
The first chase day-within-a-day now over, the Belleville-Marysville-Seneca storm's (lack of) future now assured, we felt we barely would be able to recover W along US-36, then N from Althol KS into south-central NEb with a couple hours of daylight to spare. Much of any time we made up by driving a little too fast on those wide-open roads was offset by a ticket we all got from a courteous and professional state trooper for 10-over just N of the NEb line, which we absolutely deserved and later paid without protest; in the net, we got to the target area about when we should have, just $69 poorer. There is a lesson in that. As the towers blossomed higher and broader, the anvil backsheared farther, the northwestern sky grew darker, the radar presentation grew more supercellular and we drew closer, I thought, "This storm better be worth that price of admission."
We already had seen one occasionally spectacular, sometimes maddening storm over 150 miles away. This one would become, without question, one of my handful of most favorite storms ever observed.
While we approached from the SSE (from Franklin and Minden) the storm launched its early towers skyward with astounding force, backshearing an anvil and pumping tower after tower thereunder, thereafter. It also took a very short time to attain classical, hook-shaped supercellular appearance in reflectivity, though the low level shear was slower to tighten and organize as we approached. This was good, because right as we first got within view of the base a few miles WSW of Gibbon, there was a small cone tornado already in progress! We hurried legally to get into better position E of the eastward-moving business end of the tornadic supercell, and the first tornado (distant and hazy view) died before we could stop for a photo. Sorry!
As we still drove ENE along US-30 from Gibbon to Shelton, aiming to turn N before reaching Wood River, another tornado appeared beneath a broadening wall cloud. This time I did stop briefly to document it (wide angle and 70 mm zoom), but we still were jockeying for position and a few too many miles away. A couple other storm observers I know were closer, and independently confirmed both of these early tornadoes. At several points during the storm's tornadic phases, I tried to phone in reports to the HSI NWS office, but got busy signals every time. Fortunately, several NWS employees who were chasing on their own time also witnessed the storm, along with plenty of local spotters and non-meteorologist chasers with Spotter Network connections who also were more than eager to share their video and photos online so that it all could be well-documented from almost any conceivable angle and distance.
We were hoping for more tornadic action as we tucked ourselves snug into the immediate inflow region, much closer to the main updraft area; but it took awhile for the storm to reorganize to that extent.
Numerous Cycles, Occlusions and a "Landspout"
From several vantages W and E of Wood River we watched wall clouds come and go, a few rotating briefly between several occlusions, one or two exhibiting lower-hanging, moderately rotating chunks of cloud material, but none seriously threatening tornadogenesis. [The darker puff of material that appears "below" the lowering in the last shot actually was a thick, non-rotating plume of falling precip behind the wall cloud, wrapping right to left through the back side of the mesocyclone.] Although the storm stopped producing tornadoes (for the time being anyway) as soon as we got right into potentially fantastic viewing angles, the variation in occlusion and circulatory regeneration processes was absolutely fascinating, fun and at times beautiful.
Looking WNW, here’s one new, small wall cloud developing as soon as the old one wraps in rain. In this wide-angle view, looking WNW across a verdant Nebraska corn field, the small wall cloud and RFD clear-slot cut through the supercell’s main updraft base, while an old occluded region is cast way back behind and to the NW. A few minutes later, when photographed at 55 mm focal length, the new wall cloud began to get a ragged, bifurcated look, while the old meso occlusion sported a flared, bell-shaped base and a pronounced lowering, as if attempting one last burst of supercellular glory before its demise!
