VIDEO: http://www.youtube.com/watch?v=Y_82dV0npYE

A dryline would be the target of the day across Western Kansas as a strong upper storm system began to move over the Plains.  Fear of strong capping was what kept us out of the Texas and Oklahoma panhandles and we worked to get as far north as we could.

The result was us hanging around the towns of Scott City and Leoti, KS for much of the afternoon.  Things were starting to look bad for us as the cap ended up being stronger than forecast even across western Kansas.  It took until late afternoon before the dryline showed signs of life.  When storms formed, they were made up of skinny updrafts that had short lifespans.

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Despite being severe, the Lakin storm had what appeared to be an updraft too small to support a tornado threat.  I then targeted a storm near Ulysses that looked bigger and had signs of sustained shear on radar.  Less than 10 minutes after starting toward this storm a Tornado Warning was issued based on spotter reports of a tornado near Ulysses.

A large tornado became visible (barely, due to darkness) to my east.  Starting east from about six miles north of Ulysses, I could see the tornado was still on the ground.  With the grain of the video being on the poor side, I switched to “super-night-shot” mode.  The tornado caused damage at a farmstead as it crossed the road in front of me.

Later I was shooting lightning as the storm approached Garden City.  I captured one image that not only shows the impressive updraft and lightning, but a small tornado under the center of the updraft.  A bonus tornado and an great end to what appeared was going to be a bust of a day.

I spent most of the morning concerned that instability would be lacking for any significant severe thunderstorms this day.  However, morning storms moved out of Central Oklahoma and by Noon we started getting some surface heating along the dryline that was located from Northwest to Central to South Central Oklahoma.  SPC meso analysis showed an area of Northwest Oklahoma had improving low level CAPE and a modest amount of low level shear.  I felt there was a chance of low-topped supercells under the cold pool of air aloft and with increasing towering cumulus on satellite less than an hour from Okarche, I decided to start north on Highway 81.  While in Enid, the Dodge City National Weather Service issued a Tornado Warning for a storm just north of the Oklahoma border near the town of Protection, KS.  I made a phone call to confirm why the warning was issued (a reported tornado) and figured that the potential extended to storms that were developing in Alfalfa and Grant counties.

I targeted a storm near Great Salt Plains Lake that had a large hail signature on radar that had a severe thunderstorm warning issued for it.  Visually there was nice structure with a dark rain/hail core, rain-free updraft base and vivid cloud to ground lightning.  About the time I pulled up just east of the updraft, a tornado warning was issued for the storm.
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I drove west, just north of the updraft to a point three miles east of Byron when a funnel cloud became visible to the south.  It was moving slightly east of due north and a short time later showed signs that it had become a tornado.  I continued to watch the tornado to my southeast as rain and hail increased at my location.  Eventually, the tornado became obscured and for a short period of time I didn’t know if it was still on the ground or not.  I started driving east toward where I thought it would be and it didn’t take long to become visible again.  By this time it looked smaller, but was still photogenic.

Later, and back east toward the Grant/Alfalfa county line, I came close to another tornado.  I would only see this multiple vortex tornado for a brief period of time before it became obscured in rain.  It had some nice motion with it and leaves and twigs dropped to the ground after it passed the road.

We started the day in Kearney, Nebraska and headed west with a fairly broad target area.  A large trough was located over the Rockies with 30 to 50 knot 500mb winds blowing across the Plains.  Plenty of low level moisture was in place east of a dryline that by afternoon would run from Southwest South Dakota to West Texas.

Here, cialis prescription cost we will talk about male infertility, what are the causes behind such kinds of sterility and where they can be treated. As a systematic disease, cheap cialis professional the vascular inflammation will damage on other organs as heart, kidney and lung. How does order tadalafil online ? viagra or sildenafil citrate is a PDE-5 blocker which is used to stop the way of phosphodiesterase type 5 enzyme and promote cGMP enzyme in the blood. Another type buy professional viagra of libido booster product is testosterone-concentrated products. The storm that produced the Big Springs tornado made narrowing down the target area easy.  It formed straight west of us with I-80 taking us right to it.  Timing couldn’t have been better.

We found ourselves directly under the meso-cyclone about midway between Julesburg and Chappell when the tornado developed just to our southwest.  It moved just south and east of us steadily growing in size and intensity.  It was on the ground for 40 minutes and 10 miles before weakening about 8 miles northwest of Big Springs.  While staying in rural areas, the tornado did injure two people.

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.