Last Chance near Last Chance

March 11, 2014 by · Comments Off
Filed under: Summary 

Wiggins to Cope CO
23 Jun 13

SHORT: Remained ahead of northeast CO convection as it metamorphosed from early, fuzzy slop near Hoyt and Wiggins to a supercell-infused squall line between Woodrow and Cope with several photogenic and beautiful scenes.

LONG:
Final chase days of the season usually are known in advance to us, because we tend to take our Great Plains trips near the end of the traditional spring storm-observing season in a fixed time slot. As such, many last-chance chase days are known as such that morning, if not before. They can get sentimental. We focus and reflect on the possibilities with a renewed sense of wonder and anticipation, knowing this is the final opportunity for the season and probably the year (save the opportunistic fall chase that happens once every five years or so).

Northeastern Colorado was the target area, with the old outflow boundary from the previous day’s convection in WY and NEb having settled southward into eastern CO and weakened, leaving behind some upslope flow into the Front Range, reduced low-level moisture compared to the previous day in WY, and weaker (but still sufficient) shear for supercells. Cloud bases were likely to be high, with strong potential for outflow dominance and meager, conditional tornado risk.

Yet these reduced-moisture, upslope-flow days often yield scenic skyscapes festooned with interesting storm clouds of various types–especially if one is patient with often ragged, nebulous early convection and keeps apace until it organizes. Forecast storm motion toward the CO/KS border area also likely would take us toward I-70 and a one-day drive home the following day.

Our weather-dictated itinerary the previous several days had taken us from MT-ND-SD-WY-NEb, where we were starting the morning in Kimball, right by the CO border. It was as if a storm-intercept guide had been navigating us gradually homeward with amazing skies and fantastic experiences all along the journey. How fortunate! And here we were, ready to partake of one more afternoon of beautiful storms on the way home.

Proximity to the target area allowed plenty of time to eat brunch, analyze data, and watch the southwestern horizons. Early-afternoon towers erupting to our SW, in northern CO, were easy to see from IBM, so we cruised easily S to Ft. Morgan and saw the high, fuzzy bases even from there. Continuing SW through Wiggins toward Hoyt, we got a nice close-up view of the virga factories, appreciating the majesty of the High Plains even under soft storms, on scales large and small. Small? Oh yes. We enjoyed watching birds that Elke couldn’t identify hop through the stubbled cornfields of 2012, skittering along at a deliberate clip, pecking away at bugs, seeds, or other material unseen.

Next, we retraced the path back up to Ft. Morgan, then veered southward to get on proper road options that would allow us to stay ahead of whatever would evolve from the growing multicell complex to our W. While doing so, the convection slowly acquired visible, if still high, updraft bases, which gradually grew in areal extent and number along with CG flashes. I’ve seen this before. Usually, in these favorable deep-shear profiles, a supercell will develop unless the entire mass is blasted asunder in infancy by cold outflow. That wasn’t happening; the cores offered only feeble density currents, judging by the lack of proximal dust plumes.

Jaunting off the main highway between Brush and Woodrow, a couple miles down a dead-end dirt road, we found a good place right at the terminus where we could photograph wild sunflowers and a wild storm. Cores grew. Updrafts grew in front of the cores. Inflow strengthened. The whole raggedly beautiful storm pile got better-organized and backbuilt before our very eyes, ears and nostrils, as revealed during a stop just S of Woodrow.

East on US-36 4 miles out of Last Chance, and another mile N on a (barely) paved side road, led us to temporary solitude: us, a photogenic abandoned farmstead and the rampart of storms in the west. Whoa! What’s that back there to the NW behind the old house? You guessed it, brother–not just an old storage building, but a high-based wall cloud and mesocyclone.

Although short-lived, the line-embedded supercell provided some striking, picturesque scenery as it headed ENE, before getting disorganized in favor of other updrafts to our own W and SW. While watching that spectacle, a ranch mom and her kids drove up on an ATV to make sure we were OK; we chatted with them awhile before one of the little ones drove them all back to their house on the four-wheeler. Encroaching storms sent us eastward to the Anton area.

