Chasing the Great Lakes Superbomb of 2010

Until early yesterday morning, I was pretty certain that I wasn’t going to be chasing yesterday’s squall line associated with the record-breaking low pressure system that’s moving across the Great Lakes. With storms ripping along at 60 knots, what kind of chasing is a person going to do?

Then came the 7:00 a.m. phone call from my chase partner, Bill Oosterbaan, informing me that the Storm Prediction Center had issued a high risk for the area just across the border in Indiana and Ohio. With the rapidly advancing cold front still west of Chicago, we’d have ample time to position ourselves more optimally. This would be an early-day storm chase. It would also almost surely be our last chase for the next four or five months. What did we have to lose?

I hooked up with Bill at the gas station at 100th St. and US-131, and off we went. The storms had moved into Chicago by then, and as we dropped south, it became apparent that we would also need to break east and then stairstep down into Ohio, buying time in order to let the line develop with daytime heating. Satellite showed some clearing in Ohio,

suggesting a better chance for instability to build. Catching I-94 in Kalamazoo, we headed east toward I-75, with the Findlay area as our target.

Off to the northwest in Minnesota, the low was deepening toward an unprecedented sub-955 millibar level, sucking in winds from hundreds of miles around like the vortex in an enormous bathtub drain. Transverse rolls of stratocumulus streamed overhead toward the north, indicating substantial wind shear. (Click on image to enlarge.)

By the time we crossed the border into Ohio, tornado reports were already coming in from the west as the squall line intensified. Soon much of the line was tornado warned. However, while the warnings were no doubt a godsend for a few communities that sustained tornado damage yesterday, they weren’t much help to Bill and me. Chasing a squall line is different from chasing discrete supercells.

We had in fact hoped that a few discrete cells would fire ahead of the line. But the forecast CAPE never materialized to make that happen, and we were left with just the line. In that widely forced environment, tornadoes were likely to occur as quick, rain-wrapped spinups rather than as the products of long-lived mesocyclones. Even with GR3, the likelihood of our intercepting a tornado would require a high degree of luck. It was harder to identify areas of circulation with certainty; I found myself using base velocity as much as storm relative velocity on the radar, and comparing suspect areas not with easy-to-see hook echoes in the reflectivity mode, but with kinks in the line. It was pretty much a game of meteorological “Pin the Tail on the Donkey.”

North of Kenton, we headed west and got our first view of the squall line. For all the hooplah that had preceded the thing, it didn’t appear very impressive. Just your average storm front–much windier than most, but also a bit anemic-looking compared to some of the shelf clouds I’ve seen. Still, it was a lovely sight, watching those glowering clouds grope their way across the late-October farmlands.

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Neither of us was quite ready to end the chase, so with the storm rapidly closing in, we scrambled back into the car and stairstepped to the southeast in the hope of intercepting a likely-looking reflectivity knot that had gone tornado-warned. It was fun playing tag with the storm, driving through swirls of leaves spun up by the outflow. But there really wasn’t much incentive for us to continue the game indefinitely. Eventually we turned back west and drove into the mouth of the beast.

For a few minutes, we got socked with torrential rain and some impressive blasts of wind (and, I should add, absolutely no lightning or thunder whatever). Then it was over. Time to head home.

In Kenton, we grabbed dinner at a small restaurant. Then we headed toward Cridersville, 28 miles straight to the west next to I-75, where there had been a report of “major structural damage” from a tornado. The report was accurate. A small but effective tornado had torn through the community, uprooting and snapping off large trees, taking off roofs, and demolishing at least one garage that I could see. Of course we couldn’t get into the heart of the damage path, but a few passing glimpses suggested that some of the damage may have been fairly severe.

As I said at the beginning, this chase will likely have been my last of the year. I never know for sure until the snows fly, but it seems like a pretty safe bet that I won’t be heading out again after storms until March or April. It’s hard to call this chase a bust since our expectations weren’t all that high to begin with. Plus, tornadoes or no tornadoes, it was an opportunity to engage with a historical weather system. Like other significant weather events such as the Armistice Day Storm and the 1974 Super Outbreak, this one will be given a name in the annals of meteorology. Me, I’m calling it the Great Lakes Superbomb of 2010. In a number of ways, it hasn’t proved to be as impactful as was forecast, but it’s not over yet. And regardless, I’m glad I got the chance to get out and enjoy a final taste of synoptic mayhem.

