May 222012
 

3D Rotation at Peak Intensity

It was one year ago today, on a Sunday, that an insidious tornado tore through the southern portion of Joplin, Missouri.

Insidious because of how quickly it formed, where it formed, how intense it became and where it traveled.

Even with all of the technology at our disposal, 158 people lost their lives (NWS statistics).  Here is a list of the highest single tornado death tolls on record.

Back in the 1950′s, a tornado killed 116 people in Flint, Michigan. During and soon after this tornado, huge advancements were made in tornado awareness,  radar technology, storm forecasting (the “watch box” was introduced to the public) and emergency response.  It has been stated that Flint was the last 100+ person death-toll from a single tornado due in large part to all of these advances and others such as warnings, weather radio and Doppler radar.  While this is no doubt true, no one should believe that we reached a plateau or that this type of disaster could not happen again.

In fact, just as you would adjust what the dollar is worth because of inflation, this Joplin death toll needs a similar adjustment. Note on the list I linked above that all of the deadly tornadoes higher than Joplin happened before there was radar (Doppler or otherwise), tornado warnings, tornado watches, television, cell phones and certainly the internet.  When considered in this light, the tragedy of Joplin glares even brighter.

High death tolls are a matter of horrible circumstances coming together.  The real truth is that this can happen again and it will, somewhere.  Population areas continue to expand.  There are some who think even higher fatalities are possible.

Before I go any further, I would recommend reading the National Weather Service “Service Assessment Report” for the Joplin tornado (PDF file).  A panel of individuals performed an assessment (as they do for most major tornadoes and/or outbreaks) of the events leading up to the this tornado.  There are some valuable insights in this paper.

I’m an old school guy with regard to tornado warnings.  Even with my all of my experience with tornadoes in the Ozarks and my inside knowledge of radar signatures, our family still takes shelter, without question, when a tornado warning is issued.  I’m a strong believer that a tornado warning is not “soft”, rather, it offers a choice to take shelter, yes or no. A personal decision.

But many people don’t take shelter, at least not right away.  The reasons vary but it mostly stems from a rather inescapable truth about tornado warnings: many times, nothing happens to you personally after the warning expires, even if a tornado is reported in the warned area. I state this not as a slam of the warning process but as more of a reality check of the current knowledge and dissemination limitations of the warning system.

The assessment report hits on this when it states that many folks sought a “second opinion” before deciding whether the tornado warning was important enough or close enough to take action. It is human nature to want to know what is going on around you.

Everyone needs to know that we in this country are fortunate enough to have a government organization, the National Weather Service (NWS), whose mission it is to save lives and to watch 24/7 for threatening, destructive or deadly weather situations.  This is a free service paid for by your tax dollars. The warning system is a good one. Not perfect but good. It is easy to loose site of the fact that the people in the hot seat issuing warnings have a tough job. They are being asked for more and more precision even when the current technology, understanding of the meteorological process, small scale sampling of the atmosphere and dissemination paths are not up to full potential.

The question I would throw out is this: are far can we take the precision of the tornado warning process?  There is an old observation, made to drive home the idea of not ignoring tornado warnings, which states “no one is going to come and ring your doorbell and tell you a tornado is coming!” Well, I don’t know about doorbells but technology might help in the not-too-distant future.

The NWS is slowing rolling out a warning system in corporation with the cell phone industry which will give you a short text warning based on you GPS position.  The only issue I might have with this is when cell towers go down or become overloaded during large tornadoes like Joplin.

On the other hand, weather radio is essential to anyone who takes storm safety seriously.  The reason: it broadcasts a signal on a VHF frequency 24/7 and has the ability to alert you by county and to wake you up if weather threatens while you sleep. My only wish would be to make them GPS-aware in the future which would improve the accuracy and make them truly portable.  It’s one device which should definitely remain a uni-tasker, designed only to do one thing!

Coming back to the Joplin tornado, the amount of time it took for this tornado to become a monster was very, very small. The tornado was low to the ground, perhaps indistinguishable to the untrained eye from a low cloud near the ground and made worse if trees and building blocked the view of the horizon. It started on the edge of very densely populated city (couldn’t see it coming for miles and minutes beforehand). It was really the second storm to threaten the Joplin area that evening (read the assessment report) which may have caused some confusion.