Even though the whole complex was becoming increasingly outflow-dominant in the fading daylight, a marvelous episode of deep twilight blues, slate to marine in hue, sandwiched layers of laminar cloud material to the SWto the Nto the SW again. What a show! At least transiently intense, somewhat supercellular updrafts kept forming along its leading edge, with assorted notches (some rather sparkly!) and other circulations of varying scales.

Admiring the scene, we also noticed that the base surfing outflow to our SW was becoming increasingly circular, quickly. Within less than 30 seconds, and about a mile away (closer than it appears in this wide-angle shot), a small but tightly rotating wall cloud formed from a pre-existing, seemingly benign lowering under that base (annotated version). Quickly, dust stopped then rose beneath. The circulation started to hook toward its NE–right at us. What had been light westerly (but mild) outflow winds backed and accelerated from the ESE. Time to bail out of there!

Although I doubted any substantial tornado could develop in this circumstance, I didn’t want to be the guinea pig to test that hypothesis. Even though we only had to go less than 1/4 mile to get back on US-36 and gun it eastward, we still were not comfortably relaxed–no thoughts of rocking in hammocks beneath Caribbean tiki huts while sipping dewy beverages. Instead, the rising pile of dust, under a small area of cloud-base rotation, with screaming inflow winds, nearly overtook us. I can’t say for certain if that circulation ever tightened into a full-fledged tornado, but if not, it came precariously close.

Just as fast as it formed, deeper outflow from the west crashed through the feature and tore it up, leaving behind a dispersive dust pall over the highway behind us as we gained a few miles of headway. With daylight fading fast and eyelids growing heavier, we watched the mess become more linear and turned S toward I-70, out of the way of all storms. A night at our favorite motel in ITR, lightning flickering off to the N and NE, closed out our 2014 storm-intercept season with a lullaby after the atmosphere’s final flourish.

Driving home the next day, we reflected and remembered. What a season it was…rewarding for us photographically, educationally and spiritually through the unfailingly transcendent experience of wonder and awe before storm-tossed Great Plains skies. The sting of major missed tornado events practically in our backyard was healed during over half an hour of observing from one spot a nearly stationary, violent, yet ultimately harmless tornado in open country of northern Kansas. We made some great memories amidst the solitude of the prairies from North Texas to central Montana. With heavy hearts, we also thought of old friends killed just over three weeks prior by the vaporous forms we seek, on a day when we didn’t head out. Here’s to a safer and much less destructive, yet more photogenic and inspiring, 2014 storm season to come.

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Our PING trail for this day. [PING date is ending date in UTC.]

Buried Tornadoes by the Border

February 28, 2014 by · 1 Comment
Filed under: Summary 

Chugwater WY to Kimball NE
22 Jun 13

SHORT: Intercepted 2 supercells in SE WY, first photogenic, second became dark and nasty HP with about two tornadoes buried inside and barely/intermittently visible. Lightning and photogenic outflow formations with tail end of resulting MCS in NEb Panhandle.

LONG:
Having made a full-circle back to Chadron from five days before, we did a little late-morning photography of abandoned antique vehicles that we had seen previously, then bid farewell to our favorite north-central High Plains town to head SW. We targeted as promising of an upslope-flow supercell scenario in southeastern WY as you’ll ever see, realistically. The previous day’s boundary was shunted southward toward the Cheyenne ridge, flow behind it veering throughout the day to both advect unusually rich low-level moisture upslope (beneath favorably strong midlevel winds) and yield a big hodograph. That moist air rising up the Laramies would do the heavy lifting, with help from hours of sunshine. Since we actually weren’t far away and were leaving before noon, I was as confident in seeing a tornadic storm on this day as any the entire June trip. Slap those hands together, fill the tank, hit the road, and get ready to rumble under some spinning sky.