Intense Autumn Storm System Arrives Tomorrow in the Great Lakes

I’m not going to try to be particularly clever in writing this post. Instead, I’m going to throw a bunch of weather maps and a few soundings at you and let them tell the story.

I will say that the weather system that is shaping up for late tonight on into Wednesday for the Great Lakes has the potential to be of historic proportions. In terms of sea level pressure, I’ve seen a number of comparisons to the great Armistice Day Storm of November 11, 1940. However, there are two significant differences: this storm is a bit earlier in the year, and the forecast pressure has been consistently and significantly deeper. The Armistice Day storm dropped to 979 millibars; this one may be in the 960s. In other words, we may see a record-setting barometric pressure with this system.

The bottom line is, this thing will be a wind machine like few we’ve ever seen. Here’s the current forecast discussion from the weather forecast office in Grand Rapids, Michigan.

LOW PRESSURE IN THE SOUTHERN PLAINS WILL RACE NWD AND PHASE WITH A
LOW OVER THE DAKOTAS AND RAPIDLY DEEPEN AS THE UPPER TROUGH DIGS
ACROSS THE UPPER MS VALLEY. THIS WILL LEAD TO VERY STRONG DYNAMICS
ALONG THE TRAILING COLD FRONT LATE TONIGHT. EXPECT STRONG TO SEVERE
STORMS TO DEVELOP ALONG THE FRONT AND RACE EAST. A 70KT LLJ AND
115KTS AT H5 INDICATE IT WON/T TAKE MUCH TO GET SVR WINDS WITH THIS
LINE OF STORMS LATE TONIGHT. A VERY STRONG PRESSURE COUPLET...ON THE
ORDER OF 6MB/3 HRS WILL FOLLOW THE COLD FRONT. THIS WILL LEAD TO
STRONG WINDS DEVELOPING BEHIND THE FRONT. BUFKIT WIND PROFILES SHOW
MIXING INTO THE 55-60KT LAYER AT 2K FT. IT IS LOOKING INCREASINGLY
LIKELY THAT WE/LL SEE SUSTAINED WINDS AROUND 35 MPH AND WIND GUSTS
OVER 50...AND CLOSER TO 60 ALONG THE LAKE SHORE. AS SUCH WE EXPANDED
THE HIGH WIND WATCH TO COVER THE ENTIRE CWA.

WINDS WILL DECREASE TUESDAY NIGHT AS MIXING WANES...BUT WILL
INCREASE CONSIDERABLY AGAIN WEDNESDAY. THIS IS A SLOW MOVING STORM
THAT WILL RESULT IN A PROLONGED WIND EVENT FOR THE CWA.

I’m not going to add a lot to that, but I do want to mention the possibility of tornadoes during a brief window of time. Hodographs preceding the front curve nicely, with 1 km storm-relative helicity exceeding 300 showing on this morning’s 6Z NAM sounding for Grand Rapids at 17Z tomorrow afternoon. If enough instability develops–and with winds like the ones we’re looking at, it won’t take much–then we could certainly see some spin-ups as the squall line blows through. And if there’s enough clearing to allow discrete storms to fire ahead of the front, chances for tornadoes increase all the more.

With storms rocketing along to the northeast at over 60 miles an hour, the thought of chasing them is laughable. Anyone out to intercept them will have to watch the radar, position as strategically as possible, and then hope for the best. Serendipity will be the name of the game. That game could begin as early as noon here in Michigan, and it looks to be over before 5:00 p.m.

Not the wind, though. That’ll be hanging around for a while.  Batten down the hatches, campers–we are in for one heck of a blast.

Without further ado, here are some weather maps and NAM forecast soundings from this morning’s 6Z run. Click on the images to enlarge them. Just look at that surface low! Pretty jaw-dropping, I’d say.

Forecast maps for 18Z Tuesday, October 26, 2010


Soundings

Grand Rapids, MI (forecast hour 17Z)

South Bend, IN (forecast hour 16Z)

Muncie, IN (forecast hour 17Z)

Multiple Vortices: How Deep Do They Go?

