WFO OAX-Finally, a CTC Fail!

No computer-based algorithm is perfect, right?  We had a failure of the Cloud Top Cooling (CTC).  Here is a CTC image from 2345Z, in the top right panel:

Cloud Top Cooling (CTC). Values in York County, NE are over -30C/15min.

The developing storm over York County has values over -30C/15min, which is usually a strong indicator of a developing severe thunderstorm.  As this storm developed and approached Seward County from WFO GID, a warning was issued based on CTC.  Maximum Expected Size of Hail (MESH) was 0.87″ and increasing.  However, as the storm entered Seward County, it weakened.  No severe reports were received, and the MESH dropped pretty rapidly.  Here is an image as the storm entered the CWA:

0018Z KOAX 0.5 degree Base Reflectivity image.

The moral of the story?  You can’t win ’em all, CTC!–Gordon Strassberg for WFO OAX.

CI product over E-Nebraska

The cold front over NC-Kansas and SE Nebraska was monitored for further development. As expected, storms began to build SW-wards towards the KS boarder and CI products were effective in highlighting the area with highest probabilities for potential development along that boundary.

The event occurred over Clay and York counties (Nebraska). A series of images will be added to show the evolution:

UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2232 Z
UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2245 Z
UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2302 Z

Roughly 30 min before surface reflectivity at -10C isothermal level revealed first signs of development, the CI product highlighted both counties with 50-60 % probabilities. The cloud top cooling product showed values of -15 to -25K/15 min at 2315Z (not shown) and the first significant reflectivity signal (56 dbZ ) became visible at 2330 Z. At 00Z onwards a 63 dBz cell evolved out of that NE of York.

Helge

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OAX: Cloud-Top-Cooling (UW-CTC) Success!

Issued a severe thunderstorm warning strictly off of explosive CTC at 2315 UTC (previous post), with very little showing up on radar at the time.  As would be expected, through the following 15-20 minutes, the storm exploded, with MRMS MESH spiking up to 1″ by 2334 UTC, and a quarter size hail report by 2336 UTC.  This gave us 21 minutes of lead time from the initial warning issuance off of CTC.  Would have likely issued the warning based on traditional base products by 2325 UTC, 10 minutes after the CTC-based issuance.

2334 UTC.

Comparison synthetic-real IR over E-Nebraska

The area over E-Nebraska was monitored for initiation. The synthetic images did a pretty good job in timing of thunderstorm development. The real development occurred only slightly to the north to what the synthetic ones proposed. The model forecast however overestimated the development along the cold front over C/S Kansas, where warm mid-levels prevented DMC of developing until now (although showers finally try to form at 23Z onwards).

Synthetic IR/WV in the upper left and right with real data in the lower half

Helge

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OAX: MRMS MESH Success

A report of quarter size hail came in around 2230 UTC, approximately where MRMS MESH estimated 1-1.25″ hail (lower left panel).

2226 UTC MRMS MESH. Quarter size hail was reported approximately in the same location as the MESH was estimating 1-1.25" hail.
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Fire in Catron county, New Mexico

Between 2130 and 2145 Z another burst of the extensive smoke plume occurred, which was also captured by the CIMMS Cld Top Cooling product with values mainly below -5K/15 min.

Smoke plume with CIMMS Cld top cooling in the upper right

Helge

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DDC: Initiation in C-Kansas imminent?

Latest VIS imagery indicates a rapid increase in convection along slowly SE-ward progressing cold front, namely over Hodgeman, Ness and Rush counties. UAH-CI product already showed modest probabilities (50-60 %) for CI with no reflectivity yet present in local radar data.

UAH-CI product placed in the upper left corner at 2130 Z

Latest HRRR is a bit more optimistic with SW-ward zipping convection compared to OUN WRF. Still unsure if storms can initiate in that area with warm mid-level tongue partly covering the cold front/dry line. Strong shear now gradually moving in from the west, so increasing storm organization is likely in case of initiation.

Helge

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Moving Ops to Central Plains…

At about 2130 UTC we decided to end operations over the Carolinas and move to the central Plains.  McKinney & Hirsh are working the Hastings CWA (GID) while Strassberg & Kleinsasser are covering the Omaha CWA (OAX).  Our to observers Helge & McCormick are checking out DDC (though concern over the cap in this region might move them to CO or Iowa).

Meanwhile the SPC issued a watch for the region as well…

SPC Watch for 2100 UTC to 0400 UTC on 23-24 May 2012

-K. Calhoun

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ILM: MRMS Struggling with 60dbz Echo Tops

The top image is the MRMS estimate of the 60dbz echo top of a storm over Wilmington NC CWA, estimating the 60dbz echo top around 6500 ft at 2022 UTC on 5/23.  However, the bottom image is the corresponding KLTX 8.0 degree slice, indicating 60-62dbz to at least 29,000 ft.  At least in this instance, the MRMS 60dbz echo top algorithm did not perform well.

2022 UTC MRMS 60dbz echo top of only 6500 ft.
2023 UTC KTLX 8.0 degree slice indicating 60-62 dbz to at least 29,000 ft, proving the MRMS 60dbz echo top algorithm incorrect in this instance.
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RAH: Where is Raleigh, NC??

We got some reports of large hail in Raleigh, but I couldn’t seem to find it on the map (top).  I needed to zoom in (bottom) quite a bit to see the label for the second largest city in NC.  AWIPS II developers…can this be fixed?  Zooming out should show the major cities, but it currently shows random small towns.