Supercells rolling off the Laramie Mountains under similar flow patterns and even less moisture have produced delicious tornadoes on several occasions in the last 15 years. For some reason, we (and I, before marrying Elke) had been late to the party for most of them, either missing the tubes or barely catching their end stages. The 2010 Chugwater storm was, of course, a wonderful exception. Even early initiation wouldn’t be a problem, given the long N-S roads of eastern WY and the good visibility away from the E slopes of the escarpment between Hawk Springs and Chugwater.

Over the hills and into Wyoming we went, fueling in Lusk under the midday sun as anvils began streaming off the northern limb of the Laramies. This was early initiation indeed…for which (for once) we were ready! The most vigorous cell, near Dwyer, appeared to be turning right and organizing into a supercell fairly quickly. Fortunately, it was aiming right down US-26 toward the Lingle area, where getting ahead of it would be easy. No wondering what was over the horizon, no driving 150 miles after an early-forming Wyoming storm already in progress! When we got just S of Lingle, there it was, in youthful supercellular splendor, to our W.

The supercell traveled ESE as another developed to its SW, with rain from the newer storm cascading into the established supercell‘s upshear region. After briefly encountering fellow storm observers Vince Miller and Matt Crowther, we moved a few miles S, stopping briefly to watch a beautiful phase of the otherwise shrinking and rising cloud-base configuration, characterized by a clear slot with tightening rotation. Nothing came of that; the occlusion downdraft cut too tightly into the rotation area and dry entrainment eroded what was left. The older cell then slowly weakened at the expense of the rapidly strengthening upshear storm, and we headed S toward Veteran to get in front of the latter.

What we found there was an entirely new animal–one that would turn into a menacing, growling, teeth-baring, attacking beast in short order. Looking SW at the reasonably large updraft area, ragged, slowly rotating shelf/wall cloud hybrid and dense core, it was easy to predict that this beautiful mess of a storm would become an HP in short order. Since the entire storm was moving ESE, this was an unsustainable viewing position; the forward-flank core and its hail would impose its will on us if we stayed put much longer.

A quick zigzag E and S out of the Veteran/Yoder area took us onto US-85 NE of Hawk Springs and NNE of LaGrange. We had to bolt S ahead of the strengthening mesocyclone to our SW in order to take the east option toward WY-151/NEb-88. First, however, we had a few minutes to stop, observe and admire a very rapidly intensifying circulation–a photogenic and menacing wall cloud that quickly evolved into wide, rapidly rotating, nearly ground-scraping bowl, a mesocyclone that clearly meant serious business. A small funnel briefly whizzed around the left (SE) side of the bowl, but with no clearly discernible debris beneath. The entire spinning mass of gas still was moving ESE and we were NE of it. No time to tarry…we had to go!

We skirted the E edge of the orbiting precip curtains from N-S as the mesocyclone quickly wrapped in rain and the storm took on a mean, nasty HP form. I’m used to tangling with those in north TX, but not on the more road-sparse plains of the WY-NEb border. Fortunately the east-151/88 option was conveniently located to offer a chance to get safely ahead of the whirling dervish for awhile, albeit in the eventual path. A brief glance at radar indicated a rapidly tightening and potentially tornadic mesocyclone to our NW as we approached the border. I stopped there to observe and thought I might have seen the tornado (see photos in table below), one about which I was more certain that night, after viewing the photos via camera display and talking with the NWS office. Given its S of E movement, we couldn’t stay too long.

After charging E across the border, after a mesocyclonic cycle, and while I still was driving to gain some distance, Elke took a look at the radar display and saw this rather alarming SRM signature a few miles to our NW. There was obviously another tornado somewhere in that dark precip mass–and likely a significant, potentially violent vortex to boot! It also was moving ESE, meaning we would have to stair-step along the W-E highway in multiple stops to stay safely ahead of it, and of the wrapping precip.

Needless to say, I slowed down really quickly and turned into a northward-directed side road to stare hard into the rotating cylinder of precip. At times, during the second of two different stops along NEb-88, I could make out the tornado ‘s condensation funnel–briefly, barely but confidently. We stopped again after turning S on NE-71 past Harrisburg.

