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Tornado Watch Coming for LA/AR/W. MS

Mesoscale Discussion #45

MESOSCALE DISCUSSION 0045
   NWS STORM PREDICTION CENTER NORMAN OK
   0226 PM CST SUN JAN 22 2012

   AREAS AFFECTED...NERN TX...NRN LA...SRN/ERN AR...NWRN MS...WRN TN

   CONCERNING...SEVERE POTENTIAL...TORNADO WATCH LIKELY 

   VALID 222026Z - 222230Z

   SEVERE THUNDERSTORMS SHOULD INITIATE BY EARLY EVENING NEAR THE
   ARKLATEX THEN RACE NEWD TOWARD WRN TN/NWRN MS AFTER DARK.  DAMAGING
   WINDS AND ISOLATED TORNADOES ARE EXPECTED.  A TORNADO WATCH WILL
   LIKELY BE REQUIRED BY 00Z.

   LEADING EDGE OF WELL DEFINED UPPER TROUGH IS ADVANCING ACROSS ERN
   OK/NERN TX AND WILL SOON OVERSPREAD THE LOWER MS VALLEY.  IN ADVANCE
   OF THIS FEATURE...WARM MOIST BOUNDARY LAYER HAS SPREAD INTO SRN/ERN
   AR...AS NOTED BY SFC DEW POINTS RISING THROUGH THE UPPER 50S INTO
   THE 60S...WHILE A STUBBORN WEDGE OF COOLER AIR HAS YET TO BE
   DISPLACED OVER MUCH OF CNTRL/NWRN AR.  CURRENT THINKING IS GREATEST
   AIRMASS DESTABILIZATION WILL OCCUR TO THE S-E OF THE AFOREMENTIONED
   WEDGE FRONT AND THIS WILL BE THE CORRIDOR OF GREATEST SEVERE
   THUNDERSTORM POTENTIAL.

   LATEST VIS IMAGERY DEPICTS AN INCREASING BAND OF LOW LEVEL CU ALONG
   THE DRY LINE NEAR I-35 OVER NCNTRL TX.  THIS IS ALONG THE LEADING
   EDGE OF STEEPER LAPSE RATES AND IS CERTAINLY INDICATIVE OF STRONGER
   FORCING THAT WILL SOON OVERSPREAD THE ARKLATEX.  WITH TIME
   THUNDERSTORMS COULD EVOLVE ALONG THIS LINE...OR PERHAPS EVEN DEVELOP
   WELL AHEAD OF THE WIND SHIFT WITHIN DEEPER CONFLUENT ZONE NEAR THE
   LA BORDER AS EXHIBITED BY SHOWERS BEGINNING TO DEEPEN FROM NEAR TYR
   TO JUST WEST OF SHV.  NEEDLESS TO SAY VERY STRONG SHEAR WILL SUPPORT
   SUPERCELL DEVELOPMENT AND THE POTENTIAL FOR TORNADOES.

   ..DARROW.. 01/22/2012

Morning Severe Weather Update

1/22/2012 1630Z Tornado Probabilities

This is a hazard specific graphic from the Storm Prediction Center. This graphic shows the potential for tornadoes this afternoon and tonight. The highest risk currently is centered from Little Rock, southeast to Jackson (MS), Northeast to Birmingham, and northwest to Jackson (TN). Within this area, residents have a 15% chance of experiencing a tornado within 25 miles of their location. When you think about those probabilities, they are actually pretty high. You have a nearly 1 in 5 chance of having a tornado occur within 25 miles of your location. Lower probabilities surround the 15% zone, but still present a substantial risk of tornadoes. In addition to the tornado risk, damaging winds will also be likely tonight. We’ll be providing live social media coverage all evening and overnight, so stay tuned!

Severe Weather Outbreak on Sunday in Dixie Alley

Before we dive into tomorrow’s severe weather setup, lets begin this discussion the way I always like to, starting off with the latest convective outlook.

