Day 129: Location of Highest Severe Threat on Monday

Note: Tonight’s blog post is kind of technical. I purposely avoided talking about too much of the technical side of things, but in some aspects it could not be avoided. Non-technical readers should still be able to get something out of reading the post.

As I’ve been alluding to for several days, the stage is being set for a significant severe weather outbreak on Monday. In fact, the VORTEX II crew called off any operations today, Day 9, so that they could travel to be in position for operations tomorrow.

Although it is becoming increasingly apparent that a significant severe weather outbreak will unfold tomorrow, the exact location of the worst weather is not entirely obvious. It is true that a very powerful mid-level trough will be racing through the plains at the same time warm, moist air will be drawn northward, and hot, dry air will be surging eastward from the west. But it isn’t apparent where the intersection of all these ingredients will occur.

Below are forecast soundings from a couple of sites throughout the southern plains taken from four different numerical models that were initialized and run this morning. A sounding is essentially a vertical snapshot of the atmosphere’s temperature, moisture, and wind profiles.  They allow meteorologists to assess the atmosphere’s potential for producing a wide variety of phenomena ranging from ice storms to wind storms to severe thunderstorms and tornadoes.  Temperature and moisture profiles are plotted on a Skew-T (named because the temperature lines are “skewed” at angles), whereas the wind profile is typically displayed using a hodograph.

Day 129 (a)

The image above is taken from the 12 UTC (7 AM CDT) run of the North American Model (NAM). It is the sounding and hodograph for Norman, OK at 01 UTC Tuesday (8 PM CDT Monday). The image below is taken from the same model run but is valid an hour earlier for Wichita, KS. Without going into a lot of interpretation (if enough people request it, I’ll do a future blog post or two about interpreting soundings and hodographs), both of these images are representative of what would be expected in a significant severe weather outbreak. These images alone would argue that the chance of significant severe weather would be quite high in central Oklahoma and southern Kansas.

Day 129 (b)

But, it can’t be that simple, right?

Day 129 (c)

The image above is once again valid for Norman, OK at 01 UTC Tuesday (8 PM CDT Monday), the difference is that it comes from the 15 UTC (10 AM CDT) run of the North American Model with the Kain-Fristch convective scheme (NAMKF). The image below is taken an hour earlier from Wichita, KS. Notice anything different about these two images and the two images above?

Although the hodographs (wind fields) still look conducive to severe thunderstorm development, the thermal and moisture profiles do not. In these runs the instability is considerably lacking and the moisture appears to have dried out. This would indicate that central Oklahoma and southern Kansas would not be in the axis of greatest threat for a severe weather outbreak tomorrow. So where did it go?

Day 129 (d)

This would indicate that central Oklahoma and southern Kansas would not be in the axis of greatest threat for a severe weather outbreak tomorrow. So where did it go?

Day 129 (e)

If we take a look (above) at the same kind of plot a farther east of the I35 corridor, in this case, Tulsa, OK, we can once again find temperature, moisture, and wind profiles that look similar to the first two I showed. This would seem to argue for the severe weather threat to be centered more in the northeast Oklahoma area than the I35 corridor in central Oklahoma and southern Kansas.

So which is it? Maybe looking at another model will help us determine where the highest risk will be…

Day 129 (f)

These images are taken from today’s 12 UTC run of the Global Forecast System (GFS) model. The image above is valid for Norman, OK at 00 UTC Tuesday (7 PM CDT Monday) and the image below is valid at the same time for Wichita, KS.

Although not as impressive as the NAM forecast for Norman, OK that I posted initially, the GFS forecast for Norman is certainly indicative of a significant severe weather potential. Wichita, KS, on the other hand, still has very good wind profiles, but doesn’t have the temperature and moisture profile to support a widespread significant severe weather outbreak.

What about Tulsa, OK?

Day 129 (g)

The forecast (below; valid at the same time as Norman, OK and Wichita, KS) for Tulsa, OK isn’t as impressive as Norman’s, but is a lot better than Wichita’s.

Day 129 (h)

This set of temperature, moisture, and wind profiles would argue for a severe weather threat centered in central Oklahoma, extending northeastward through Tulsa, OK and not much in the way for south central Kansas.

Anything else to look at? You bet! Below is a set of forecast soundings from a model with a grid-spacing of 4 kilometers. This model doesn’t have to parameterize convection as it is capable of generating thunderstorms in the model natively. What does this model forecast?

Day 129 (i)

Once again, this model was initialized at 12 UTC (7 AM CDT) and the plots are valid for 00 UTC Tuesday (7 PM CDT Monday). The image above is for Norman, OK and the image below is for Wichita, KS. Norman’s sounding is once again indicative of a potential major event whereas Wichita’s is considerably more marginal.

Day 129 (j)

Examining the sounding for Tulsa, OK (below) indicates that severe thunderstorms would be possible, but the threat for tornadoes might not be as high as the other models would indicate.