What follows is a chronological table of links to a selection of photos taken at the stops, looking NW at first, then WNW. The photos show the region as it looked with eyeballs (“PHOTO”), heavily enhanced (“ENHCD”) and in a few cases, enhanced and annotated (“ANNOT”) to bring out the tornado where possible, and to illustrate the motion. Curved arrows on some ANNOT images show the area of very intense rotation. All of these were processed within a few weeks after returning and provided to the CYS WFO for their evaluation. [I have them prelim track and time estimates the same night via phone call using adjusted camera times (camera was 4 minutes fast).]

[Please scroll down to see the tornado-photo table and the rest of the post. I don't know how to fix this gap.]
































































Sequence Number & Viewing Location

Normal and Edited Photos

1. 2 W WY/NE Border, WY-151 PHOTO ENHCD ANNOT
2. 2 W WY/NE Border, WY-151 PHOTO ENHCD ANNOT
3. 2 W WY/NE Border, WY-151 PHOTO ENHCD ANNOT
4. 3 E Stegall S Rd on NE-88 PHOTO NO ENHCD NO ANNOT
5. 3 E Stegall S Rd on NE-88 PHOTO ENHCD ANNOT
6. 3 E Stegall S Rd on NE-88 PHOTO ENHCD ANNOT
7. 3 E Stegall S Rd on NE-88 PHOTO ENHCD ANNOT
8. 3 E Stegall S Rd on NE-88 PHOTO ENHCD ANNOT
9. 3 E Stegall S Rd on NE-88 PHOTO ENHCD ANNOT
10. 4 NE Harrisburg on NE-71 PHOTO ENHCD ANNOT

Because the tornado on the Wyoming side of the border (images 1-3) appeared to shrink and get deeply occluded into the precip, and because NWS CYS surveyed a distinct tornado track on the Nebraska side, I now very strongly believe (>95% certainty) that the Wyoming and Nebraska tornadoes were separate. On the Nebraska side–yes, there also was another dark, columnar area to the left (SW or WSW) of the tornado cyclone in a few images (mainly 4-5), but I could not tell what it was. The rotation of precip around the tornado in each photo was furious and obvious. Even when I couldn’t see the tornado at all (which was most of the time), there was no doubt of its presence.

Due to lack of visual continuity, I also can not state definitively if the Nebraska tornado was continuous between stops, or two separate events. NWS surveys indicated one path in Nebraska, so I’ll count this as a single, second tornado for now, given no firm evidence to the contrary. The tornado only hit a few things, earning an EF1 rating due to sparse/weak damage indicators. However, its WSR-88D radar signature is consistent with many strong to violent (EF3-4) events, based on a study underway by Bryan Smith and others at SPC. We’ll never know its true strength.

The tornado moved almost directly toward my position in image 9, but dissipated before it got to NE-71. By that time, we had bailed S, out of the way, and found a hilltop S of the 71/88 intersection. There, we tried to view the deeply occluded, embedded meso as it got thrust back out of the rear side of the precip area (enhanced. There may have been a weak tornadic (or nearly tornadic) circulation still going at that point (enhanced), as visible cloud-base rotation still was reasonably strong. I can’t say with complete certainty. By this time, a big gust front and shelf cloud had surged well ahead of the mesocyclone. The supercell was evolving into a linear structure with more storms erupting to the SW–we had an MCS and QLCS on our hands.

Plenty of daylight remained, so…time to go tail-chasing! We proceeded S to and past Kimball in search of a vantage, and found one 3 SSW of town on County road 28, right along the N side of Kimball airport (IBM). This was a treat! Even though the complex was decidedly outflow-dominant at this stage, its arcus underside and photogenic lightning were just plain fun to observe. The core passing to our N fired a good volume of electrical artillery from the same general area (including one whose most visible segment was “questionable”). One bright outlier, an outflow-influenced channel and a few other strikes followed as the core moved E. Meanwhile, the arcus’ underbelly passed overhead and to the S with fantastic sharpness to its turbulent texturing. What a crazy, interesting sky!

