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 272012
 
SPC Outlook Area for Friday

I will be intercepting these storms in Kansas and then positioning the Mobile Weather Lab to ride any threatening storms into Missouri until dark. Meteorologist Chris Smith will be along helping to track the storms! We will be doing live reports in the early newscasts for KOLR.

A threat for severe storms exists today especially for areas of western Missouri this evening. The Storm Prediction Center has put much of central and eastern Kansas and a portion of western Missouri under a moderate risk.  Note that this is an evening event, no severe weather is expected during the day in the Ozarks.

A warm front will be moving back northeast across Missouri and Kansas today. South and west of this front through a portion of Kansas, the air is expected to become very unstable.  Also, a dry line will be moving into this unstable air over central and eastern Kansas by later in the afternoon and early evening.

Severe storms are expected in two areas. One near the warm front may evolve earlier in the day with Kansas being the most likely location for a severe storms. These would tend to move up toward the Kansas City area. They are not the main threat.

The dry line is the second area and the greatest threat.  It looks now as if storms firing along the line will quickly become severe in south-central Kansas and move northeast into eastern Kansas.  There is a tornado threat with these storms. They are expected to remain discrete (single) severe cells.

Sometime during the evening hours, these storms will cross into western Missouri. The biggest questions remain how far south the line will develop and how long will these storms hang on to the severe/tornado threat?  Some computer models have the environment becoming hostile to storms into the late evening hours over western Missouri while others keep it going into the evening.

To err on the side of caution, I would expect a few single severe supercells to be approaching the Missouri border by the 7-8:00 pm hour.  The exact timing and extent of storms will be monitored carefully later today. I believe the threat to be greater the more north along highway 71 you are located.

The threat may extend to the Springfield area or just west and north of the city by the 8:30-10:30 time frame.

Storms today will be coming out of the southwest at around 35-40 mph.

 

 

 

 

Apr 252012
 

Significant Tornado Parameter, 10 pm Thursday

It looks like a go for a storm chase Thursday.  My concerns are still the same but I think the potential outweighs the bust factor.

The overall concern is the strength of a mid-level warm, but unstable, air layer known as the elevated mixed layer.  I’m also going to keep a close eye on the quality and depth of humidity return into the target area.

The Significant Tornado Parameter (STP) from the SREF (9z run)  for 10 pm Thursday is shown. This is of course after dark in that portion of the Great Plains.  However, the parameter is developing nicely on the 7 pm chart.  There appears to be a window for tornado development in the daylight of early evening in southwest Kansas and northwest Oklahoma.

Also shown is the significant tornado ingredients map for the same 10 pm time.

I hate to be predictible but I’ll pretty much target this area for a storm intercept, subject of course to mesoanalysis in route.

Significant Tornado Ingredients, 10 pm Thursday

SPC Outlook for Thursday

 

Apr 232012
 

EHI 7 pm Thursday 18z NAM

I am contemplating a trip to Kansas on Thursday to chase severe storms.

This is based on the data coming in from the 12z Monday computer model runs.  Actually, Thursday and Friday look good but personally, Thursday works out better for me despite the distance.  We’re actually talking about northwest Kansas up into northeastern Colorado.  I would only as far as Kansas but it should be enough.

A strong cap of warm air will take hold over much of Texas, Oklahoma and southern Kansas on Thursday.  However, a curved area of unstable air will stretch from western Kansas northwest into Colorado.  I would target western Kansas as it stands now.

There are some issues. First, I’m somewhat dubious of the forecast values of dew points into the sixties riding NNW into this region. Lower dew points would reduce the instability.  I could handle this if the wind shear was fantastic it it too might be right on the edge.

It’s one to be watched to be sure!

 

 

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 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.

 

 

Mar 192012
 

Flood Advisories Tonight/Tuesday

The HPC forecast calls for widespread 3-5 inch total rainfall over much of the Ozarks. Much heavier rain is expected over areas of northwestern Arkansas and extreme western Missouri.  Those areas may receive locally 7-8″ totals!

This will cause flooding and a flood/flash flood watch is in effect for much of the area.

Also, severe thunderstorms could erupt over a portion of the Ozarks later today.

A slow-moving upper level low pressure area will bring repeated and slow-moving rain rain to this area.

More updates later today!

Rain Forecast Through Tuesday

 

 

Mar 042012
 

February is not known for its tornadoes in the Ozarks. Here are a few from the archives:

Izard/Sharp Counties in AR

More recently, a tornado touched down during the early morning hours of March 1st 2007 in extreme eastern Ozark County and tracked northeast into Howell County doing damage near Caulfield, MO.  The National Weather Service write-up of this tornado.