We scooted ENE on US-30 then S on US-34 a few miles, avoiding the stoplights and slow local traffic of GRI, and hoping that any reinvigoration of tornado potential from these mesocyclone cycles would not happen until after the storm passed over town. As we were talking to a local spotter, who was there for the infamous 1980 tornado, we saw a faint dust tube under the base of the flanking line — a non-mesocyclone tornado (a.k.a. landspout). DF and Ross filmed it while I ran back to the car for a different lens than the wide-angle that was affixed to the camera. By the time I got the lens on and got back to my viewing spot, it almost was gone, but still can be seen faintly (super-enhanced crop-n-zoom), as the storm’s rear-flank gust front pushed the bottom of the translucent dust tube toward the left (S). This was a short-lived, inconsequential gnat-fart of a tornado, but it did happen — 2012-2015 CDT, estimated 5-6 miles WSW of Grand Island. Meanwhile, here’s how the supercell appeared at wide angle, as we looked NW in fading daylight, with the newer wall cloud and occlusion area to the right (E) and the older one to the left and more distant (W). The storm clearly was getting better organized, each new meso looking a little larger and more robust than the one before…
A Grand (Island) Transformation — The Phillips and Aurora Tornadoes
Good fortune kindly graced Grand Island and Aurora on this evening. That “magic hour” when inflow still is surface based, but the cooling surface temps lower the LCL, and the low level jet begins to develop and enlarge hodographs, was upon us. The storm politely waited until exiting GRI to respond to its improving proximity environment in an amazing way, then obligingly shut down its resultant ravages right before it reached Aurora.
Knowing that the best photographic contrast for low-light conditions would be to silhouette the base, we decided to get due E of the strengthening mesocyclone — by exiting I-80 at state road 2, then marching E on US-34 in step with (and just ahead of) the supercell. The strategy was deliberate, and for once, worked like a charm!
As we cruised E on 34 near Phillips, with Elke now driving, I turned to look out the window, saw a broad but strongly rotating funnel cloud behind us, and hollered for her to stop fast. I got out and shot this wide-angle of the broad, conical protuberance beneath outstanding storm structure. We were too close to get the entire storm in either of our wide-angle lenses, but the view looking WSW wasn’t bad either!
Intermittent dust whirls began to appear under the funnel as it tapered and lowered…tornado! The condensation tube coiled itself into a striking scorpion-stinger appearance, shown here in a zoom and also as part of a wide-angle structural view via Elke’s 17 mm lens. The tornadic meso was moving east toward us, and we weren’t far from it. This non-trivial challenge precluded setting up a tripod in the declining light, and I didn’t want the added noise and grain of high-ISO given such high dynamic range across the field of view. So instead I braced myself well and practiced blur-bracketing, i.e., shoot rapid-fire like hell, and trust that at least one photo within any given magazine-clip of attempts will be steady and sharp. Fortunately it worked when it counted. Most of my images of this and the next tornado were shot at anywhere from 1/20 to 1/6 of a second, hand-held!
The Phillips vortex lasted 5-6 minutes, but only a couple of minutes as a recognizable tornado. Suspecting another would follow, we zoomed east to allow the storm room to move and recycle, which didn’t take long. As we cruised farther E (sound familiar?), another funnel formed, a separate and distinct event from the one before, and I hollered, “Stop…another one!” We pulled off the road and watched the new tornado raise its own dust plume, while a peculiar column of rising dirt jetted up from a plowed field just to its south. Annoyed by the parked car with headlights blasting into my viewfinder and messing with the exposure settings, I ran across the street to shoot as the southern dust plume dispersed and the tornado kept plowing eastward toward our position. [If the dude who was running that car sees this BLOG, here's a belated and hearty thanks for turning off those lights after I hollered at you.]
With escape options N, E and S at our crossroads between Phillips and Aurora, and vigilance for satellite vortices, I felt comfortable letting the expanding tornado get within 1/2-3/4 mile, close enough to hear the whooshing sounds as it churned through that field. It was the first time since 28 March 2007 (Hedley-McLean TX) I had been close enough to hear a tornado, and the most audible one since the 16 May 1991 Haysville KS event.
