OUNWRF over NE Colorado

OUNWRF evolves long-lived supercells over Morgan, Washington and Lincoln counties with a rapid eastward progression. This may place highest supercell risk a bit more to the north compared to theta-e difference forecast (mentioned in the blog entry below). Despite LCLs aoa 2.5 km and increasing DCAPE towards C/E Colorado, the WRF keeps max hourly wind speeds on the lower end side. Feeling is that initiation of WRF activity may be too optimistic/early with slow BL moisture recovery still underway.

OUN-WRF updraft helicity (upper left), surface hourly column hail (upper right), surface max hourly wind speed (lower left) and surface max hourly updraft helicity (lower right)

Helge

RAH: CTC provides >1 hr lead time on severe hail report

The CIMMS cloud top cooling algorithm first detected cooling rates of approximately -10 C/15 min with a thunderstorm developing across eastern Hoke and western Cumberland counties on the 1815z image. The algorithm continued to show strong cooling rates on the next two images with accumulated CTC values of approximately -30 to -35 C/15 min before the cell was dropped from the display after 1845z. A report of quarter sized hail was received in far southwestern Harnett county with this thunderstorm at 1937z, almost an hour and a half after the algorithm first detected stronger cooling with this storm.

Accumulated CTC values for a cell that produced severe hail.

Awaiting initiation over NE Colorado

Conditions gradually improve for thunderstorm development over NE Colorado although initiation may be delayed until the 23-00 Z time frame. Surface boundary pushed through as lee depression slowly consolidated over W-Kansas. 12Z Denver soundings showed steep lapse rates with a deepening and well mixed boundary layer. Numerous weak caps present (roughly at 700, 600 and 500 hPa).  CIMMS Cld top cooling product revealed numerous spots with moderately cooling tops in the order of -10 to -15 K/15 min with UAHCI CI product showing low to non existent probabilities. This may be the reason for growing updrafts before reaching one of those aforementioned caps, which suppressed further development. For the forecaster however this is already helpful to pinpoint the area, where enhanced cumulus growth occurs and where initiation may be the most likely.

Question now arises if moisture recovered since 12 Z. Surface dewpoints struggle to exceed mid to upper 30s with lower 40s now entering far NE Colorado as winds backs more to NE-erly directions in response to the consolidating lee cyclogenesis. However, products like the 780mb equiv pot temp and the theta-e diff show robust signals for available potential instability over far NE Colorado with an increasing trend during the following hours. In fact, latest HRRR forecast and the tongue of pot. instability seem to overlap nicely. Hence initiation seems possible around and south of a line Steamboat Springs-Denver-Deer Trail during aforementioned time frame. Incoming mid-level speed max pushes DLS aoa 80 kt, which is more than adequate for well organized storms.

Helge

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ILM: CTC Lends to Good MESH Lead Time?

In the 1815 UTC vis satellite image (upper right of top 3-panel), cloud-top cooling was on the order of -17C/15min with a developing thunderstorm.  By 1858 UTC, MRMS MESH product reached 1″ hail size (middle image), and just over 2″ hail size by 1906 UTC.  The UW-CTC product lead to 45-50 minute lead time for 1-2″ hail (as estimated by MRMS MESH).  This is one of many instances we’ve noticed the CTC give decent lead time for 1″ or larger hail.

1815 UTC. Rapid convective development as indicated by -17C/15min cloud-top-cooling rates.
1858 UTC. MRMS (multi-radar, multi-sensor) MESH (max estimated hail size) is estimating 1.02" hail, about 45 minutes after rapid CTC.
1906 UTC. MRMS MESH now estimating 2.13" hail, about 50 minutes after initial rapid CTC.

RAH: MESH success

The MRMS MESH algorithm predicted a maximum hail size of 1.34 inches with a thunderstorm across far southwestern Harnett County on the 1930z image. A report of quarter sized hail was received with this storm at 1937z to the southwest of Pineview, NC.

MESH values for 1930z across southern Harnett County, NC.
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RAH: CI algorithm sucess over North Carolina

The UAH-CI algorithm displayed two areas with high strength of signal values (64 and 92) across southern Cumberland and western Sampson counties on the 1702z image. These cells intensified quickly into two thunderstorms and a report of penny sized hail was received from the eastern storm at 1823z, more than an hour after the algorithm first detected these thunderstorms.

RAH: CTC algorithm sucess over North Carolina

The CIMSS-CTC algorithm showed cloud top cooling rates of between -10 to -15 C/15min on several images with a thunderstorm developing across Sampson county in North Carolina. The CTC first appeared on the 1715z image and continued to highlight this cell through the 1815z image. As the algorithm continued to show moderate cooling rates with the cell the radar presentation became more impressive and a three body scatter spike developed with the cell. A report of penny sized hail was received with this cell 1823z 5 miles WSW of Newton Grove, NC.

BIS: 3D-VAR Max Updraft & Max Divergence…Good “Heads Up”

It’s becoming increasingly evident that 3D-VAR’s maximum composite updraft and max divergence above 8km can be utilized as a good “head’s up” display of the largest storms on the scope.  This can be seen in the image below.

Cluster of storms ESE of BIS on the evening of 5/22. Upper left (base reflectivity), upper right (max divergence above 8km), lower right (max composite updraft speed).

BIS: 3D-VAR & Rapid Storm Growth

Refer to the northern-most storm in the below images.  Between 0045 and 0100 UTC, explosive thunderstorm growth occurred southwest of BIS, rapidly becoming severe as evidenced by 50-60+ dbz well above the -20 and -30C heights and mid-level rotation per BIS SRM.  3D-VAR products such as maximum composite updraft speed and max divergence above 8km picked up on this explosive thunderstorm growth, as shown in the 4 images below.

0045 UTC. Base reflectivity (upper left), max divergence above 8km (upper right), max composite updraft speed (lower right).
0050 UTC. Base reflectivity (upper left), max divergence above 8km (upper right), max composite updraft speed (lower right).
0055 UTC. Base reflectivity (upper left), max divergence above 8km (upper right), max composite updraft speed (lower right).
0100 UTC. Base reflectivity (upper left), max divergence above 8km (upper right), max composite updraft speed (lower right).

MR/MS MESH showed up to 2.76 inches with the stronger of these two cells.  The cell to the southeast produced golf-ball sized hail, per spotter reports.  This would lead me to believe that the stronger cell is no doubt producing large hail and I would feel confident issuing a strongly-worded SVR.

HIRSCH