This video shows the beginning of the Joplin tornado and sums up how quickly it spun into existence:

Apr 162012
 

Twin Tornadoes North of Cherokee OK

It was the third day of an extended storm chase into the Great Plains and I have several good storms to show for it including an awesome twin tornado shot near Cherokee, Oklahoma during the last 20 minutes of the chase on Saturday.

First off, there was an incredible number of violent tornadoes in Nebraska, Kansas, Iowa and Oklahoma on Saturday.  Thoughts and prayers go out to all affected.

I chase storms as a hobby and in an official capacity either for broadcast (KOLR/KOZL) or for education (Missouri State University).  Chasing is thrilling to be sure but I also learn more about tornadoes and supercells every time I head out.  The twin tornadoes pictured are an excellent example of how much different each tornadic storm can be.

The chase started in Kansas. We hung in east Kansas for a while on a hunch that something my fire there but abandoned this idea and started heading west in southern Kansas.  Several supercells were forming southward into Oklahoma and the plan was to catch one and then drop south to the next one, which largely worked out for us.

First Stop

The first encounter was south of Pratt, Kansas just southwest of the town of Sawyer, KS.  Radar indicated rotation with this storm and visuals confirmed the existence of a well-defined wall cloud.  The wall cloud passed just north of our position south of Sawyer.  It passed north of the town as well. We chased it north of town as it was weakening.  It looked is if a new circulation center had formed on radar but this was hard to get a visual on.  There was a tornado report on highway 54 just east of Pratt which seems to confirm this idea.

We stopped for three more supercells before dark. One was near Medicine Lodge. Once again, a clear rotation that never tightened up into a tornado.  The second storm was south into Oklahoma, it passed just northwest of Burlington on Highway 11.  We watched this for a while in the 7 o’clock hour.  It became clear that a larger storm to the south was hindering the development of this cell.

It should be noted that we were deprived of radar data at this point. 2G Verizon was the best we had which delivers images slowly!  If I had know how much larger the southern-most storm was, we would have broken off of the Burlington storm sooner!

With only about 20 minutes of daylight left we checked out the last storm. It was on the way home anyway. When we busted out of the “anvil core” heading south on highway 11, another wall cloud was visible on our right.  A family was watching this storm and said “you missed it” They were referring to a tornado which had already formed and dissipated.  I advised these folks to keep following us south as we were too close to the direct path of the storm.

Second Stop, Two Circulations

In the video, you can see a second tornado formed as we were driving south. The right twister appeared white in the sunlight.  We stopped again at the Highway 11/64 intersection just north of the Cherokee Airport.  This is where one tornado passed in front of the other (see picture)  and then became one again as it passed just northwest of this intersection.  A close-up of the ground dust and debris is included in the video too.

Finally, we took up a position in the parking lot of the airport.  The video shows this as a classic looking black tornado with a diffuse back-light made of of rain and hail providing excellent contrast even after sunset.

For those wondering, the Cherokee storm went on to produce the EF-3 monster tornado in southeastern Wichita later in the evening.

Probable Tornado Path (courtesy Disaster Mapping)

Apr 142012
 

SPC High RIsk Today Including Strong Tornadoes

This is the big storm outbreak day which has been talked about for a few days now.

Overall, the set up is much the same. There is an abundance of warm and moist air today.  The jet stream (up high) and low level winds will be very favorable for supercell thunderstorm development with tornadoes likely.

The Storm Prediction Center has been expanding the high risk area northward steadily. I don’t believe we’ll travel into Nebraska, favoring areas of Kansas instead.  There is some question as to the extent of supercell development more south along the dry line. I believe they will happen, it will be trying to figure out exactly where and which ones will be the strongest that will be the trick, as always!

I’ll be video streaming live today as technology permits. I’ll also be doing two live reports on the news: one on KOLR at six o’clock and then again a recap on KOZL Local news at 9 o’clock.

 

Apr 142012
 

We were very close to the Norman, OK tornado on Friday but made a wise storm chase decision which likely prevented us from a too close and possibly dangerous encounter.

The radar image shown was tweeted on Friday as we were heading south on I-35 toward the Oklahoma City metropolitan area.  The huge supercell, not yet tornadic, is plain.

