Time of Tornado 2

The 0-2km product still highlighted all three parts of the line, and reflectivity still shows the line breaks up north, but the velocity product itself is not showing much gate to gate tight mesos there, despite the higher AzShear numbers.

Charley

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West of Tornado 1…several areas of interest…then more discrete cells to the southeast and east

The merged 0-2km AzShear product shows threat more areas of interest along a north/south line crossing MXX.  The southern one obviously is the strongest, but one just north of the radar and one farther north of the radar has reflectivity and velocity tags indicate some potential for tornadogenesis.  Reflectivity shows line breaks and a convergence zone at enough of an angle to the 0-3km shear vector to induce some stronger mesos.

The 3-6km shear vector focuses more on the southern one of those three.

 

Charley

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ILX All_Layer CAPE Comparison

Taking a look at a quick comparison example of when the model fill-in of the All_Sky CAPE product may not be the best solution. In this example, an ongoing MCS was diving south through north central IL earlier this morning before it dissipated rapidly over the central part of the state. The GFS model struggled depicting the rapid de-escalation of said storms, and attempted to stabilize much of the ILX CWA in its wake. Unfortunately, this led to quite the gradient between areas where clouds prevented in-situ satellite observations to be utilized in the All_Sky CAPE product. Taking a look at the SPC Mesoanalysis (RAP) output in image 2 for comparison, the more accurate CAPE values across eastern IL should be closer to the 2500 – 3000 J/KG range while the ALL_Sky CAPE layer (Image 1) is showing 1000 – 1500 J/KG tops. A suggested best practice to overcome this discrepancy is to  include the AllSkyLAP Layer Cloud Type Image underneath any AllSkyLAP product so you can easily depict what is sensor derived and/or model output.

—————————————————————————————————Mountain Bone

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AzShear EOX high ahead of TOR…other factors point toward downstream TOR

AzShear product for EOX, showing higher elevation rotation, was strong for this cell as it was getting organized.  MXX was lower, but the merged shear product picked up on the high value.

Other Dual Pol factors indicated the supercell was starting to get ready to drop a TOR…with ZDR arc forming on the MXX radar.

A few minutes later, the MXX AzShear on the base tilt still didn’t show the high values until right at tornado time.

Then at time of touchdown, it showed a better max in the lowest tilt.

The merged 0-2km Azshear product then cycled down after that max, despite continued higher values from the EOX radar…in fact the trend was getting stronger from that radar, with peak values near 0.03 at touchdown time.  Sampling indicated the AzShear on the base tilt was at 1.7-1.8 km AGL at this time, so I would think it still would factor into the 0-2km AzShear product.

Charley

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Attempting to determine which weaker circulation is stronger

EOX radar depicted two distinct weaker circulations from circulations near the AL/GA border.  Both storms had similar presentation on reflectivity and at a broad glance, the relative strength of the circulations were similar.  The single radar azimuthal shear depicted that the southern circulation was stronger.  One remaining question though is whether the southern circulation was stronger based on proximity to the radar.

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Storm Merger

A storm merger was about to occur around 2200z in eastern MN as a northeastward moving reflectivity tag was moving toward the larger likely severe thunderstorm.  By 2206z after the merger occurred, the azimuthal shear sharply increased in the 3-6km layer, and radar velocity also showed mid-level rotation (not shown).  By 2212z, the azimuthal shear sharply increased in the 0-2km layer, with the low-level velocity (not shown) transitioning to covergent then rotational.

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AllSky CAPE high in one place low in another

cells persisting in far western CWA has high CAPE on latest AllSky product.  However, the line of storms that moved through the middle of the CWA is now in the eastern part and into ARX’s area.  Line continues to look severe, with AWOS in northwest ARX gusting to 52 knots, but CAPE not as high.

CHARLEY

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LSX Warning 1 (Mountain Bone)

SPS’s have been upgraded to a warning due to some interesting velocity couplets. At the time of the warning, the new Prob-Severe model had (ProbHail: 5%, ProbWind: 56%, ProbTor: 2%). At the storm’s severity peak, the new Prob-Severe model had (ProbHail: 8%, ProbWind: 78%, ProbTor: 17%). While the warning decision was made based on the velocity signature showcasing 30+ kts inbound with some broad rotation, the added confidence of the Prob-severe model assisted in “pulling the trigger” and likely provided several minutes of added lead-time in this scenario. Also taken into account was the understanding that it was the northern-most cell in a line that is moving into a favorable environment charactarized by ML CAPE values near/above 2000 J/KG based on the All-Sky LAPS analysis. A bit disappointed with the data latency of the new MDA product on this cell, with little to no MDA information available. The digital MDA has done a good job tracking the feature with only one hit available on the old version.

There was also a considerable lightning jump that occurred in this cell as it underwent strengthening.

Tree damage was reported within the warning shortly after it was issued.

22:34z: Due to persistent cycling and broad rotation, a “tornado possible” tag was added to the warning. This rotation is likely being spurred on by a combination of a cell merger and boundary interaction.

2250z: Warning continued upstream continuing the “tornado possible” tag. Still some broad rotation from boundary interaction. No gate-to-gate, but I feel that the Prob-Tor model is underduing things a bit. Possibly because the environment isn’t condusive to Tornadoes? At the time of issuance, the Prob-Severe model was showcasing (ProbHail: 9%, ProbWind: 68%, ProbTor: 3%). My forecaster prob-tor would be closer to 15% at time of SVR T-Storm issuance.

~2215Z: Spotter reported a brief tornado touchdown in a field on the east side of Rosebud, MO. Still trying to confirm the authenticity at this time. Screenshot above of possible Tornado spinup from the area of the spotter report.

Storm has weekend and become primarily a wind threat which should be coverable with an SPS. Will allow the warning to expire on-time.

 

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