Ravenously hungry by now, and chilling uncomfortably from all the outflow, we snapped the shutters at a few more strikes from the last passing core, then headed into town for dinner. Amidst that huge and expansive puddle of outflow, we didn’t imagine that an updraft would blossom to the E that was surface-based, and produce a brief tornado (seen by a few observers still afield) before being undercut. That’s how it goes sometimes. While somewhat disappointed, we could live with it. We had seen some serious tornadic action already, and the hot pizza tasted mighty good going down. Here was one final look at the back side of the complex from the pizza-parlor’s parking lot, as the storms retreated into the suppertime sky.

After checking into the motel in Kimball, I got the tornado time/track info to the CYS WFO to the best extent possible, then reflected back upon another long but very rewarding chase day–one fruitful both photographically and in terms of both tornadic and nontornadic storm experiences. Forecast guidance also indicated that we had one more day of decent storm potential in CO before we had to head home. Our time in Montana was growing ever farther away in the rear-view.

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Our PING trail for this day. [PING date is ending date in UTC.]

Roundup from Roundup to Roundup

January 21, 2014 by · Comments Off
Filed under: Summary 

near Denton, Judith Gap and Roundup MT
19 Jun 13

SHORT: Fun chase day. Marginally supercellular to linear but scenic storms central MT, with day and night photography.

LONG:
Prologue and Pre-storm Fun
Central Montana had been in our sights for several days as a potential chase target–an ejecting Pacific shortwave trough, negatively tilted and fomenting reasonably strong deep shear, with backed low-level winds into the area of surface isallobaric response–but with the common northern High Plains problem of marginal moisture. Capping didn’t look to be a substantial problem. The strongest deep-layer ascent would be north of the Canadian border in SE AB or SW SK. However, for one, we didn’t have our passports…for two, storms up there would be racing northward and potentially messy, and third, the potential in the corridor between BIL and GTF didn’t look too bad. Low-level forcing looked rather nebulous and uncertain away from the higher terrain, so we decided to cling closely to potential orographic foci–the various ranges NW through SW of LWT, and the Little Snowy Range, a small mountain range sticking up out of the plains S of LWT that is a rarity in the Rocky Mountain region by virtue of being oriented E-W.

Storm observing in Montana is a different experience altogether. While they call this Big Sky Country for a reason, you need the great visibility because paved roads often are very widely spaced and oriented in ways not amenable to staying close to a storm. Small mountain ranges and pockets of forested hills poke out of the vast Plains like islands in the sea of prairie grass, presenting obstacles to both visibility and direct routing from one point to another. Deep river valleys with choppy terrain break up the otherwise decent-quality network of unpaved roads, which otherwise are pretty passable for those of us with high-clearance 4WD. In many areas, you’re 60-90 miles from the nearest services of any kind, and cellular phone coverage is often nonexistent away from major highways. The fuel tank must be topped off at every reasonable opportunity, and the vehicle kept in good working order with knowledge of how to handle minor mechanical breakdowns yourself.

Why chase in Montana? Intercept strategy there must be flexible and humble–two concepts often quite unfamiliar to Okie-style “storm chasers” who love to sniff the vapors and get the “XTREME INSANE” footage. Instead, storms up here are best appreciated from a distance, with occasional sampling up-close as they cross safe roads. That’s fine with me. The landscapes are vast, often breathtaking in their grandeur and late-spring beauty. As foreground settings for skyscapes, or on its own merit, Big Sky Country is a photographer’s delight. Finally, though it is being discovered, chase crowds are far less of a problem here than in the southern and central Plains. It is possible to get off by oneself on a storm and not see another vehicle for a long time.