I don’t like storm chasing in metropolitan areas. Too much traffic, too few quick escape routes.  As we were intercepting this storm I had two thoughts in mind 1) we will just get ahead of this by continuing south on I-35 or 2) we need to get out ahead of it by heading east on I-40.  Traffic was stop and go and close to rush hour on a Friday so we took the I-40 option.  By my calculation, this decision prevented us from crossing paths with the tornado as it crossed I-35 near Norman.  I enclosed some videos of that tornado in action.

By heading out on I-40, we were able to get ahead of the storm. After the Norman tornado, the storm disorganised somewhat.  But from our new vantage point in Tecumseh, OK, we could see good structure lots of cloud-to-ground lightning and a clear base.

A new tornado warning has eventually put out for this storm as it travelled  just to our north. We changed position to west of Tecumseh to try and improve our view.  There are a surprising number of hills and trees in the area just east of Oklahoma City which made spotting tornadoes, especially those wrapped in rain like this storm, very difficult.  Local media was reporting a tornado arounf Shawnee on I-40 but we had no few. As of this writing, the SPC has not verified this report.

We then travelled west on highway 9 to chase storm two. This took us out on th south edge of Norman, passing right by the tornado damage from earlier including wehere the tornado crossed I-35.  This second storm was dominated by cool air at the surface and wasn’t pursued further because of new storms in southwestern Oklahoma.

We had enough daylight to chase these storms but only the lead one.  Driving southwest on I-44, we cut over to Apache and then watched another tornado-warned storm take shape northwest of Boone, OK.  The backlighting was very poor because of the large area of clouds and storm to the west. If there was a tornado in there, we couldn’t see it!

We ended up back in northern Oklahoma City for the night, ready for the big day today!

 

Apr 132012
 

High Risk Area for Saturday

A high risk for severe weather and a probable tornado outbreak is forecast for an area west of the Ozarks (see included threat area map).  The greatest threat as outlined today is from north of Wichita south-southwest into Oklahoma west of Oklahoma City.  I will be staying an extra day, extending my current storm chase, to report on these storms!

I will have a live report in the 6 pm news on KOLR on Saturday which hopefully will include live streaming video. (tech willing!) Additional reports are possible on KOZL Local News at Nine and the KOLR 10 pm news as well.

The long talked-about upper level storm is providing the strongest jet stream winds to the central Great Plains on Saturday.  After days of working on this, the atmosphere will have delivered quite a bit of deep rich humidity to a long fetch of the Great Plains, providing a key ingredient for very unstable air.

This is only the second time the the Storm Prediction Center has issued a High Risk for a day in advance (what they call “day 2″). The last time was April 7th, 2006. Here are the reports of severe weather for that day.

The question naturally arises as to how far east these storms will travel and how severe they might be with regard to the Ozarks.  The upper level winds which steer these storms coupled with the still slow movement of the upper level storm generating them suggests the most violent weather will stay confined to areas of Kansas and Oklahoma.  The individual storms will probably form a line of storms which might be knocking on the doorstep of west central Missouri after midnight Saturday night.  This will be monitored carefully.

Sunday could see some severe storms in the Ozarks as the system again shifts a few hundred miles more to the east. Separate blog coming on this possibility.

 

 

Apr 092012
 

Storm Prediction Center Outlooks

A change in the upper level jet stream winds should be responsible for multiple rounds of severe weather over the Great Plains states by late week and into the weekend.

By late this week, a pattern of upper level winds out of the southwest will be established over the central and south-central U.S. as a trough of low pressure develops over the southwestern U.S.

The pictured outlook areas move very little over the three day period.  This is because the overall pattern aloft is forecast to only slowly move. Meanwhile, smaller disturbances traveling through the upper-level wind pattern will help to shape the position of the severe thunderstorm on any given day.

Generally, this area will become better embedded in higher and deeper humidity as each day progresses as a steady wind from the Gulf of Mexico continues to flow.  Actually, there is even a risk on Wednesday (not shown) just as this begins to happen from the panhandle of Oklahoma and Texas southward.

By Thursday, not only will the humidity and its associated unstable air be better established but the upper level wind core will begin to strengthen to the point of more widespread severe possibilities.

Friday looks slightly better with the overall jet stream structure.

This will be a two-day chase for me leaving early Thursday and returning late Friday.  It should be exciting!

NAM 500 1pm Thursday

NAM CAPE 1pm Thursday

Mar 212012
 

Tornado North of Mangum OK 3/18/12

My storm chase to the High Plains did pay off as one storm hung on to produce some weak tornadoes.