Hoofin’ It toward a Tornado
Nigh time to bail east again, we headed about the equivalent of a city block past the railroad crossing 1 mile W of Aurora to put some distance between us and the oncoming tornado, and to prevent being barred from escape by a train (just in case). Unfortunately, that also put the elevated light standards of the railroad crossing smack-dab across my view of the tornado. Already out of the car, I asked Elke to back it up to the E edge of the tracks. I then took off in an all-out sprint up the road, across the tracks and straight toward the tornado that was moving toward me. Somehow this felt neither dangerous nor frightening, but quite natural and whole and good. Of course, it helped that the escape machine arrived 40 feet behind me as I set up to shoot another photographic magazine-clip, which now yields one of my all-time favorites among my rather limited tornado portfolio. Even while bracing and shooting, I thought of how that scene reminded me of the content and composition of those old-time tornado pictures that graced the inner plates of Flora’s Tornadoes of the United States and Battan’s Nature of Violent Storms — the silhouetted vortex spinning over the road, looming ominously, trees and/or low buildings on one side or another to add texture to the foreground. I grew up on photos like those in the monochrome books of yore, and now I was privileged enough to be in position to capture one.
I’ll always remember the sound of that scene too — there was none but a light breeze, just outside the mesocyclonic surface flow. The road was devoid of traffic for a few amazing minutes. Aurora police blocked traffic coming westward from town (behind me), and the chaser caravans hadn’t arrived yet. I almost could have heard a pin drop, and certainly a train coming, even though the tornado was at peak size and only a little over a mile away.
Winding Down a Fine Storm Day
We headed through town promptly so as to not be caught there when the tornado arrived. I’ve often heard sirens blaring in towns while storm observing, but very seldom with a bonafide, obvious, mature and robust tornado bearing down. That made the experience finally frightening — not for me personally, but on behalf of the townsfolk, who were well-warned but whose lives appeared soon to be altered for all time. Fortunately it never hit Aurora. The vortex turned left (N) and crossed the highway before it dissipated in the twilight, sparing the town (the lights in the last photo), 18 minutes after genesis. Subsequently, the supercell appeared to become more cut off from boundary layer inflow, though it kept some spectacular structure (wide angle, and even wider angle) for a short while after dark, as it approached York.
At some point during our eastward trek ahead of the Phillips-Aurora tornadoes, I saw DF (who already had an injured back) hanging out his vehicle’s passenger window to shoot video, and hoped all the subsequently inevitable pain would be worth it! Ross was overjoyed as well, and I was thrilled for them both. They had gone through a great deal of trouble, effort, expense and literal pain to be there, and deserved the majesty of the tornadic supercell experience that unfolded.
It was a long way and a long day from that strange, truck-pulled edifice back at Belleville. Two gorgeous supercells, several tornadoes and an Applebee’s steak dinner later, we went to sleep very content with the best chase day in a long time, and a storm intercept season made very good after all. Even a stormless bust the next day in northern Iowa couldn’t dampen the satisfaction of hard-earned accomplishment, sprinkled in no small measure with good fortune of having the right vacation timing to experience a magical June of both supercells and tornadoes on the Great Plains.
Until next season…
Bad Timing in Brush
13 Jun 9
Morgan County, CO
SHORT: Intercepted briefly tornadic supercell near Ft. Morgan and Brush CO that evolved out of nondescript storm band.
LONG:
We left the DEN area about the time a severe storm rolled out of the adjacent mountains toward Broomfield. At the time we still were undecided as to whether to head to a distant and receding storm in SE WY moving into an apparently better environment near the NEb border, or stick around northern CO for the closer activity and hope conditions (namely low level shear) would improve with time in the projected path.
We hit Greeley, the no-turning-back point, and decided it would take at least 2.5 hours to get to the area where the WY storms would be in west NEb, if they still existed. So…instead, we chose to go E to get ahead of the discretely propagating multicell cluster slithering NE out of the Colorado metromess.