Day 129 (k)

So what does all this mean? Well, for one, all these plots did was show whether the temperature, moisture, and wind profiles would be sufficient for severe weather. I didn’t even discuss whether or not a thunderstorm would develop in an environment characterized by one of these soundings. In general, the farther north you go tomorrow (based on the domain laid out in the post of central OK, southern KS, and northeast OK) the better your chance of seeing a thunderstorm. Thus, while the environment may be supportive of a major tornado in central Oklahoma, we aren’t guaranteed that a thunderstorm will develop.

Keeping all this in mind, what would you forecast if you were working tonight at the Storm Prediction Center? What would you forecast if you were working on the VORTEX II project? In both cases your forecast will put into motion various plans that affect a lot of people and millions of dollars worth of equipment. Do you err on the side of caution and over warn with your forecast, knowing it’s better to be safe than sorry? Or do you take a chance by making a more specific forecast, trying to save some people money and stress, and risk being wrong?

It’s a tough decision that meteorologists are faced with all the time. What is the best way to convey this kind of uncertainty? I’m interested in hearing your thoughts…

  • Damon Lane

    Love the blog! Oklahoma is very sensitive to tornadoes. ( Just mention May 3rd and we all know what you’re saying). In this situation, you raise public awareness by pushing the strong wording of your discussion, but you also hit the uncertainties hard as well (and explain why you are uncertain). Once the public is able to read both the pros and cons, then they can start to lose the mentality that us weather folk have the easiest job in the world. We can be wrong half the time and still have a job (that saying is not old right? Some people get to have spell check proofread their work, we on the other hand have to deal with the forces of nature)

  • http://www.convectiveaddiction.com Jesse Risley

    Good article Patrick!

    This is a tough call, but based on 00z data tonight, along with the incoming RUC variables, if it were my call I would err on the side of caution and hope that it’s better to be safe than sorry. Given the fact that the parameters are lining up across the region for a potentially respectable severe weather event, and the models do at least show that a threat exists, better to highlight the risk area and note that the parameters are forecast to be ripe for an event than to be sorry and end up being too persnickety, perhaps missing a target with a forecast that is too narrow.

    If we could get more people to understand that this model business is somewhat just “pretend” until the event unfolds, and that it’s a best guess at the dynamics in play, then the meteorological community would stand to get much less criticism. At any rate, highlight the risk area based on the prime thermodynamic and kinematic environment and hope for the best – that’s my call.

  • http://www.facebook.com/jdrenken7 Joseph Renken

    Awesome write-up!

    I am a spotter for Central MO and Accuweather.com supermoderator who’s passion is the weather. Might I add that you didn’t even hit on the low/mid-level cloud deck that might hamper this situation even more. As you said in the Part 2 blog…I’m not stating it won’t happen if the cloud deck is there…just not as severe.

    The biggest thing is that we get the word out to those ‘in the zone’ and pray that they have severe preparedness plans drawn up. It’s going to be a rough and wild ride for sure!

  • Michael

    Issue Moderate Tonight with strong wording then look at VIs Sattelite first thing in the morning and see what the Cloud Deck is gonna do. Then decide whether to go High or Stay Moderate tomorrow. Tough setup for tomorrow looking at tonights 0z NAM

  • David

    Are these model sounding plots only available to the SPC? I love the observed sounding plots on the SPC website and have been searching for model soundings like them. Great write-up by the way! Was out on V2 last year with the MGUAS sounding team but was not able to make it this year

  • http://ddwxblog.blogspot.com Daniel Dix

    Well put concerning tomorrow’s event. One thing after years of forecasting severe weather in the Plains/Midwest is to anticipate many scenarios. When a ‘classic’ setup like this occurs it boils down to timing and boundaries. Typically, as is the case right now with initial WAA thunderstorms into the morning hours will either potentially lower the threat, or can actually increase the potential despite many meteorologists writing it off. Morning precip that ends allowing for clearing skies gives way to some incredible boundaries for storms to later focus upon. The key is where they form and can you get to the right one(s) in time. As we used to say in the office, “morning rain, afternoon pain.”

    One thing learned is hourly HAND analysis was always superior to any model mesoscale analysis. One to sometimes a 1/2 millibar analysis would be done as well as 1 deg temp and dew point contours. Amazing what you find along with vis imagery and clear-air mode radar to compliment.

    Good luck!!

    Daniel Dix
    @DDwx

  • Danny Murphy

    Nice article Patrick. I am a few months into trying to interpret a skew-T and only have touched the tip of the iceberg from what you have mentioned in the different soundings. I have gotten within the ball park on some of my forecasts, but further study would be beneficial. Thanks for the ins and outs of tommorrows soundings and what to look for.

  • http://www.patricktmarsh.com pmarsh

    The software used to generate these sounding plots is a piece of internal software at the Storm Prediction Center. We are working on ways to try and generate model soundings using this software and will provide them on the web. However, finding computational resources is the main hold up. Hopefully we’ll have this working before the end of storm season!