1/21/2012 11:30 AM CST - Day 2 Convective Outlook

The Storm Prediction Center has issued a large standard risk of severe weather, identified by the orange outline denouting a 15% risk, from Shreveport, LA eastward to around Atlanta, GA, northward to Knoxville, TN and west back towards St. Louis. Within that 15% risk zone is an enhanced risk of severe weather which is identified by the red outline. Within the red line, residents have a 30% chance of experiencing severe weather within 25 miles of their location. That’s a nearly 1 in 3 chance, so it’s pretty significant. The white, dotted line indicates the potential for higher end severe weather, in this case meaning wind gusts over 75 MPH and the potential of significant tornadoes (EF-2+). I believe the outlook may be shifted west a tad with part of the 30% zone being upgraded to a 45% probability, which indicates a ‘Moderate Risk’ from the Storm Prediction Center. There’s no doubt that a major, significant severe weather outbreak is becoming increasingly likely. The wind shear values are very favorable for severe weather and the instability values will be unusually high for January. You combine those two ingredients and you have the potential for several tornadoes, some of which could be significant, and a major wind event (derecho) with 75+ MPH winds. This event will begin in Arkansas late in the afternoon and really ramp up overnight, before a squall line forms along a cold front from Louisiana up north into Missouri. That line will sweep eastward along with the severe weather risk. If you live out in the affected areas shown on this map above or have someone that does, let them know that there could be very bad weather tomorrow night. It could be down right dangerous. Now that I’ve described the risk areas, lets begin to dive into the overall setup.

0Z NAM: 250 Millibars at 6 PM Sunday

I’m going to start off a little higher then I normally do in these discussions. The following graphics will be from the 0Z NAM for 6 PM on Sunday. This is at 250 millibars which is around 35,000 feet above sea level. I’m not even going to describe the thresholds for wind shear in this case, because all those are met and nearly doubled for Sunday. It’s not a matter of if there will be enough wind shear, its just a matter of where. At 250 millbars off the 0Z NAM for 6 PM Sunday, the base of the trough is located across East Texas and Southeast Arkansas, with the leading edge of the trough digging into Indiana and points southwest towards Eastern Arkansas. Notice the black lines, known as heights, on this map. I want to point out the top portion of the graphic. See how the lines are pointed in a southeasterly fashion? This means this storm is going negative tilt, which nearly doubles its energy. We should have at least 100 knots of wind at 250 millibars across eastern Arkansas at 6 PM tomorrow, which is very supportive of upper-level organization of updrafts.

0Z NAM: 500 Millibars at 6 PM Sunday

Looking lower in the atmosphere, specifically at 500 millibars or 18,500 feet above sea level, can you find the storm? This is a very strong system that’s going negative tilt by 6 PM on Sunday. Winds in the base of the trough located across Northern Texas are over 95 knots with a peak value of 100 knots across Missouri. For those that have been long-time readers of the blog, you’ve seen this graphic several times in my discussions. You know how we usually see the yellows (55-65 knots) at 500 knots, but you don’t normally see the red and purple values which indicate 70-100 knots. You will tomorrow! I cannot stress how amplified and strong this system will be as it pushes into Dixie Alley tomorrow night. We see these systems a few times each winter and because we don’t have the moisture/instability values, we don’t have issues. As you’ll see in a few graphics, we have unusually high instability amounts for January. Combine those with this wind shear and we could be facing a very significant outbreak tomorrow night. The fact this will be after dark just amplifies the risk. Tomorrow night is going to be dangerous across the Southeast!

0Z NAM: 700 Millibars at 6 PM Sunday

0Z NAM: 850 Millibars at 6 PM Sunday

As we look at the lower part of the atmosphere, not much changes. We still have very high wind shear at 700 millibars and 850 millibars. In terms of the specific severe weather mode, I do want to discuss the wind direction in the lowest 150 millibars (850 millibars down to the surface). When we’re looking for the potential of tornadoes, we need directional shear. That can best be described with southeast winds at the surface, south winds at 850 millibars, and southwesterly winds at 700-500 millibars. Looking at the 850 millibar graphic, we see that winds will generally be out of the Southwest. I want to focus my attention on Eastern Arkansas, which is where we’re monitoring for a potential chase on Sunday. Winds at 850 millibars are out of the southwest at about 50-55 knots, which is pretty strong. Looking from 500 millibars down to 850 millbars, we don’t see a lot of change in the direction of the wind. This is what could be described as a linear look, meaning squall lines verses a major tornado potential. However, out in Dixie Alley especially, we see this more often then not with most tornado events. The one exception I can remember is April 27, 2011 where we had southeasterly 850 millibar winds. If we had southeast 850 MB winds tomorrow, we would be facing a massive tornado outbreak with dozens of tornadoes likely. I don’t think we’re going to have that many tornadoes tomorrow, but let me show you something a little different.