In a recent thread on Stormtrack, storm chaser Shane Adams speculated that all tornadoes exhibit some degree of multi-vorticity. He opened up a topic that has intrigued me for a while.

Just how deep does multiple vorticity extend into a tornado? It may go deeper than most of us chasers imagine. We all understand that many tornadoes display multiple vortices, and a lot of us have witnessed the phenomenon firsthand. It’s possible, though, that the process we call a tornado is a actually an entire complex of vorticity consisting of rotations within rotations. It’s no secret that circulation ranges downward from synoptic scale to mesoscale to microscale; why shouldn’t it continue to do so on increasingly smaller scales? Maybe this concept is nothing new to tornado researchers, but I haven’t heard it discussed to any degree in the general storm chasing community.

While I used to associate multiple vortices with larger tornadoes, it’s the smaller ones that in recent years have intrigued me as I’ve taken a closer look. Some of the more transparent tornadoes have revealed fascinating inner structures, including a sheath-like outer wall cloaking a vigorous center, and a sort of braided appearance that has made me think of the strands that weave together to compose a rope. The 2007 Elie, Manitoba, F5 drillpress is a good example. Check out this video and I think you’ll see at least some of what I’m talking about, particularly around 4:17 into the clip.

Another video of this same tornado, shot at a closer location, offers an excellent front-row view of the tornado as it dissipates. Unfortunately, I can no longer locate that video on YouTube, and I really wish I could, because as I recall, the close-up of the tornado in its last couple of seconds amazed me. The funnel appeared to unravel; for a brief moment, you could see it separate into what I’m going to call vortex strands as its energy abruptly gave out, following which it simply vanished. As striking as how quickly the tornado transformed from a town-wrecker into nothingness was the manner in which it did so.

More recently, I finally got a good firsthand look at extensive, small-scale vortices on May 22 this year in South Dakota. The much smaller, highly photogenic tornado that followed the massive and violent Bowdle wedge was a shape-shifter that went through some fascinating transitions. Parking itself in a field a mile northwest of our vantage point, unobscured by rain, it was beautifully visible and offered a study in multiple vorticity throughout its life. For me, the high point was when the funnel assumed the form of a truncated tube, with delicate tendrils of condensation circulating underneath it one after the other like horses on a merry-go-round. (My thinking is that a pocket of drier low-level air stripped out condensation except in the places where the vortex strands rendered the pressure low enough to make themselves visible.)

In the photo (click on the image to enlarge it), some of the vortices are apparent, but if you look closely, you’ll notice that some of the larger vortices actually appear to be made up of more than one vortex strand. You’ll also see a tendril or two appear to branch off. In all, I’m able to make out eleven strands, ranging from the obvious to the nearly undetectable. Granted, I may be pushing things; my point is that the circulations in this tornado were numerous, varied in scale, and complex. I suspect that there were even more vortices present than meets the eye, but I’m not going to force the issue because I’m no scientist, just a thoughtful observer with an aversion to crackpotism.

If there’s any recent weather-related post on this blog that I hope will draw some solid, informed comments, it’s this one. I’d love to get the opinions of others in the storm chasing community; and while I don’t expect that it will happen, I’d be extremely interested in hearing from those who are actually involved in tornado research.

Sandhill Cranes

The GFS continues to show hopeless ridging throughout most of October. I hardly pay any attention to the long-range forecast models these days, just mention this as a note of idle interest. A trough does finally seem to shape up around 300 hours out per the 6Z run, and it could make life interesting within reach of Great Lakes storm chasers on the 27th and/or 28th. But I don’t have the heart to wishcast that far out; I just don’t believe it’ll happen..

As for the saxophone, I’m extremely pleased with my personal progress. But while I’ve been practicing a lot, my sessions have involved material I’ve already covered in previous posts, and I’d imagine the results interest me far more than they would you.

Lacking anything of great import to write about concerning either jazz saxophone or storm chasing, my radar is scanning for a topic that’s at least conceivably related to either of those two interests. Yesterday’s earthquake in Norman, Oklahoma, would do well except I wasn’t there. I hear it was a loud one, but I’ll leave the reportage to those who actually experienced the shakeup. As for me, I need something closer to home. Like sandhill cranes.