We set up about 15 NE of Brush to give the convective slop to our SW and W time to evolve, then pick a “best storm”. For a long time, the storms looked like speckled, disorganized rubbish, nothing rotating, or with only brief, short and weak bouts of cyclonic shear. Cells developed overhead and moved N, merging into a band that extended from NNE-WSW of us. Meanwhile a promising looking cell formed to our NE on the CYS Ridge, closest to the maximized 0-1 km SRH, and tempted us…until it took a hard left turn and started charging due N past SNY. All these storms had low cloud bases for Colorado, and the farthest ones looked more distant than they were.
We spent an hour or more of waiting for all these junky looking storms to do something, while petting a friendly quarter horse and feeding it green grass and apples. Finally, we noticed that the southwestern cell in the band (WNW of Ft. Morgan) started to sport a base with persistent scuddy lowerings. It also began showing cyclonic shear in lowest-cut SRMs. Off we went!
By the time we got to our first vantage near Brush, it had a pronounced supercell look, with tail-cloud banding, and intermittent, small wall clouds near the notch area. At times the structure was classical, but not as wildly sculpted nor brilliantly contrasted as the Arkansas Valley storms a couple days before. Photogenically, this supercell was underwhelming. It lay constantly under heavy anvil canopy, with junky storms upshear. Little occlusions and wall clouds came and went, a few with fairly rapid rising motion and/or cyclonic shear at cloud base.
Several crappy showers formed in the inflow region, atop us, and rained within already cool-feeling air. They dropped the sfc temps to the low-mid 60s F, and appeared to mess with the Ft. Morgan storm’s morphology for awhile, cycling down the wall cloud production and giving it a flat, strung-out and cold looking base. But then those stupid showers drifted off to the NE, and storm organization improved again.
We observed and took photos of the storm for two rather long periods of stops near Brush. I’ve got photos up to 1844 MDT and beginning again at 1914 MDT, although we had a good view of the storm for all but a few minutes in between while driving and hunting for vantage. Those few minutes? The time of Bill R’s and Scott L’s tornado observation matches the short interval we were passing through the town, repositioning to get closer; therefore, we didn’t see the tornado.
Afterward, we were closer, watching a series of quick occlusions and RFD cuts interspersed with rapid cloud base motions. At one point, a needle funnel appeared for maybe 20 seconds (driving…no photo), and one or two other ragged but at least weakly rotating funnels showed up later. At no point after 1914 MDT did we see firm evidence of a tornado, though we saw a few brief episodes of strong cloud base motion while we drove essentially abeam of the storm, up US-6, NE of Brush.
It was getting dark, and the new anchor storms to our SW looked like outflow-dominant garbage (despite the “law enforcement” report of a funnel therewith…cop probably was psyched out by the earlier, legitimate storm). The anchor storms barfed a cold load, estimated outflow winds of up to 50 mph blasting past the windows where we ate dinner at Brush.
Too tired from a long day of car repairs, laundry, phone calls home, and chasing, we decided not to go back to DEN for the night, only to head back out at least as far E the next day.
Instead, we snagged a tax free room at a cheap motel in the area. I love that kind of deal. The old man at the desk was funny: “The rate’s $40 plus tax with a credit card, or just $40 with cash.” Well then, we agreed…hell with the tax man! Unfortunately, their advertised “Hi-Speed Internet” didn’t work at all, so I used my I-Phone for online stuff. I love the device, but no way am I writing any posts from that…too awkward — “keys” too small, fingers too big.
As lame as things looked for the longest time, I was glad to salvage an interesting supercell with cyclic occlusions and funnels, and chalked up missing the brief tornado to just another instance of what’s happened several times before. I’m accustomed to it. I would have been more upset missing a sig-event, which clearly this wasn’t. If the storm hadn’t ingested that rainy air from the junk showers, I’m convinced it could have done more, sooner, and for longer. We were farther E and had stronger sfc winds than the other chasers I know, for much of the supercell’s pre-tornadic lifespan; and it seemed the main inflow channel was E of the storm.