0Z NAM: 925 Millibars at 6 PM Sunday

During these blog posts, I don’t normally get this detailed in terms of diagnosing tornado potential because it starts getting pretty complicated. This graphic comes from a different weather website, but is still from the 0Z NAM and is for 6 PM on Tuesday. This is actually at 925 millibars which is below 850 millbiars, and is around 2500 feet above sea level. I know it’s pretty small on this graphic, but I want you to notice the wind direction across Eastern Arkansas and points east. The wind direction seems to be coming out of the south/southeast. That would help provide the directional shear I was talking about above. Honestly, I can’t tell you if this is going to be how it turns out. However, I need to stress that if we get more directional shear, much like is shown on this graphic, the tornado potential will skyrocket. We’re walking a very fine line between a few tornadoes and a major tornado event with significant, long track tornadoes. At this point, I’m expecting several tornadoes tomorrow night with the potential for one or two to cause significant damage. If we get a backed low level jet (fancy way of saying southeast winds), tomorrow night is going to be a very active tornado night, likely the most active we’ve seen since last Spring.

Before I begin to speak on the instability, let me describe the overall scenario based off current data. A strong mid-level inversion layer, known as cap, will keep storms from developing most of the day across Arkansas and Louisiana. I’m not looking further because my focus is on the I-40 corridor and points south. By around 4 to 5 PM, the energy associated with our negative tilt trough is going to begin influencing the region by providing lift and weakening the inversion layer. We’ll likely have storms going by 6 PM. Current data suggests we’ll be dealing with a mixed storm move, both linear segments (small lines) and discrete supercells. The supercells will have the highest risk of producing long track tornadoes, but the line segments will be capable of producing tornadoes as well. By around 9 to 10 PM, we’ll have a solid, to near solid, line of thunderstorms extending along the cold front. With the extreme amounts of wind shear present and assuming instability will be sufficient (we’ll get into that next), I’m expecting a long duration, bow echo to develop. This bow echo will likely be producing widespread damaging winds, some exceeding 80 MPH. Tornadoes will also be a problem with spinups likely in the line as it moves east across Tennessee, Mississippi, and Alabama. Tomorrow night will be a night that folks in Dixie Alley want to have a way of getting weather information.

0Z NAM: Surface Based Instability Values at 6 PM Sunday (SBCAPE at 0Z 1/23/12)

Finally, lets talk about the instability values for tomorrow. When dealing with cool season severe weather events, we often have a lack of instability, which is the primary reason we don’t have to deal with severe weather. With the excellent wind shear in place, thunderstorms don’t need much instability to become organized. I generally want to see at least 750 joules per kilogram of Mixed Layer CAPE in the cool season to support a marginal severe weather risk and anything about 1,000 joules is a red-flag indicator of a potential issue. It looks like we’ll have widespread instability values over 1,000 joules across most of Arkansas by 6 PM. While I’m not posting the graphics showing the progression, these values will spread eastward overnight across Mississippi and Southern Tennessee. That amount of instability combined with the excellent wind shear will help thunderstorm organize and remain organized for a long duration, as I said above. I won’t repeat what I said above, but it does look like it’s going to be a busy Sunday Evening and Sunday Night.

Now, we are a storm chasing website, so let me detail our plans for chasing this event. Connor is going to leave Oklahoma City tomorrow morning to head out and chase in Eastern Arkansas, likely targeting near Pine Bluff based on current data. He’ll most likely have his live streaming video available, which you’ll be able to watch on our Live Video page on our website! His stream will be available for media use. Media can contact us via the information on the contact page. I’m planning to remain in Dallas tomorrow to help provide up to date coverage on our social media pages, which is great for yall because we’ll be on top of our game tomorrow! Stay Tuned, I’ll be providing numerous updates tomorrow and tomorrow night as we get underway.

 

Watching Next Week…

0Z GFS: Surface dewpoint values for Wednesday Evening

This graphic is from the 0Z Global Forecast System (GFS) and is looking at 6 PM Wednesday, December 14. The 0Z GFS is showing rich, plentiful moisture flowing into Texas and Dixie Alley ahead of a storm system moving in out of the Southwestern US. Any time we see dewpoint values approaching 65 degrees in December, we generally have a problem. While we’re several days out and model guidance will change, I’m beginning to monitor next Wednesday with interest regarding the possibility of severe weather. Lets take a brief peak into what we may be dealing with next week.

