Procedures and perspective displays set up. Time to start watching current storms.

Warned on this storm with a 5 sigma lightning jump. It appears to be a right-mover.

Lynford

3rd severe warning for a hail core over southwestern Ottawa county, moving northeast. Lightning Jump Algorithm jumped over 4 sigmas around the time when the hail core aloft looked the best. ProbSevere jumped from 69% to 92% with MESH building to over 1.50 inches. DTA came out well in advance though it overlaid with a 2nd, more appropriate DTA, related to the more intense storm approaching from the south. Although fairly large area of 60 dBZ above -20 C, and MESH at 1.50 inches, only used 1 inch hail in warning due to lack of large hail reports during the afternoon.

Brick Tamland

While observing the Probability of severe throughout the event today, I have noticed that it seems to do well when there are discrete or individual convective cells and was useful in the warning operations when combined with the base data we were looking at interrogating the storms.  The storm we originally warned on seen in the image below had high prob severe values and verified with a 60 mph wind gust report.

However, later in the event the convection became linear and looking at the base data interrogating the storm there was not evidence supporting a warning along the line as the 50dbz cores were relatively low and the line of storms had become outflow dominated with the outflow boundary pushing well away from the storms.  The probability of severe though was showing values near 85% along the entire line.

So I think it is important to note for the users of this product that when the convection becomes linear the probability of severe may not be as useful and should not be as relied on compared to individual convective storm environments.

Jack Bauer

Another cell developing to the east of the two previously warned cells provided another opportunity to use both ProbSevere and Lightning Jump Detection Algorithm in conjunction to issue a Severe Thunderstorm Warning.

Really started to see an increase in the mid level reflectivity on the storm and during that time the ProbSevere increased from 8% at 2204Z to 64% at 2208Z.

At that point, we were starting to think about issuing a SVR and as we were making that decision, there was a 5 sigma lightning jump noted. That data arrived before the next version of ProbSevere arrived but tied in with the increase shown in the previous couple scans. At that point, we decided to issue the SVR and our thought was confirmed by the next version of ProbSevere increasing to 84% with a MESH value of 1.25″.

The warning was issued at 2217Z and the ProbSevere value reached 94% with a MESH of 2″ as the warning was issued.

Although the experience with these two products has been limited thus far, they have shown to work well in conjunction with the radar analysis to lead to increasing confidence on issuing a warning during rapid intensification.

-SRF

With the move to ICT we were able to issue our first warning of the project. The storm that was previously discussed re-intensified after splitting. The increasing reflectivity aloft led to the MEHS data to give a hail estimate of 1.55″ and pushed the ProbSevere up from 58% to 95%.

Thus, a warning was issued for that cell.

To the northwest, a storm in DDC started to take a right turn right around the same time as a series of 2-3 sigma lightning jump values (orange in bottom left screen). Those values occurred as the storm intensified on radar and led to the ProbSevere values rising from 80% to 97% as it was nearing the cwa. Also, notice the overshooting top detection in the lower right screen.

With all of those values and the expected movement into the cwa, issued a warning for the ICT area for the storm.

-SRF

Looking back at the big picture and focusing on the GOES-R convective initiation, there was not much showing in our area of responsibility (TOP) but further south in northern Oklahoma I noticed some increasing probabilities at 1900 UTC.

15 minutes later at 1915 UTC the CI probability jumped to 90% on the east side of a cluster of identified clouds while there were also 40% probs on the west side.

Immediately after this time it was evident there was convective development was occurring as seen in this 2000 UTC satellite image below.

By 2030 UTC some CG lightning strikes were noted seen in the image below.  Radar at 2030 UTC also included.

Jack Bauer

With limited convection in the OAX area, we have moved over to ICT. The ICT CWA is along the same boundary, but now is on the southern side.

Taking at the quick look at the radar, there is a strong thunderstorm over the north-western part of the CWA. I decided to use the ProbSevere data as a quick overview and found the MRMS MESH data (hail size ~1″) to be very helpful in giving a quick look at the current expectations on the storm. I also found the satellite indicators to be helpful with the switch to indicate the current state of the storm (Mature).

Starting to see some increase in the eastern cell while typing this and will follow up this blog post with additional information. -SRF

CI was 81 at 1830z in northern Jeff Davis County (first image). By 1901z 0.5 deg reflectivity (image 2) showed the first greater than 35 dBZ returns. By 1945z the Probability of Severe was 27 percent (image 3). Severe hail, 1.75 inches, was reported at 2008z through 2025z (image 4). By 2049z the storm had a massive Three-Body Scatter spike (image 5).

Time from the 81 percent chance of CI to hail report was 98 minutes.

Time from the first 35 dBZ returns to hail report was 67 minutes.

Time from 27 percent Probability of Severe to hail report was 23 minutes.

-Lynford

Last three images from Vivian Darkbloom

I like the gradual color change and polygon thickness increase as the probabilities increase. See the image below for an example of the lower prob (thin blue) vs the higher prob (thick pink) and some gradients in between. This allows a warning forecaster the opportunity to quickly filter the sub-severe storms and focus on the potential for stronger convection in other areas.

Brick Tamland

Noticed how a storm may briefly increase to 40 flashes/min, yielding a level 3 DTA for a cell. See the images below which highlight that although the DTA threshold was met for briefly for a few minutes, the successive flash rates dropped below the 40 flash/min threshold for minutes thereafter. The DTAs may be more useful for operational forecasters if the valid time were reduced from 45 mins to 30 mins. This would reduce the amount of products that may clutter up the radar interrogation process.

Brick Tamland