Here in Michigan, now into November is the time of year when the cranes congregate in great numbers in suitable locations that offer nearby sources of both food and cover. Sometime next month they’ll take off for warmer climes in southeastern Georgia and Florida. Meanwhile, this ridging that has quashed the so-called “second season” for storm chasers has provided glorious weather for the sandhill cranes and sandhill crane watchers. The Baker Sanctuary northeast of Battle Creek and the Phyllis Haehnle Memorial Sanctuary near Jackson are well-known staging areas for massive numbers of the birds. However, I’m fortunate to have a location much closer by where over 100 cranes hang out, foraging in a field across the road from a marsh where they shelter for the evening.

Mom and I went out there Sunday evening. It was a blessing to spend the time with my sweet 85-year-old mother, watching the sandhills feed; listening to their captivating, ratcheting calls; witnessing their sporadic, comical, hopping dances; and waiting for them to take off and fly overhead en-masse into the marsh at sundown. Here are a few photos for you to enjoy.

Guest Post: Saxophone and Storms

Every once in a while I like to feature a post by a guest blogger from the worlds of either storm chasing or jazz. Today let me introduce to you my buddy Neal Battaglia. Neal is a tenor man who maintains a wonderful blog on jazz saxophone called SaxStation.com. The site covers acres of territory of interest to saxophonists. If you’re not already familiar with it, then you owe it to yourself to check it out.

After contemplating the nature of my own site, with its odd blend of wild winds and woodwinds, Neal is here to share his thoughts in a post titled…

Saxophone and Storms

By Neal Battaglia, SaxStation.com

Initially, storms and saxophones seemed an odd combination to me.

On this site, I would read Bob’s posts on saxophone, but not always the ones about storms.

However, when I thought about it for a minute, a number of musicians enjoy nature and are inspired by it. And storms are some of the most extreme examples of nature.

One of my favorite trumpet players, Freddie Hubbard, had a record called “Outpost.” The cover shows a lone farmhouse out in a wide-open plain with a storm beginning to brew overhead. When you listen to the tracks, you really hear the movement of the storm–the lead-in to it, the calm in the middle, and the conditions afterward.

My all time favorite saxophone player, Stanley Turrentine, recorded an album called “Salt Song.”  On it is a tune that I like a lot called “Storm.”

These two masters both took musical ideas from many places, reminding me that music is a reflection of our experiences. Your life comes out to be shared with the audience when you improvise on saxophone and write music.

In October of 2009, I took three planes across the country to Nashville and eventually arrived in the backwoods for a “music and nature” class. It was an awesome experience.

The guy in charge of that class recorded an album called  “‘Thunder.”

Nature in general and storms specifically seem to act as a muse for musicians. They are something that we all experience (although possibly less if you’re an extreme city slicker). And music transcends language barriers.  So you can feel storms by listening.

A Real Michigan Squall Line

Man, what a great storm we got last night here in Caledonia! Though actually, I can’t say exactly how it was in Caledonia because I was in my car tracking with the squall line, belting eastward down 100th St in a frenzied attempt to catch up with and outpace the gust front.

I didn’t succeed. Just west of Alden Nash Avenue, a large tree blocked both lanes of the road. Pulling into a driveway, I phoned in a report to KGRR, then managed to squeeze around the treetop and continue on.

Just south of Alto on Alden Nash, traffic was stopped where another large tree had fallen. I turned around and headed east on 76th St only to encounter yet another good sized tree lying on the road. I slid past this one as well, and then, after phoning in another report, completed the big block back into Alto and fueled up at the gas station.

At this point, I had my buddy Bill Oosterbaan on the phone. He was down in Tennessee, but he was following the storm on radar. Since I was chasing sans laptop, I wondered where the line was now located. With I-96 just a couple miles north of me, I had a half-cocked notion that I might still have a chance of catching up with the front of the storm once I hit the Interstate. But Bill informed me that the storm was already halfway to Lansing.

No real surprise there, but nevertheless, nuts. End of chase. Still, there was plenty of lightning crawling the clouds to enjoy. So with my fuel tank replenished, I caught 68th St east and soon found myself once again having to grease my way past a downed tree. Nasty, scraping sound–ugh!

