A widespread outbreak of severe thunderstorms and tornadoes affected the Plains.  An argument could be made for several different target areas from South Dakota to Oklahoma, but it made the most sense for us to stay close to home.
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A monster supercell developed over Custer County in Western Oklahoma.  This storm spent several hours tracking east, and then east northeast before weakening near the Arkansas/Missouri/Oklahoma border.  We observed hail to about 5 inches in diameter with the storm in its early life.  We ended up seeing a couple of weak tornadoes in Canadian County, but the largest tornadoes were buried deep in rain and out of our view.  Incredible supercell structure was observed across Canadian County.

Video capture of the tornado illuminated by lightning.

VIDEO: http://www.youtube.com/watch?v=KF34C59g4mo

Intense supercell storms formed across Southern Kansas during the afternoon and evening of May 12th.  There were several tornadoes produced across Harper County with different storms.
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We approached the area from the north, having chased in Nebraska the day before.  The target area was fairly small, but quickly became cluttered with numerous storms.  We first observed storms near Pratt and Sawyer, while hearing reports of many tornadoes from a storm to our south.  We had made the decision to try and catch up with the southern storm, which ended up putting us in good position for a new storm that formed southwest of Attica.

It was after dark by the time this storm began producing tornadoes, but we had good visibility and a good east/west road to operate on which made for a nice intercept.  The tornado which formed about 6 miles east southeast of Attica was on the ground for 13 minutes and four miles.  It stayed to the east and southeast of us and was only seen with lightning flashes.  While feeling safe at our location, it still made for an eerie experience only being able to see the tornado with lightning.

VIDEO PART 1: http://www.youtube.com/watch?v=A4oxyGPmmQg

VIDEO PART 2: http://www.youtube.com/watch?v=gFylAp5osv4

Looking back, I’m not sure I would pull the trigger on chasing (from Oklahoma) if this same setup were in place today.  There was an upper low over the Western U.S. with decent 30 to 40 knot flow spreading over Colorado.  Low level moisture was returning on upslope flow and it definitely looked like a day where you could get some supercell storms.  If I was in the area on a chase trip I would be excited about the days potential, but I don’t think I would make the drive from Central Oklahoma for it.

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The supercell that was responsible for the tornadoes northwest of Limon was an interesting one.  It spent most of its life slightly stretched out from west to east and usually had more than one – sometimes three – meso-cyclones.  The tornadoes that were produced moved generally due north, resulting in paths that were parallel to each other, but with a progressive farther north latitude.  The tornadoes would tend to move to the northwest near the end of their lives.

In retrospect, it was a privilege to have been able to view this supercell.  It would have been nicer with about an hour more of light, but still very impressive none the less.  I saw very few storm chasers, but it did put on quite a show for the locals.  As I was driving north out of Limon, there were yards full of people in lawn chairs that were viewing the spectacle.

It should tell you what kind of day it was when I went to the SPC storm events browser and found they didn’t have a page for April 6, 2004.
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An upper low over West Texas moved northeast during the afternoon with strong flow and cold air overspreading a region of 50 dewpoints with CAPE around 1000 j/kg.  Several low topped supercells formed and I observed at least three different storms near the Red River, all with typical supercell features.  Wall clouds with slow to moderate rotation were common.  The storm which ended up producing the weak Hollister tornado formed near Oklaunion, Texas and moved northeast around 15 mph.  The tornado itself didn’t appear to be more than 20 to 40 yards wide.  I think it made the SPC log as having a width of 10 yards.  It was on the ground for two minutes.

VIDEO PART 1: http://www.youtube.com/watch?v=LKkOg-t1cpM

VIDEO PART 2: http://www.youtube.com/watch?v=dYk8kG1v0ms

VIDEO PART 3: http://www.youtube.com/watch?v=fY0ETbJJeGc

VIDEO PART 4: http://www.youtube.com/watch?v=RXsxERkrDuk

VIDEO PART 5: http://www.youtube.com/watch?v=KRzwf9IriHI

VIDEO PART 6: http://www.youtube.com/watch?v=K76RIfyGEbI

VIDEO PART 7: http://www.youtube.com/watch?v=MZGMTUILz60

VIDEO PART 8: http://www.youtube.com/watch?v=8wuO-flXqcQ
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One crazy day.  Before it was over, 15 tornadoes were observed.  All shapes, sizes, intensities.  Two tornadoes during the 5 o’clock hour, three tornadoes during the 6 o’clock hour, four tornadoes during the 7 o’clock hour, six tornadoes during the 8 o’clock hour.

I woke up in O’Neill, Nebraska, stepped out of the motel room and it just felt like a tornado day.  Dewpoints in the 70’s had returned to Northeast Nebraska and were being ushered up into Southeast South Dakota on stiff southeast winds.  A well timed short wave trough would move across the area later in the afternoon with 50 knots of wind at 500mb.  I figured one would really have to screw up to not see something, but screwing up wasn’t in the cards.

I left O’Neill and took my time driving, crossing into South Dakota at Springfield.  I made it to Parkston when a storm started developing to my northwest.  The hard part was over.  Two photogenic tornadoes were observed with this storm near Mount Vernon between 5:12 and 5:35 pm.  The storm held together, but was ragged as it continued to move northeast.  Around 6 pm, the storm was still struggling but a new storm was developing to the west northwest.  Soon after I started toward that storm, a large tornado formed and moved by Woonsocket, SD.

There were a couple of weak tornadoes produced just north of Artesian just before 7 pm, and another at 7:16 pm near Cavour.