We went this past Sunday, March 18th. On board and my wing-man was Eric Freeman. Eric was a big asset on the last Missouri State University Storm Chase Class in 2011 and knows my laptop and all of the various hookups like video streaming and radar data.

Also joining us was Richard Hahn. Aside from being a current student of mine in Weather and Climate at Missouri State, Richard is Director of Safety & Environmental at the Assemblies of God Headquarters in Springfield. The AG Headquarters recently hosted the Greene County Spotter Training Course put together by the Springfield National Weather Service.

Radar at 6:54 pm

Our target was somewhere in the eastern panhandle of Texas or western Oklahoma. Many chasers where already in position early as we were still traveling down I-44 in Oklahoma.

Being “fashionably late” was only a concern if thunderstorm initiation happened too early. As luck would have it, we were just in time and didn’t have to do any backtracking east as storms started to fire in the southeastern Texas Panhandle southward. We only then had to get off on Highway 34 south off of I-40 in western Oklahoma.

We started calling the storm closest to us, which would eventually track northeast to near xxxx as storm #1 while a second, reachable storm showing slightly better development in extreme northern Texas was called storm #2 (creative, right?)

Storm-Relative Velocity at 6:54 pm

As we watched storm #1 track into Oklahoma, it just didn’t look that great (first few shots on the video) and on several occasions we started to leave it for storm #2. But just as we would start driving away, a cloud feature would keep drawing us back. “Bird in the hand” became the mantra of the chase and as luck would turn out, it was the right call of the chase.

Even though storm #2 went tornado-warned in Texas, we stuck to our guns.

As we continued to stair-step the roads in pursuit of our northeast-moving storm, the lowerings and wall clouds starting to look more and more impressive.

Finally, after passing through the town of Mangum and flying westward a bit, we ran into this storm just as it was reaching its greatest rotational strength (see radar images)

The video tells the story pretty well, shot from Highway 9 northwest of Mangum.

Chaser convergence on highway 34 north to near Willow OK was pretty bad, lots of chasers and gawkers pulling off the road. It got really bad when this supercell decided to drop a weaker tornado just of the western side of the highway! This is the elephant-truck which ropes out at the end of the video. It was an unexpected surprise!

The National Weather Service out of Norman, Oklahoma has not received any damage reports from the tornadoes which dropped from this supercell and is putting the tornado rating on each report as an EF-0.

Enjoy the video! My “now that’s a tornado!” comments are in reference to the frustration in seeing the tornado with some of the poor contrast backdrops.

Mar 142012
 

SPC Severe Forecast for Sunday

I’m investigating a possible personal storm chase for this Sunday (3/18) into the Great Plains.

This idea has been evolving slowly all week.

Much of the success of  this chase will hinge on how a deep storm in the upper atmosphere moves into the Great Plains.

It seems clear that humidity will be in good supply and that the above mentioned storm will finally bring the wind shear values up to severe levels.

12z runs this morning look like the back up the included forecast area from the SPC.

The pluses include the unstable air and wind shear.

GFS Sounding /Great Bend KS/7 pm Sunday

Minuses: I did notice evidence of a large middle and high-level shield of clouds out ahead of the system which could limit daytime heating a tad.

Also, the storms which fire along the dryline may not reach severe levels under after they move east into the more favorable air which this time of year could very easily be after dark.

 

Mar 122012
 

The Big Four Supercells of 3/12/2006

This tornado outbreak was intense for the Ozarks.  In terms of the number of well-defined supercell thunderstorms, tornado count and tornado intensity, it was actually worse than the imfamous May 4, 2003 outbreak.

A total of 13 tornadoes tracked over the Missouri Ozarks with another three tracking across northern Arkansas on this Sunday evening.

The Early Storms Up North

Earlier on this Sunday, storms broke out to the north and northwest of Springfield.  The EF-1 tornado tucked up in the northwest corner of Benton County (see map below) actually occurred shortly before 4 pm.  The rest of the tornadoes were later in the evening.

This tornado which nicked Benton County was part of a supercell thunderstorm which lasted an amazingly long time! The so-called “six state supercell” started in Oklahoma and could be tracked through Kansas,Missouri, Illinois, Indiana and Michigan.

Here’s a “follow the storms” radar loop to examine.

Double Take

One of the most talked about aspects of this outbreak was the eerie path one tornado took over nearly the same path as one of the tornadoes during the above-mentioned 2003 outbreak.

