Alert archive / Texas / Mesoscale Discussions in 2011

Mesoscale Discussion 696

May 6, 201117 counties in Texas

The Storm Prediction Center issued this mesoscale discussion at May 6, 2011, 1:41 PM CDT for 17 counties in Texas. It was in force for 2 hr.

The area

The outline as issued.

The facts

Issued
May 6, 2011, 1:41 PM CDT (18:41 UTC)
Expired
May 6, 2011, 3:45 PM CDT
In force
2 hr
Issued by
the Storm Prediction Center

Counties Coke County, TX, Crane County, TX, Crockett County, TX, Edwards County, TX, Glasscock County, TX, Irion County, TX, Midland County, TX, Pecos County, TX, Reagan County, TX, Schleicher County, TX, Sterling County, TX, Sutton County, TX, Terrell County, TX, Tom Green County, TX, Upton County, TX, Val Verde County, TX, Ward County, TX

The radar

The San Angelo radar (KSJT), 134 km from the middle of the area, began a volume at 18:43 UTC, the scan nearest the moment this went out.

Open the radar archive at this moment

The archived warnings, watches and discussions in force at that minute are drawn over the scan, this one among them.

The nearest sounding before it

Del Rio, TX (KDRT), launched 12:00Z, 6.7 hours before the alert went out and 154 km from the middle of its area. This is the routine balloon launch nearest before it, the air the forecaster had in hand, not a measurement taken for the alert.

Skew-T log-pSkew-T log-p diagram, Del Rio, TX at 12:00Z on 2011-05-06Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel. CAPE 325 joules per kilogram.LCLLFCEL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°0°10°20°30°40°
Temperature in red, dew point in green, the mixed-layer parcel dashed.
HodographHodograph, Del Rio, TX at 12:00Z on 2011-05-06The wind through the lowest 10 kilometers. Zero to 1 km storm-relative helicity 159 square meters per square second.19395878Sfc1 km3 km6 km9 kmRMLM
The wind turning with height, colored by layer: ground to 1 km, 1 to 3 km, 3 to 6 km, 6 to 10 km.
Mixed-layer CAPE
325 J/kg
Mixed-layer CIN
-416 J/kg
Mixed-layer LCL
851 m above ground
0-6 km bulk shear
26 kt
0-1 km storm-relative helicity
159 m²/s²
0-3 km storm-relative helicity
252 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0

Open this sounding in Storm Lab

The text

As transmitted, in the capitals the NWS used until 2016.

792 
ACUS11 KWNS 061841
SWOMCD
SPC MCD 061841 
TXZ000-062045-

MESOSCALE DISCUSSION 0696
NWS STORM PREDICTION CENTER NORMAN OK
0141 PM CDT FRI MAY 06 2011

AREAS AFFECTED...PORTIONS OF SWRN TX

CONCERNING...SEVERE POTENTIAL...WATCH UNLIKELY 

VALID 061841Z - 062045Z

WHILE AN ISOLATED SVR STORM OR TWO WILL BE POSSIBLE THIS AFTERNOON
OVER PORTIONS OF SWRN TX...THE ISSUANCE OF A WW IS UNLIKELY.

THE INFLUX OF A PARTIALLY MODIFIED GULF AIR MASS ACROSS PORTIONS OF
SRN TX IS SUPPORTING A FAIRLY WELL-DEFINED MOISTURE GRADIENT ARCING
ENE TO WSW ACROSS THE EDWARDS PLATEAU TOWARD A WEAK MESOLOW 10 W OF
6R6...AND EXTENDING FARTHER SOUTH ALONG THE E-FACING SLOPES OF THE
NRN MEXICO MOUNTAINS. THIS AIR MASS IS CHARACTERIZED BY SFC
DEWPOINTS IN THE UPPER 50S TO LOWER 60S...CAPPED BY AN ELEVATED
MIXED LAYER FEATURING MID-LEVEL LAPSE RATES FROM 8.5 TO 9 C/KM PER
12Z OBSERVED SOUNDINGS. THESE FACTORS ARE SUPPORTING MODERATE
INSTABILITY /MLCAPE VALUES OF 1000 TO 2000 J PER KG/ INVOF THE MOIST
AXIS.

CONVECTIVE INHIBITION HAS BEEN SLOW TO ERODE THUS FAR WITHIN 60 NM
NE OF THE RIO GRANDE RIVER OVER THE EDWARDS PLATEAU...OWING TO
PERSISTENT STRATUS SINCE THE MORNING HOURS. HOWEVER...GREATER
INSOLATION FOUND NEAR A SFC CONFLUENCE AXIS EXTENDING NNW OF THE
AFOREMENTIONED MESOLOW IS SUPPORTING LESS CINH OVER THE NWRN
PERIPHERY OF THE MOIST AXIS -- I.E. OVER ERN PORTIONS OF THE EDWARDS
PLATEAU INTO THE TRANS-PECOS REGION. AS SUCH...RECENT VISIBLE
SATELLITE IMAGERY DEPICTS THE DEVELOPMENT OF A CU FIELD AROUND AND
JUST W OF FORT STOCKTON.

THERE WILL BE THE POTENTIAL FOR ONE OR TWO DEEPER CONVECTIVE PLUMES
TO EVOLVE FROM THE CU FIELD BETWEEN 20Z AND 22Z...AS AFFIRMED BY
RECENT CONVECTION-ALLOWING MODEL GUIDANCE. ANY CONVECTION WILL
LIKELY BE HIGHER BASED INITIALLY WITH THE POTENTIAL FOR GUSTY WINDS.
HOWEVER...AS THE ACTIVITY IS STEERED EWD OVER THE EDWARDS PLATEAU
AND INTERACTS WITH THE RICHER LOW-LEVEL MOISTURE AND GREATER
INSTABILITY...IT WILL HAVE THE POTENTIAL TO STRENGTHEN AND POSSIBLY
BECOME SEVERE POSING THE THREAT FOR DMGG WINDS AND LARGE HAIL. WHILE
THIS POTENTIAL WILL BE SUPPORTED BY NOTABLE DIRECTIONAL SHEAR IN THE
0-3-KM-AGL LAYER PER AREA PROFILER DATA...THE RELATIVELY WEAK
MID-LEVEL FLOW WILL LIKELY TEMPER THE OVERALL SEVERE THREAT.
ADDITIONALLY...WITHOUT ANY SUBSTANTIAL DEEP-LAYER FORCING...THE
COVERAGE OF SVR STORMS IS EXPECTED TO BE ISOLATED...AT MOST. AS
SUCH...A WW IS UNLIKELY.

..COHEN.. 05/06/2011

...PLEASE SEE WWW.SPC.NOAA.GOV FOR GRAPHIC PRODUCT...

ATTN...WFO...EWX...SJT...MAF...

LAT...LON   29710172 29770240 30310299 30900330 31630307 32040210
            32200079 31690008 30790009 30010025 29540070 29470124
            29710172

Nearby

Mesoscale Discussions in Texas, 2011Every mesoscale discussion in 2011

Sources

The product and its follow-ups from the Iowa Environmental Mesonet's archive of National Weather Service and Storm Prediction Center text; the sounding from the Mesonet's radiosonde archive; radar from the NEXRAD Level II archive.