0Z GFS: 500 millibar wind/heights for Wednesday Evening

Lets take a peak at the mid-levels of the atmosphere. This graphic is showing us the winds at 500 millibars for Wednesday evening. For those new to the blog, 500 millibars is about 18,500 feet above sea level and what I like to look at to see if we have enough mid/upper level support for organized thunderstorms. The overall setup is going to depend on where the storm system is positioned on Wednesday. I want to remind you that we are looking several days in advance and this setup is running about  12 to 24 hours slower/faster depending on which model you’re viewing. Anytime we see 500 millibar wind values at or above 35 to 40 knots and adequate moisture/instability is in place, we really watch for the potential of severe weather. The 0Z GFS is indicating values of 60 to 80 knots across the region, which would definitely be very supportive of severe weather.

0Z GFS: Mixed Layer Instability for Wednesday Evening

While the wind profiles are looking impressive for this upcoming system, instability values are looking marginal based off current model guidance. Sure, we’re not going to see extremely high instability values because we’re in the winter season, but I would still like to see values AOA 1,000 joules per kilogram to increase my confidence in some severe weather occurring. Digging a bit into the GFS, it looks like widespread cloudiness across the state on Wednesday along with warm upper level temperatures are limiting the instability.

If this event was tomorrow and I was using current model data, I would say we would likely have the potential for a few strong to marginally severe thunderstorms. The main issues would be lightning and a few marginal hail storms. However, this isn’t tomorrow and we still have several days to go before we even get this system into the upper air observation network (weather balloons that help weather models by ingesting more data to make the model’s solutions more accurate.) Since we don’t get much interesting weather during the month of December here in Texas, I wanted to get a blog post out early so we can keep a good eye on this upcoming system. If nothing else, we should get more rain by Wednesday of next week.

- David

Uncertainty Remains with Weekend Storm System

Good afternoon,

I posted on the social media pages yesterday about how the mid-range models were showing a powerful upper level system moving through the Central United States later this weekend, and how it was pretty darn impossible to say anything with certainty. Even a day later, we’re still having that problem. I wanted to show you what kind of data we’re dealing with when it comes to this system.

06Z GFS - Dewpoints at 7 PM Saturday

06Z GFS - Mixed Layer Convective Available Potential Energy (MLCAPE) at 7 PM Saturday

This data comes from the Global Forecast System (GFS) and is from the 06Z run from early this morning. The first graphic shows the dewpoint output at 7 PM on Saturday. Notice that the dewpoints are fairly low along/ahead of the dryline across Texas with values from 50F to 54F. As a result of the low dewpoint values, instability is non-exsistant on this run. If this run were to verify, we would be lucky to get a rumble of thunder, with absolutely no severe weather to be found. Now, lets take a look at the same model except the 12Z version that was run later in the morning.

12Z GFS - Dewpoints at 7 PM Saturday

12Z GFS - Mixed Layer Convective Available Potential Energy (MLCAPE) at 7 PM Saturday.

Now we fast forward to another model run from the GFS, the 12Z version run about 6 hours later. This is the same time period at 7 PM on Saturday with the same graphics as the 06Z run, except a few important differences. With the 12Z GFS, rich gulf moisture returns northward. 50F degree dewpoints are drawn northward along the cold front/dryline northward into Iowa. Dewpoints at/above 60 degrees spread inland across Texas and make it up to the Red River. Concentrating on Texas, notice how a 5 to 8 degree increase in dewpoints affects instability values. On the 06Z GFS with dewpoint values around 54F, there is no instability. With the 12Z run and with dewpoint values near 60-65F, a large instability pool is able to develop. Mixed Layer Instability is able to build up to 1000-1500 joules per kilogram (J/Kg). For a fall event in early November, that is a moderate to decently high amount of instability.

12Z GFS - 500 MB Winds/Heights at 7 AM Saturday

Here we’re looking at 500 MB (18,500 feet) winds and heights at 7 AM on Saturday from the 12Z GFS. While the instability/moisture questions remain, models are remaining fairly consistent on the position/strength of the upper level disturbance. Timing differences remain which would also have a significant impact on the forecast for the weekend, but the point I’m trying to make here is that this is a very powerful system. Winds at 500 MB exceed 80 to 100 knots. If moisture and instability are in place when this system arrives, there could be some severe weather issues. Even modest amounts of instability could do the job with this kind of a setup.

Can you understand why we can’t be specific yet on what we might be dealing with this weekend? We’ll be able to provide more details as we get closer to this possible event. Heck, it’s possible that there won’t be any event! We’re still over 125 hours away from this and high resolution model guidance doesn’t really kick in until 3 days out. Moisture return is a big question. The cold front that’s going to move through the region tomorrow night is going to really dry us out. Whether or not moisture can get back in here in time to produce any severe weather is the big question, as it normally is for fall/winter events. Stay tuned!

 

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