My thoughts turned to Ben Holcomb. Oh, he’d be having a picnic with this system, I thought. Why he ever left this storm chaser’s paradise called Michigan for Oklahoma City I’ll just never understand. Might as well rub some salt into the wound. So I gave him a call, and he told me that he, like Bill, had been tracking the storm front on radar. He informed me that he’d observed base level winds of 88.5 knots on GR2AE. Over 100 mph! Zounds! That, if you please, is one sweet little zephyr. I doubt winds reached quite that speed anywhere on the ground, but we most certainly got one heck of a blow. I’ve encountered my share of trees blocking roads, but I’ve never had my progress consistently blocked by them. Driving through the Alto area last night was like navigating a maze and hitting dead end after dead end.

More weather is on the way later today as a warm front lifts north through Michigan. With 0-6km shear around 55 knots forecast, things could once again get interesting.

Great Lakes Waterspout Season Is at Hand

Now is the time of year when waterspouts start putting in an appearance on the Great Lakes. I had largely forgotten about spouts until a few days ago when my friend and fellow weather weenie Mike Kovalchick mentioned them in an email. Bing! A light blinked on in my head: That’s right! Waterspouts!

I’ve never seen a waterspout. But then, until last year about this time with my buddy Kurt Hulst, I’d never made a point of going out after them. Kurt and I busted that day, but maybe this year I’ll get lucky, provided I increase my chances by taking more opportunities to chase spouts.

I have zero experience forecasting waterspouts. Thankfully, there’s a snappy little graph called the Waterspout Nomogram that simplifies the process. Developed by Wade Szilagyi of the Meteorological Service of Canada, the Waterspout Nomogram provides a quick visual aid for determining when certain critical parameters are in place for four different classifications of waterspout: tornadic, upper low, land breeze, and winter.

The tornadic variety is self-explanatory, and any storm chaser with some experience making his or her own forecasts should have a good feel for when that kind of waterspout is likely. Mike favors the 500 mb cold-core, closed low setup, which to my thinking may be a variant of the first in producing low-top supercells. The remaining two, land breeze and winter, seem to involve different dynamics. For all the waterspout categories, one of the constraints is that for spouts to occur, winds at 850 mbs have to be less than 40 knots, something I find particularly interesting in the case of supercell-based waterspouts.

In any event, I’m hoping that this year is my year to finally witness a spout or two. Michigan chasers and weather weenies, it’s time to pay attention to the marine forecasts. The “second season” can include action right along the lakeshore even when nothing’s popping anywhere else. Make sure you bring your shotgun just in case a waterspout gets too close for comfort (written with a wink and a grin).

An Independence Day Double-Header: Summer Weather Is Here

It’s July 4, Independence Day. Happy Birthday, America! For all the problems that face you, you’re still the best in so many, many ways. One of those ways, which may seem trite to anyone but a storm chaser, is your spring weather, which draws chasers like a powerful lodestone not only from the all over the country, but also from the four corners of the world.

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This has been an incredible spring stormwise, but its zenith appears to have finally passed for everywhere but the northern plains. And right now, even those don’t look particularly promising. That’s okay. I think that even the most hardcore chasers have gotten their fill this year and are pleased to set aside their laptops and break out their barbecue grills.

Now is the time for Great Lakes chasers to set their sights on the kind of weather our region specializes in, which is to say, pop-up thunderstorms and

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squall lines. The former are pretty and entertaining. The latter can be particularly dramatic when viewed from the eastern shore of Lake Michigan, sweeping in across the water like immense, dark frowns on the edge of a cold front. If you enjoy lightning photography, the lakeshore is a splendid place to get dramatic and unobstructed shots. Not that I can speak with great authority, since so far my own lightning pictures haven’t been all that spectacular. But that’s the fault of the photographer, not the storms.

The images on this page are from previous years. So far this year I’ve been occupied mainly with supercells and tornadoes, but I’m ready to make the shift to more garden variety storms, which may not pack the same adrenaline punch but lack for nothing in beauty and drama.

July 4th is a date that cold fronts seem to write into their planners. I’ve seen a good number of fireworks displays in West Michigan get trounced by a glowering arcus cloud moving in over the festivities. But tonight looks promising for Independence Day events. Storms are on the way, but they should hold off till well after the party’s over.  That means we’ll get two shows–the traditional pyrotechnics with all the boom, pop, and glittering, multicolored flowers filling the sky; and later, an electrical extravaganza, courtesy of a weak cold front. A Fourth of July double-header: what could be finer than that?