Roundup is a friendly but rather dormant little town with a few (but just a few) lodging options. Its few restaurants and one grocery store close early, so if you arrive after 9 pm from a chase, you’ll have to eat gas-station food. Bring extra soap, too–the water is wretched: unclear, extremely hard and laden with sediment. We finally found a place on the Plains with nastier water than Odessa! Still, we started the 19th there after the previous day’s leisurely trip up through the Bighorn Basin and BIL. Little did we know that we would end the day there too, making a full circuit through and around LWT.

With storm initiation several hours off, we headed for LWT–a surprisingly picturesque and pleasant town smack in the center of MT, with the Little Snowies lining the nearby southern horizon. The lunch buffet at the Yogo Inn was outstanding–one of the best I’ve had anywhere up and down the Plains–with fast Wi-Fi to check the latest data. The town’s water supply is cold, clear spring water–absolutely outstanding in taste and quality, the very opposite of Roundup’s, and some of the best I’ve ever consumed. It’s one of the few times I’ve had nothing but water to drink with a meal, and loved it. The worst and best water I’ve had on any chase trips are less than 90 miles apart!

Towers gradually developed and deepened to the W as we were finishing up lunch, so we picked up a camera supply piece for Elke, did a brief driving tour of town, then headed N on US-191 to the Carters Ponds public fishing area on the Plains for an unimpeded view to the W. While visually monitoring the slowly evolving convective buildups to the W, we enjoyed the bird watching and photographing opportunities there, along with views of the low range of mountains to the E, and even did some fishing–didn’t catch anything, but it was fun anyway. We had a great pre-storm experience–definitely beats hours spent sitting around some Interstate truck stop!

Judith Gap/Snowy Range Supercells
Anvils began streaming off very distant convection back in the Absaroka Mountains SW of BIL, shrouding the convection to our W and making it harder to see. Still, the darkening of the closer area meant storms were building–an assessment confirmed by a brief window of online radar accessibility. We headed NW on MT-81 across the broad Judith River gorge to the Denton area to get closer, stopping at the abandoned Great Northern Railway car number 902 near Coffee Creek to photograph that and watch the convection to our W.

This was the farthest W and NW we ever have been on a chase trip–due N of eastern UT and eastern AZ! Elke was uneasy to be so far from home–the most distant yet by vehicle alone, a 3-day drive if any emergencies came up. Still, we kept vigilance. The storms took on a more strung-out, linear configuration, running parallel to their NNE-SSW axis of orientation, remaining rather fuzzy and featureless visually, and hugging the E edge of the mountains. This convection didn’t appear to have much of a future except as a quasi-linear mess.

Fortunately, additional storms were firing on the northern tip of the Bighorn Mountains near BIL and well SW of LWT, back near I-90. Plenty of daylight remained at this high latitude, so we reversed course and headed right back through LWT then WSW toward the Judith Gap, stopping along the way to photograph an abandoned farmstead. A supercell became apparent on radar S of Harlowtown, right on US-191 and moving N up the highway toward the W edge of the Little Snowies. We mapped out an intercept strategy to head down 191 and see the supercell before it hit the mountains, and in case the storm right-moved, jump onto what appeared to be a good unpaved road network S of the Little Snowies to watch the whole process.

Popping through the Judith Gap revealed an expanse of plains S of the Little Snowies that bristled with wind turbines–a fitting setting for the approach of a northward-moving supercell (looking SSE). Alas, the storm was being undercut by its own outflow and that of more convection upshear to its S, while moving N. We would have to either: 1) jump E into those unpaved roads to get out of the way of approaching cores with their probable hail and flash flooding, or 2) retreat back through the gap then E into LWT, awaiting whatever was left of the storm as it came over the mountains. We chose the former–but before doing so, managed to shoot a few daytime lightning photos from a high spot just S of the town of Judith Gap.

One captured a CG in the rear-flank core region behind a small wall cloud and RFD slot that soon became overwhelmed with outflow (looking WSW–again these storms were moving mainly N, so turn your conceptual perspective 90 degrees to the left). A few others were shot looking SW as that core passed, and another approached.

