Unfortunately the 1830Z pass of the NPP just barely skimmed the ICT area. The only points available in relatively clear air were on the western edge of the swath, so we are taking the data with a grain of salt.

The sounding after editing the surface data (used the nearby Dodge City obs)

Overall the sounding doesn’t look too terrible. The CAPE is way higher than the GOES-R LAP…in fact it was around double.

To compare a real (and way more impressive) sounding, here is the 18Z KOUN obs:

which had SB CAPE over twice the GOES-R LAPS values There was decent cloud cover at the time.

For what it’s worth, the 18Z RAP analysis was overdone in both locations, though much closer (within ~400 J/kg) near OUN compared to about 1,000 J/kg near our NUCAPS sounding.

-V. Darkbloom

First glance at GOES-R products indicates a CAPE gradient from around 700 J/KG for the southern portions of the GID CWA to about 200 J/KG for the northern portions of the CWA. We had a satellite data outage affecting CAPE/PWATs at 17Z. The southern portions of the CWA remain in an area of confluence between southwesterly flow DDC area and southeasterly flow from the ICT/TOP area. Satellite PWATs remain above 1 inch across the region with surface dewpoints in the upper 50s to lower 60s. Initial look at radar indicates multicellular appearance for southern portions of GID. Viewed the adjusted NUCAPS sounding around 19Z and found CAPE values near 2000 J/KG. Biggest threat appears to be large hail, damaging wind gusts, and isolated tornadoes.

So far have noted a few hail cores aloft with All-tilts though ProbSevere has remained mostly below 50%. The westernmost SVR warning (#2) had 60 dBZ to near -25 C. One cell approaching from the south possessed rotation in the lower levels and thus we issued a TOR warning. ProbSevere for the TOR built as high as 64%.

Brick Tamland/Alexander Darkband

This being my first day really focusing on the ETN data, my initial thoughts on the thunderstorm alerts in the warning operations environment is that is can be useful to identify when storms are becoming electrified but I find myself gravitating to only looking at the DTA (Dangerous Thunderstorm Alerts) as opposed to all three thunderstorm alerts. As others have mentioned I concur that the length of time that the alert boxes remain on the screen is entirely too long (45 minutes).  In some cases, the storm has completely dissipated or moved well outside of the alert box and the boxes become more of a distraction in my opinion.  I think a reasonable time frame for the alert boxes would be 15 minutes or 20 minutes max.

Jack Bauer

Now evaluating this cell. Rapid intensification past 3 scans. Prob of Svr now 84%. 2 sigma lightning jump.

Lynford

First warning issued. Solid structure with good storm top divergence and deep mesocyclone. Prob of Svr was 81% at 1944z with a MESH 1.10 inches. 1 sigma lightning jump at 19:37 and 19:39z.

Also saw a 2 sigma jump at 1938Z, seen on the image below.

A tornado warning was issued just after 1950Z based off the latest radar signatures.

Shortly after that and as the tornado touched down, there was a 3 sigma lightning jump.

classic gate to gate rotation. 2 inch hail reported with this cell.

Lynford/SRF

Upon sitting down at the desk today initialized as the Wichita WFO (ICT) there was a tornadic storm already in progress in the northern portion of the CWA, which had a ProbSevere of 82%.   Since we are just getting set up and getting familiar with the environment we are going to assume that storm has been covered and monitor new convection as it develops.

The water vapor imagery is showing a deep upper low over northeast CO with shortwave energy rotating across the central plains which is helping to initiate convection early this afternoon.

A special 18 UTC sounding from OUN shown below revealed strong instability with MUCAPE of around 2200 J/kg and favorable shear for tornadoes with 0-1km SRH values just under 200 m2/s2 and good directional shear in the lowest 2 km.

An initial look at the Convective Initiation product revealed some probabilities above 70% near Wichita at 1900 UTC and further to the west over the eastern portion of DDC CWA.

The GOES-R LAP CAPE product reveals instability is not quite as high over our area (but the trend has been increasing with more clearing of the clouds) compared to further south over OK but combined with the shear will be enough to support severe convection through the afternoon.

Jack Bauer/V. Darkbloom

At 2353 UTC, a developing thunderstorm was seen on radar southeast of Lubbock.  At 0007 UTC, lightning jump data increased to 4 sigma.  At this same time, flash density increased to 70-80 flashes.  A warning was issued at 0011 UTC, based off the lightning data and radar data (50 dBz core at 33000 ft per MAF and low Zdr values per LUB).  ProbSevere increased to 87% at 0007 UTC also, and remained above 84%.  The storm took on a classic supercell structure and later produced a tornado.

Had a storm report come in from 2mi north of Roscoe at 2350Z with 1″ hail within our warning. As indicated in the image below, the ProbSevere data was still indicating 95% severe probability at that time. That provided around 20 minutes lead time from both when the warning was issued and the ProbSevere value jumped above 90%. It looks like the MRMS MESH data was overestimating the hail size slightly (1.34″). -SRF

We decided to issue a warning at 2323 UTC for Lubbock county on a storm that was moving eastward towards the city of Lubbock. The ProbSvr increased to around 59% at 2316 UTC with a MESH of 0.76 inches.The PGLM data and Lightning jump data at 2316 UTC were not very impressive with flash density less than 10 flashes (upper left in the image below) and the Lightning jump showing values less than 1 sigma (lower left in the image below).

Based on the base radar data from the all tilts display off of the MAF radar (LBB was too close to the storm and not able to see the top of the storm), we began writing up a severe thunderstorm warning at 2320 UTC which was issued at 2323 UTC.  It was noted that at 2322 UTC the Lightning jump algorithm displayed a 2 sigma value on the storm (we did not see this is real time as we were writing up the warning), while the PGLM showed an increase in flash density to around 23 flashes which was still relatively unimpressive.

In this instance the PGLM and Lightning jump did not really provide any significant factor in the warning decision although the 2 sigma Lightning jump is a positive sign but in this instance did not outperform traditional base data storm interrogation.  A large hail report of 1.75 inches was received just southwest of Lubbock at 2333 UTC.

Jack Bauer