June 5 Storm Chase: Illinois Tornado Outbreak

We were close to the tornado, roughly a quarter mile south of it, paralleling it as it tore an eastward course through the Illinois fields. Dirt and shredded corn swirled around its base like an aura. As Kurt Hulst and I  pulled aside and stepped out of the car to take pictures, we could hear the roar. It wasn’t loud, just audible and big, very big, an intensely focused sound like an immense blowtorch or a rocket engine. Yet, close as Kurt and I were to the tornado, we were out of its path and beyond the range of any apparent debris, and I sensed no particular danger.

A brief staccato of blue flashes suddenly lit up the base of the funnel, accompanied by a loud bang, and chunks of debris flew skyward and centrifuged out. The tornado had hit a structure out in the field, most likely an outbuilding of some kind.

Fortunately, there was little real harm the twister could do out there in the broad Illinois prairie. Not yet, anyway. But a little way to the east lay Yates City, and two-and-a-half miles farther, the community of Elmwood…

The day had started off rather inauspiciously, with the previous evening’s aggressive SPC outlook degrading into a forecast for straight-line winds. The 12Z NAM, too, looked unpromising, and the RUC corroborated it, with mostly southwesterly surface winds veering with height to a unidirectional, westerly mid- and upper-level flow. A persistent batch of cloud cover from a mesoscale convective system threatened to minimize daytime heating and instability. In a word, the setup wasn’t one that suggested tornadoes.

But with a trough digging in from the west, rich moisture, great shear, and at least a semblance of clearing moving in from the southwest, Kurt and I decided to chance it anyway. Our friend and fellow Michigan chaser Ben Holcomb had alerted us the previous evening to the evolving weather situation, and after reading Friday night’s Day 2 Convective Outlook and scanning the NAM, which showed an impressive juxtaposition of the right ingredients, including high helicities stretching along I-80 from Iowa into Indiana, we knew that we had to go.

So off we headed for Illinois late Saturday morning. As Kurt pointed out, the forecast models don’t always have a good grasp on things. One thing we could tell from both the NAM and RUC, though, was that the best parameters now lay well south of I-80. Accordingly, we set our sights on Galesburg, and once there, we continued on, crossing the river at Burlington and heading west into Iowa.

I took a dewpoint reading of over 72 degrees on my Kestrel at New London. The air was juicy. But the clearing we had driven through in western Illinois was giving way to a an extensive mid-level cloud deck. Rather than continuing to forge farther west toward the cold front, we decided to backpedal eastward in the hope that convection would fire near the edge of the cloud shield. This idea became a moot point as the cloud cover rapidly expanded across the river into Illinois.  But better parameters still lay in our area. We were presently in an area of maximum sigtors and optimal 1 km helicity, and on the radar, a scattering of blue popcorn echoes suggested that localized convection was trying to get started. Anticipating that these features would all translate to the east, we drifted back in that direction.

We soon noticed a cloud base with a tower reaching up toward the higher cloud deck. It showed on the radar, as did another stronger one directly down the road from us. As we headed toward it, the second echo progressed from yellow to red. Not far to our northeast, we could see a rain curtain. Skirting it, we moved east of the developing storm cell, parked, and got our first good look at it.

The cell was organizing nicely and was already showing supercellular characteristics–nice separation of the  saucer-like updraft base from the precipitation core; a strong, crisp, tilted updraft tower; the first signs of banding, and a hint of an inflow stinger. Positioned on the southeast edge of the convective cluster in southeast Iowa, it was in a favorable position to

ingest moist inflow unimpeded by other storms as it drifted at 30 knots toward Illinois.

This was our storm. We tracked with it back across the river, watching it develop, watching the base lower and the first hint of a wall cloud blossom and put on muscle, watching it tighten as the RFD notch wrapped around it.

Just southeast of  Maquon, Illinois, we saw it: a cloud of dust billowing up from the ground with brief, streaming tendrils of condensation forming and dissipating above it. Tornado! It was a brief appearance of maybe a minute’s duration, but the storm was just getting started, mustering energy for the next round.

We didn’t have long to wait. A minute or two later, as we proceeded down CR 8, a slender elephant’s trunk of a funnel probed its way earthward, intensified, and began gobbling its way through the corn, closing in to within a quarter-mile of us before turning straight east.