What was left of the inflow-notch region coiled back into the mountains to our W, while the base of another marginally organized supercell revealed itself behind still more core to our S. What fun! All this convection was training up a quasi-linear series, just as the earlier useless mush SE of Great Falls; however, this was offering more interesting processes and features.

Zigzagging E and S from Judith Gap to get out of the way, we stopped several times to observe what was left of the second supercell gust out spectacularly. As it did so, the storm veered NE into the Little Snowy Range in scenic fashion, the mountains forcing lift of cold, moist outflow air, the arcus and scud scraping the slopes as it rose. The hard-rightward deviance wasn’t because of convective propagation on the rear flank, but instead, the storm’s surfing its own outflow.

It’s a good thing we didn’t take the LWT option and wait on the other side of the mountains. The storm’s outflow barreled down the north slopes of the Little Snowies and smashed through LWT with significantly severe ferocity: measured 81-mph wind gusts that downed numerous trees in the town where we drank such delicious water several hours earlier.

Southern MT Storm Complex

The supercell having exterminated itself, we turned our attention and our path southward toward Shawmut and the paved US-12. In the distance, bases and cores were forming in several places to the S, SE and E, seemingly all at once, including what was left of the earlier Bighorns convection. Meanwhile, storms pulling off the mountains to our SW, behind the supercell, were growing in size and looking like linear outflow-makers. We were in an island of relative uneventfulness, but far from any paved roads for the inevitable closure of the storm gap SE of Judith Gap.

Before figuring out how to navigate that predicament, we stopped briefly to photograph an abandoned farmstead (main farmhouse and accessory outhouse), then jog SW a bit and view a picturesque, onrushing arcus roll from the trailing storms. While the scene back at the farmstead was a treat, we knew that a lot of storms were going to come together not far from us, and tangling with the resulting complex wasn’t going to be easy. Going E would just keep is on unpaved backroads a lot longer and delay the inevitable. If we headed S, we’d stay in a relative gap for awhile, with maybe some moderate precip, before being engulfed somewhere near the paved road where at least driving would be on firm footing. So it was…

For 20-something miles, we wound generally southward on pretty firm dirt and gravel back roads before reaching the crossroads of Shawmut, and paved US-12. Meanwhile the big wall of outflow that produced the roll cloud had surged out NE, E and SE, raising even more convection into storms–and those began unloading on us right as we reached the highway. The storms to our E also filled in.

With only this option back E, and the text day’s target area somewhere in western-central ND, we were resigned to plowing through (and with) a big blob of convection moving the same direction, all the way to wherever we felt like stopping for the night. We found large branches across the highway in the Ryegate/Lavina area, and PINGed that, while hearing reports of hail and damaging wind in locales ahead of us along the highway. I slowed down in order not to penetrate the worst of the wall of wind and woe.

Right about at Roundup, twilight started deepening, so we decided to stop there for the night. Hailstones littered the ground — some over an inch in diameter, along with broken small limbs; and golf-ball-sized hail had been reported there earlier. Exactly one room was available in town, about 70% below ground level, so we grabbed it and hoped against flooding. The room was actually decent quality–better than we had the night before.

Upon seeing a great, post-sunset mammatus display outside our room window (which was up the wall, at ground level), I wanted to head outside of town to shoot the sky. Elke was very tired, and stayed back. By the time I found a good vantage on a dirt road a few miles NE of town, the mammatus display had smoothed some and moved off quickly in step with what now was a raging, quasi-linear MCS blasting away toward Jordan and Glasgow. Still, in the fast-fading twilight, a blend of in-cloud and distant cloud-ground lightning peppered the eastern and northern sky, as the trailing mid-upper clouds streamed off to the NE. Here is a short animation looking NE that includes the latter shot, and another short time lapse looking E.

This was a long and nontornadic chase day–but nonetheless, very interesting, rewarding and memorable 12-hour circuit around central MT! We slept very well that night, and needed the rest to prepare us for an unexpectedly big drive into southern ND and northern SD the following day.

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Our PING trail for this day.

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