Comparison of Tornado Tracks

The map below is actually two maps superimposed: one shows the track (heavy red line) of the May 4th, 2003 tornado while the other shows the track (thin red line) of the March 12th, 2006 tornado. The tracks are exactly on top of each other near Verona and never drift more than a mile from each other until the very end. The 2003 storm turned left near the end of its track and struck Battlefield while the 2006 storm maintained more of a straight line. These maps were created by the Springfield National Weather Service Office and can be found in their original form here (2003) and here (2006).

Turning Winds

The low-level winds with this event were amazing.

Doppler radar can sense whether raindrops or hail are moving away or toward the radar site. This principle also works in an environment without storms because radar beams can actually bounce off of large cloud droplets and turbulent pockets in the atmosphere. Doppler codes winds that are blowing toward the radar with green, wind blowing away as red.  The first image captured at about 6:00 pm shows winds near the surface of the earth coming from the SSW. Two hours later at 8:00 pm, the winds had turned slightly or backed to the SSE. This turning of the wind in the lowest layer of the atmosphere has been shown to have a profound impact on the potential for thunderstorms to produce tornadoes.

Detailed reports on the Missouri tornadoes from the Springfield National Weather Service.

Tracks in Missouri

Arkansas Tracks

Mar 122012
 

It is *oh* so important to talk about the concept of tornado weather.

Tornado weather is not as obvious as you might think.  If you are relying on just your senses, you can be misled.

The most important statement I can make here is that a tornado watch means tornado weather so watch for tornadoes, no matter what time of day or year it happens to be!

Many of you probably have some less than useful statistics in your head regarding tornado occurrence.  The idea that statistically tornadoes tend to strike in the late afternoon and in the spring months, while not inaccurate, is not very helpful when assessing the risk for a tornado.  One only has to to look to our Leap Day Outbreak to know that tornadoes can and do strike at night and in February!

Moreover, studies (namely the Super Tuesday Outbreak Assessment PDF file) show that people may not take tornado information like a watch area as serious if it occurs during a cool time of year or during what they consider to be a lesser threat time of day or year.

From the assessment:

“Over 50 percent of the people interviewed acknowledged that they associate tornado outbreaks with the springtime or summer months. This caused many of them to minimize the threat of this early February outbreak because of their perception that it was too early in the year and outside the “traditional” tornado season.”

Many of the ingredients which make a weather pattern tornadic simply cannot be sensed such as overall strong jet stream winds, the proper low level winds (not just windy!) and particulars involving unstable air, to name a few.  This is why meteorologist are charged with the task of looking for these features and alerting the public to their presence.  If you think about it, you’ve experienced strong winds, high humidity days, abnormally warm weather, cold air colliding into warm, thunderstorms, etc, lots of times without tornadoes forming, there is obviously more to tornado forecasting!

Now, is there anything you can do to help yourself? Sure!

  • Look at Radar: There are so many sources to see radar screens now.  The interactive radar at Ozarks First is a great place for a quick look.  It’s a situational awareness concept: are there thunderstorms close to you?  How fast are they moving and from what direction?  Knowing that thunderstorms are near even before you see darker skies gives you a leg up!
  • Buy a Weather Radio: As I stated before, these are great little devices that can be programmed to alert you when severe weather threatens your immediate area.
  • Pay Attention to Tornado Warnings!:  Wow, pretty simple.  There are some who don’t act because they believe nothing has ever come of warnings in the past therefore they aren’t worth listening to. Get over it!  While they are not perfect, tornado warnings are the best information we can muster as meteorologists.  The National Weather Service is always trying to improve the process. It’s a matter of personal responsibility!

FYI, if you hear the “freight train” or rumbling sound of a tornado, you’d better already be in a shelter!  The sound of a tornado is caused by the intense wind which ramps up quickly close to the tornado. With weaker tornadoes, no hearing advantage at all.  In the largest storms, perhaps some.  If you hear it, it’s very close!  I wouldn’t rely on hearing a tornado as your only “OK, this is serious” clue.

Finally, a note on warning sirens.  The outdoor tornado warning sirens are extremely helpful but in case you didn’t know, they were never intended to be heard by everyone, especially if you are inside.  If you are relying on outdoor sirens as your only alert to a possible tornado you are in trouble!

Next blog on this topic: Taking Shelter!