This turned out to be a beautiful, highly photogenic tornado, all the moreso for the amazing display of lightning that accompanied it. Kurt took some great video of it which will give you a much better appreciation for how

electrified the tornadic environment was. At one point, at the 8:50 mark, you can see a bolt shoot directly from the funnel to the ground. I didn’t have the good fortune to witness the famed Mulvane, Kansas, tornado, but I’ve got to believe that this storm was similar in terms of its incessant lightning.

The funnel morphed through a variety of elegant formations, and the overall storm structure was beautiful. It was a stunning and mesmerizing sight, but with growing concern, Kurt and I realized that it was making its way toward Yates City and didn’t show any sign of weakening.

Fortunately, the funnel veered slightly to the northeast, passing just to the north of the town. At that point, it was an intense drillpress spinning furiously a mile distant. We closed the gap and tracked with it as it headed toward the larger town of Elmwood, just a couple miles down the road.

What was the funnel doing? It appeared to be shifting to the right. Oh my gosh! Elmwood was going to get hit! The tornado was beginning to rope out,

but not in enough time to spare the town. Taking a hard right, it plowed through the town center. Three-quarters of a mile ahead of us, power lines arced and transformers exploded, debris blasted into the air, and a large dust cloud billowed skyward.

It is a weird and awful feeling to witness a community get hit by a tornado. I’ve seen it happen twice before in Springfield, Illinois, and in Iowa City, but those were night time events. It’s different in broad daylight, when you can see what’s happening. The rather blurry photo shown here was taken just before the tornado crossed Main Street in downtown Elmwood. It’s not a very dramatic shot. You can see a few pieces of debris floating in the air and no more than a cloud tag to mark the presence of the tornado. But a second or two after the photo was taken, things got very nasty in that town. If there’s anything at all good to be said about what happened there, it’s that no one got killed or, as far as I’m aware, even injured.

A couple hundred yards south of Elmwood, the tornado dissipated. Gone, poof, vanished just like that. There’s a certain ugly irony about a force of nature that can wreak havoc in a community and then vanish a few seconds later without a trace. If the tornado had dissipated just thirty seconds sooner, a lot of people might have experienced just a good scare rather than a local disaster.

Kurt and I continued tracking with the storm as it made its way toward Peoria. The next tornado soon formed–a larger, bowl-shaped cloud with multiple vortices. This broadened out into a large tornado cyclone with multiple areas of rotation that produced, among other things, a brief but spectacular horizontal vortex. Sorry, I have no photos to show of it. It had gotten too dark, we were moving, and any picture I took at that point would have been blurred beyond recognition.

In Peoria, we got a bit snagged by roads and traffic, but thanks to Kurt’s great driving, we soon found ourselves heading east on I-74. As we crossed the Illinois River, I could see what appeared to be a large cone funnel to our north making its way across what was probably Upper Peoria Lake, silhouetted by frequent strobes of lightning.

Catching CR 115 at Goodfield, we headed north to Eureka, then continued east along US 24. We were still tracking with the storm, which was slowly weakening as the next tornadic supercell to its north began to dominate. It was still no pansy-weight, though, and at Chatsworth, in a final show of strength, it spun down a brief but well-defined rope tornado.

As our storm merged with the northern storm around Kankakee, Kurt and I caught I-57 and headed home. After May 22 in South Dakota, I really didn’t expect that I’d get another decent storm chase in. But this El Nino year, which got off to such a rotten start for storm chasers, now is paying dividends with some highly photogenic tornadoes.

And the season isn’t over yet. There’s no telling what the rest of June may hold. I doubt I’ll be making any more forays this year into the Plains, but if the Great Lakes region continue to light up, I’ve got my camera and laptop ready.

To see more photos from this chase, click here. And while you’re at it, check out the rest of my images of storms, tornadoes, wildflowers, people, and whatnot in my photos section.

May 7, 2010, Northwest Ohio Supercells

Yesterday’s outbreak of supercells in the southeastern Great Lakes was no tornado breeder, but it made for an enjoyable chase. I left Caledonia around 10:30 with Bowling Green in mind as a target, noting that the SPC had outlooked a narrow, northern swath of northeast Indiana and northern Ohio with a 10 percent tornado risk.