All of this was just build up to the main event.  At 7:27 pm, a tornado developed southwest of the tiny town of Manchester, SD.  This tornado became very large – 1200 yards wide – as it clipped the edge of the town and moved north for several miles.  It was easily the most impressive tornado of the day.

Despite the storm shrinking in size and not really looking all that great on radar, it continued to produce several other tornadoes – some quite photogenic – as it tracked near Desmet and Erwin.  The show kicked off at 5:12 pm and the last tornado weakened at 8:35 pm.

I’m sure other tornadoes occurred in the area, but by this time the entire area was being blown up with widespread storms – embedded supercells – wind damage producing line segments – and it was getting dark.  It was time to flee the area and it took some good nowcasting by Doug Speheger to navigate me through a mine field of bad storms.

When I finally found a safe hotel, the only room they had left was a suite.  I figured if there was ever any day that deserved it…

Lorraine Evans and I sat in Southeast Wyoming most of the afternoon watching numerous areas of building cumulus.  Most of the attempts looked rather pathetic, with a few getting to the point of producing precipitation before weakening.  Shortly after 8 pm, one storm did take hold over the far northwest corner of Nebraska.  We approaching the storm from Wyoming on Highway 20 as it steadily looked better and better.

We made it to the south side of the southward moving storm a few miles south of Harrison, Nebraska and realized that the storm was really starting to take shape.  The lowered updraft region was broad and had good inflow.  A wall cloud/tail cloud had developed and we were observing strong cloud base motion.

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After getting south of the storm once again, Lorraine looked back to see that a tornado was developing.  The tornado lasted about 9 minutes, stuck out of the south side of the updraft on the southwest side of the storm.

VIDEO: http://www.youtube.com/watch?v=dtZs0X8i7GU

A significant outbreak of severe thunderstorms and tornadoes was expected on this day and I drove up to Topeka the night before.  I was in pretty good position to start the day, but initial development was cluttered with many storms and rapid storm evolution.  I got myself stuck around Saint Joseph while a tornado producing supercell organized and moved across the northern part of the Kansas City metro area.  I fell in just behind this storm and came across large hail and tornado damage, but bad roads and quick storm motions kept me from staying with that storm.
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There was a brief time that I thought I may have missed my chance on the day, but other storms were forming south and southwest of Kansas City that would be in play.  I worked my way southeast of Kansas City and saw a couple of tornadoes with a storm near Chilhowee, Missouri.  The storm was a small one and very well isolated.  I was finally able to get into a good viewing position to the southwest of Knob Noster for the most significant tornado with the storm.  This F2 tornado was on the ground for 5 miles/7 minutes.

One more brief tornado was observed near Sedalia before the storm started weakening.

VIDEO: http://www.youtube.com/watch?v=1ZeBK4iOS7Q

A lot of storms were scattered around Southwest Oklahoma, and we managed to land on one of the better ones.  We spent a bit of time hanging around the airport at Hobart as a supercell organized just to our west.  This storm began to produce a tornado to the east of Hobart just before 3 pm.  We were initially hampered by a dirt road while getting blasted with strong RFD wind and golfball size hail.  Things smoothed out for us after we reached an east/west paved road east of Hobart.  This made viewing the second tornado nicer.
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The second tornado formed about midway between Hobart and Gotebo, and it was on the ground for 12 minutes.  While it curved away from us during the late stages of its life, we had a nice vantage point and decent contrast for video of this very dynamic tornado.

We almost blew this day completely.  We felt sure that storms would form in Kansas, but that others would develop southward into Oklahoma.  We sat in Gage for 45 minutes or so, evaluating the sky and listening to reports of tornadoes coming from the Kansas storms.  Finally, we had had all we could take, pulled the plug on Oklahoma, and starting driving toward tornado producers in Kansas.
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The show was almost over, but had one more tornado in it as we arrived near Kingsdown.  The tornado was classic looking and on the ground for seven minutes.  After that, the storms had some merger problems and outflow under cutting issues.  We spent the rest of the time in the area playing with hail cores where we found stones larger than baseballs.

VIDEO: http://www.youtube.com/watch?v=m_fuB3Xt6J0

My friend, Steve went on three storm chases with me.  His first was a trip to Northwest Oklahoma that was a complete bust.  His second was a trip to Southwest Oklahoma that saw some severe thunderstorms.  Natural progression meant that we should ramp it up to some supercells on this chase, and we did.
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The day was a fairly classic May dryline day across the Plains.  Moderately strong southwest mid-level flow was overspreading a long plume of rich low-level moisture which extended all the way from Texas to South Dakota.  There would be plenty of severe thunderstorms and tornadoes.  With no particular spot seeming that much better than the others, we took the logical shortest drive straight west on I-40.

By 6:30 pm we had positioned ourselves on a supercell storm located west of Happy, Texas.  The storm had a persistent wall cloud with moderate to strong rotation and we had southeast winds blowing into the storm that were gusting to 50 mph.  The first tornado appeared as a very broad bowl of rotating dirt under the wall cloud that didn’t seem to be spinning that fast.  The dirt extended to cloud base and gave the appearance of a very large tornado.  Still, the motion wasn’t all that impressive.  We got closer and could see that there was a much more intense smaller core to the tornado.  It was on the ground for 14 minutes before weakening just west of Happy, leaving the air filled with suspended dust.  It only took a couple of minutes for another tornado to form on the west side of the city.  Unfortunately, this tornado was positioned perfectly to move through the city.  We could see roofs of houses being lofted as the tornado moved through, and came across a considerable amount of damage in the city.  Our first scan of the damage didn’t reveal anything that looked all that bad, or even anything that might have required our assistance.  In fact, the tornado only ended up receiving a rating of F2.  The bad news was that it did find a mobile home where two people were killed.