March on the other hand is actually quite active in the Ozarks.  The infamous outbreak of March 12th, 2006 comes to mind.  Other outbreaks include March 12, 1961, March 26, 1976 and March 15, 1982.

I put all of the outbreak track maps in this Google + album.

Buffalo and Lebanon Missouri were hit by tornadoes on March 31st 2008.

 

 

Wright, Ozark & Howell Counties

Mar 042012
 

It was a wild and crazy week for tornadoes. As the Ozarks are taking a final count of the Leap Day twisters, many states out east of us are dealing with the aftermath of an even larger outbreak on Friday.

The National Weather Service has performed extensive surveys of damage caused by Tuesday night’s storms.  The official tornado count is at eight with two fatalities.

Radar Image at 11:05 pm 2/28/12

The outbreak began with wind damage reported in Pittsburg, Kansas.  This was the beginning of what would be the Lamar tornado in Barton County.  This storm was rated an EF-1 and ended its path near the Lamar Airport.

Tightly Wrapped Hook on Radar at 11:31 pm

The next storm starting developing south of the Barton County storm. This EF-1 tornado started north of Greenfield in Dade County, tracked for just over 18 and one half miles to the northeast, passing north of Dadeville and ending up southeast of Aldrich in Polk County. The included image reveals a particularly well-defined hook echo with this storm at the beginning of its track.

A few minutes before midnight, the beginning of a tornado that would produce EF-2 damage near Buffalo, Missouri started 4 miles south-southeast of Halfway, in Polk County.  This stronger tornado was on the ground for 10 miles.  It was responsible for the first fatality of the night.

The same cluster of storms continued to race east.  Another tornado formed 1 mile southeast of Bennett Spring. This EF-1 twister was only on the ground for a quarter mile.  Another EF-1 tornado injured one person while on the ground for about 11 miles from Phillipsburg to just southeast of Lebanon.  It lifted around 12:30 am.

At about the time the Lebanon tornado was lifting, a cluster of thunderstorms with distinct circulation patterns starting coming out of McDonald County in extreme southwest Missouri.  As these storms moved into western Barry County, an EF-2 tornado was produced near Cassville around 12:45 am.  This storm killed one person.

Radar at 1:14, Right After the Tornado Touched Down in Kimberling City

The same storm area moved quickly east across Barry County and into Stone.  This is where the third EF-2 tornado of the outbreak started.  Joe Bald Road in Kimberling City is the start point for this tornado that would eventually produce damage right along Country Boulevard, Highway 76 West in Branson and downtown Branson.  The tornado travelled 22 miles total and ended near Kissee Mills.  It took about 20 minutes to travel this distance, giving the tornado a forward speed of about 66 mph!

At about the same time as the start of the Kimberling City damage, an EF-1 tornado traced a path through portions of Phelps and Dent Counties.  It had the second longest path length of the night at 19 miles.

All totalled, 8 tornadoes. Three EF-2′s and 5 EF-1′s made up the outbreak with two deaths.

Please see this post for a review of how this outbreak stacks up to others in the Ozarks during this time of year.

 

 

 

 

 

 

 

Jan 072012
 

Had anyone prior to January 7th/8th, 2008 tried to convince me it was possible for 35 tornadoes to churn across the Ozarks in January, I don’t think they would have been successful.

Four years ago today, a major outbreak of tornadoes struck the Ozarks hard, lasting into the wee hours of the 8th.

The tornado count is at 35 (including two in Benton Co. Arkansas) separate twisters including  2 EF3′s, 5 EF2′s and 13 EF1′s. There was loss of life with this outbreak. One woman died just east of Strafford and another woman died north of Marshfield.

At a count of over 30 tornadoes, the outbreak which occurred across southern Missouri and northwest Arkansas starting on January 7, 2008 is easily the most extensive in recorded history.

As if an outbreak of this magnitude needed any help becoming infamous, there were other factors which accomplished just that.

First, it was the time of year. January is not known as a tornadic month in our area. Prior to this outbreak, only four tornadoes had been recorded in this month since 1950!  Because of the time of year, most of the outbreak occurred in the dark, adding to the tension.

Secondly, while the possibilty of severe weather with isolated tornadoes was extensively discussed by meteorologists and forecasters, a major outbreak simply wasn’t anticipated. The Storm Prediction Center (SPC), never put us in an overall risk higher than slight (by contrast, the previous two extensive outbreaks occurred in a high risk area).

Then there was the repetition. A check of the radar loops for this time will reveal how supercell thunderstorms inititated and tracked over the same small region again and again. This “training” effect has lead to many flash flood situations but in this case, the discrete nature of the storms