I wound up rendezvousing with my long-time chase buddy Bill Oosterbaan in Ashton, Indiana, where Mike Kovalchick also joined us. (Note to self: that Baptist church parking lot on the west edge of town has a fantastic hilltop view to the west.) We dropped south to Waterloo, where I parked my car at a convenience store, then hopped in Bill’s vehicle, and we headed east, watching as a cumulus field began forming overhead. The warm front was moving in, and when we left Ashton, the chilly temps were already rising and bringing the dewpoints with them.

Farther to the east, we hooked up with Ben and Mike Holcomb, and CMU meteorology students Aric Cylkowski and Cort Scholten. Our contingent of four vehicles at the Sonic drive-in made up what was probably the first chaser convergence that Bryan, Ohio, has ever experienced, and probably the last.

From there, we dropped south toward the warm front, which had stalled over the area. Temps had been in the lower 70s in Bryan, with east-northeasterly winds and dewpoints around 59 degrees; farther down the road, at our new location in a parking lot next to a cemetery, we gained another degree of dewpoint and the surface winds veered. On the radar, one discrete cell to our southwest began to take on supercellular  characteristics. We decided to intercept it, and the chase was on.

But another cell formed southwest of our storm, and in its tail-end position, it rapidly evolved into the main player of the day. So we left the storm we were on and headed toward the new one, which was hooking nicely. A couple miles south of the town of Paulding, we encountered one of the most flat-out beautiful hailstorms I’ve ever seen. It moved toward us in shifting, pearly strands across the fields. I tinkered frantically with the settings on my camera in order to get a fast enough shutter speed for snapping pics from our moving vehicle–there was no shoulder to the road, and no stopping–but by the time I finally had what I needed and Bill had found a turn-off, the amazing nuances and texture of the hail shaft had blended into a homogeneous sheet (click image to enlarge). I took a couple quick photos which nowhere near capture the essence of what we had seen just a minute or two prior; then, with maybe thirty seconds to spare from getting cored, we beat a hasty retreat.

Out in the field just to our southwest, we could see a crapload of dust being kicked up by the rear flank downdraft. We pulled aside and let it pass 100 feet or so in front of us. In the photo, notice how the dust fills the ditch to the right. I’ve read some discussions about the wisdom of the longstanding advice to abandon one’s car during a tornado and seek shelter in a ditch. Maybe that’s a best option in a worst-case scenario, but judging from the photo, it looks to me like the wind is doing a pretty good job of invading the ditch. Depending on the depth of a given ditch, tornado-force winds could conceivably just scoop a person up and launch them into the main air stream.

But I digress. The hail and RFD were the highlights of the day. From then on, it truly was a storm chase, and a futile one. With the storm rocketing to the east-northeast at 70 mph, we had a choice of barreling eastward and losing the storm to the north, or northward and watching it vanish to the east. We pursued it longer than we should have, but we had a fun time of it. The roads in that part of Ohio are great, the countryside is flat and open, and overall, the territory is fabulous for chasing. But when storms are moving at such breakneck speeds, the best road grids in the country–and these probably qualify–can’t compensate.

I managed to get a few shots of a cool, bell-shaped wall cloud as the storm moved away from us. Eventually, though, we called the chase off and started on our way back. West of Paulding, we encountered significant wind damage–large trees snapped off at their bases and pieces of outbuildings scattered across the fields at a couple farms. Could have been weak tornado damage, but it was likelier the work of straight-line winds.

I should probably mention the rope funnel that hung down from a small storm as we headed back toward Waterloo. Okay, it wasn’t really a funnel, just evidence of what wishful thinking can do with a snaky-looking cloud.

Back in Waterloo, I picked up my car, hit I-69 north, and headed home.

I noticed that Illinois-based storm chaser Adam Lucio was also on these storms, and appreciated his Facebook comment that you don’t need tornadoes in order to have an enjoyable chase. I wholeheartedly agree. Yesterday was a great chase, particularly for the Great Lakes, and that hail shaft near Paulding alone made my day.

Of course, everyone has been rumbling about the big event shaping up for Monday in the Plains. Wish I could go, but it’s not in the budget. Best wishes to everyone who heads out. Stay safe, get good photos and video, and have fun.