  • http://www.patricktmarsh.com pmarsh

    I couldn’t agree more about hand analysis. All of my students know how much of a fan I am and (initially) dread having me as an instructor because of the importance I place on it. By the end of the semester they are converted and begin to appreciate the value of actually looking at the data themselves instead of taking a computer at face value!

  • http://www.patricktmarsh.com pmarsh

    I’ll certainly try to find time to do a post on sounding analysis in the coming weeks! Feel free to ask questions!

  • Tim

    First..OUTSTANDING Blog! And..Go ahead, get more technical!

    I’m not within the forecast zone for tomorrow, but my interpretation and examination of the last 4 model runs..NAM/GFS/RUS/SREF all leads my thinkings to strongly favor the to “where” the highest THETA-E ridge sets up along with the highest EHI/SWEAT index’s pool…. that is NE OK.just S/SW not north! …High Risk by Day 1 at 18Z

  • http://www.KMIZ.com Jeff Huffman

    Based on my tendency to place a higher value on analogs, I predict this becomes more of a latitudinal outbreak and has trouble spreading north due to the occlusion of the low. This seems to be the pattern for events coming out of an El Nino winter. The recent shot of abnormally cold air in the Midwest and Ohio valley will be tough to erode leading to a more dynamic warm front than cold front/dry line. I would suggest a mod or high risk area drawn 100 miles either side of a line from OKC to ICT to SGF to CGI. I would cut off slight risk north of I-70 in KS and north of US HWY 36 in MO.

    Great blog btw!!!

  • http://www.mhartman-wx.com Matthew K. Hartman

    My one concern is moisture return. You elude to this, but it’s really going to depend how quickly tonight’s convection pushes east-northeast with the warm front and where clouds can thin enough for maximum heating. The 00z NAM and GFS this evening are both a little bit further east with the dryline. Contrasting the soundings from the NAM and GFS to me, it looks like the NAM wants to mix out the dryline and convect earlier than the GFS (between 18 and 21z). The NAM also doesn’t push the 60 degree dewpoints as far north into KS. With that, I’d favor N-Central OK for a potential target, if I were to go out. The GFS, on the other hand has 60 degree dewpoints well into KS, placing areas just west of Wichita in a decent threat.

    Honestly, I think it’s gonna be wherever the dryline bulge occurs and where those higher dewpoints setup.

    Also, the EHI’s on the NAM look strange tonight on the 00z NAM. There’s a narrow ribbon that develops east of Dodge City around 18z, then disappears by 00z, when the main area of high EHI (7+!) then appears from Wichita and eastward. Not sure where that narrow ribbon is coming from (maybe just from the center of the Low) but that may be something to watch for on the Mesoanalysis during the mid to late-afternoon. That could kick things off a little earlier.

  • Tim

    Well, Looks like SPC pulled the gun “earlier” than I had speculated above, but right in the area I had about forecasted the HIGH Risk would be highlighted. Going to be a wild ride on Monday…

  • http://www.mhartman-wx.com Matthew K. Hartman

    Good luck to everyone going chasing tomorrow. Out of all the areas in Oklahoma to chase, the northeast is the worst. :) Poor road network, hills, trees, and water. Not ideal for V2, but with this kind of setup, I can definitely understand them going for it.

    These hodo’s looking amazing!

  • http://www.spc.noaa.gov Greg

    Great comments on this post! And to think the only visuals are forecast soundings and hodographs. Wow!

    In hindsight, the analog of May 8, 2003 at T-48h was an eye-opener for me. There are two other aspects of this event that stand out from a short-term forecast perspective:

    1) I took the time to draw a detailed full-CONUS composite map at 8am CDT, Monday, May 10, 2010. To do this right usually takes me about 45-50 minutes. So, just before a FEMA briefing at 9am, I took a look at what I had in front of me and was stunned. Staring me in the face was a “textbook example” of a classic Southern Plains severe weather outbreak scenario! There was little doubt in my mind that Oklahoma and parts of Kansas would experience significant severe weather before the day was out.

    2) At HWT map discussion around Noon CDT, Monday, May 10, 2010, we reviewed the morning observed and forecast soundings. The hodographs for parts of central Oklahoma from a variety of models all showed tremendous low level shear and pronounced curvature. This not only supported tornadoes, but strong to violent tornadoes. Storm motions were also ominous, with speeds exceeding 50 knots in some cases. Again, an analog helped drive the point home. One of the forecast soundings found an analog for a sounding taken in Dayton, Ohio on the evening of April 3, 1974 – The Super Outbreak.

    As storms initiated in western Oklahoma only a short time later, I decided that any updraft initiating within 50 miles west-southwest of Norman would have to be taken very seriously (response time would be extremely short given those forecast cell motions!). I sent a text message to my family a little after 2pm stating that tornado potential in Norman around 5pm would be very high and to maintain vigilance and be ready to take cover should a thunderstorm move in our direction.

    That’s not prophetic, that’s modern meteorological analysis and forecasting at its best!

    Thanks for the opportunity to comment on this event and on meteorology, in general, Patrick.