Thunderstorms, some severe, may produce heavy to excessive rainfall and isolated flooding over portions of the Southern Plains today and Saturday. Dry conditions, combined with gusty winds and low relative humidities will continue to support an elevated to critical fire weather threat in the Desert Southwest into to early next week. Read More >
Storm Total January 13-15 2010 | Oso Creek and Staples at 19.95 feet | Oso Creek and Staples |
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Introduction
A series of short wave troughs affected South Texas during November and December 2009 resulting in above normal precipitation and notably alleviating residual severe drought conditions. Most of these events consisted of stratiform precipitation over a low-level cold air mass. The coldest air mass of the season previously brought arctic temperatures to the region between January 8 to 10th, not felt since the years of 1989 and 1998. However, this cold dome of air was completely mixed out prior to the onset a narrow area of rain on January 13th which allowed surface dew points to rise into the 60s F and layer precipitable water to reach 1.40 inches. The event on 14-15 January 2010 was the strongest in the series of troughs that occurred in an El Nino influenced jet stream pattern and resulted in heavy localized rainfall and significant cloud-to-ground lightning strikes. Widespread 2 to 4 inches of rain occurred across South Texas and 3 to 5 inches across the Coastal Bend. Local amounts up to 6 inches fell along the immediate coast. Soils were nearly saturated from the December rainfall and significant runoff caused sharp rises to creeks and eventually minor flooding to several rivers. In addition, localized rainfall rates of 1 inch per hour produced urban and small stream flooding. (see Local Storm Report below)
Medium range numerical weather prediction (NWP) advertised the potential for a significant rainfall event several days prior to January 15th. NWP quantitative precipitation forecasts (QPF) generally placed the axis of heavy rain from the waters of the Northwest Gulf to across the entire Coastal Bend. The 1200 and 1800 UTC 13 January NAM runs began to focus the axis of heaviest QPF across the interior coastal plains, eastern portions of the Brush Country and the northern Coastal Bend. GFS model QPF also began a trend of placing the axis across the northern half of the Coastal Bend and northwestward towards San Antonio. Corresponding predictions from the Hydrometeorological Prediction Center (HPC)kept the maximum across Corpus Christi but expanded the area north and westward. The ECMWF model was last to depict the heaviest axis inland from the immediate coast but this model, along with the GFS, was superior for the Coastal Bend. The NAM verified the inland axis of heavy rain better than the other models but had poor run-to-run consistency along the coast where the strong moist convection occurred.The short range ensemble forecast (SREF) runs were similar to the HPC forecasts but depicted lighter amounts.
KCRP base reflectivity loop starting 2132 UTC 14 January 2010 | KCRP base reflectivity loop starting 1206 UTC 15 January 2010 |
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GOES water vapor and wind loop starting 1715 UTC January 14 2010 | GOES water vapor and wind loop starting 1415 UTC January 15 2010 |
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GOES infrared and NLDN loop starting 2201 UTC 14 January 2010 |
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0000 UTC 15 January | 1200 UTC 15 January | 0000 UTC 16 January |
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Rainfall Reports (most of the rain occurred from 0000 UTC 15 to 0000 UTC 16 January)
SEADRIFT | 5.88 | GEORGE WEST | 2.86 |
CORPUS CHRISTI CWOP | 5.76 | VICTORIA RAWS | 2.81 |
CORPUS CHRISTI 6 WSW | 4.98 | PORT OCONNOR | 2.81 |
MATHIS | 4.72 | VICTORIA AIRPORT | 2.75 |
MATAGORDA ISLAND | 4.70 | ODEM | 2.51 |
PORT ARANSAS | 4.66 | GOLIAD | 2.45 |
PORT LAVACA | 4.34 | NUECES AT COTULLA | 2.43 |
COTULLA | 4.36 | GEORGE WEST | 2.44 |
ARANSAS | 4.30 | WESER | 2.30 |
CORPUS CHRISTI OSO BAY | 4.26 | ROBSTOWN AIRPORT | 2.20 |
INDIANOLA | 4.25 | COTULLA AIRPORT | 2.19 |
BISHOP | 4.19 | CORPUS CHRISTI AIRPORT | 2.16 |
TILDEN | 4.00 | ||
AUSTWELL | 3.89 | ||
CHOKE CANYON DAM | 3.78 | ||
ARANSAS PASS | 3.77 | ||
BLOOMINGTON | 3.73 | ||
FLOUR BLUFF | 3.68 | ||
CORPUS CHRISTI NAVAL | 3.66 | ||
ROCKPORT | 3.65 | ||
VICTORIA GUADALUPE | 3.57 | ||
BEEVILLE | 3.34 | ||
CHRISTINE | 3.24 | ||
KINGSVILLE NAVAL | 3.23 | ||
PORT LAVACA AIRPORT | 3.12 | ||
DILLEY | 3.10 |
0000-0600 UTC (6 pm to Midnight CST)
northward along the southern Coastal Bend producing rainfall rates of 0.50 to 1.50–in per hour. The precipitation
developed in a rapidly destabilizing air mass that responded to strong low to mid-level moisture advection,
increasing upper-level divergence ahead of a closing off upper-low in
region. Surface-based instability was marginal (200 J/kg or less) Thursday evening with the greatest values
over the
surface was considerable (see Bufkit sounding) across the Coastal Bend and within an area of strong 850-mb
moisture convergence. Rainfall rates dissipated across the far northern Coastal Bend as thunderstorms
were carried away from the strong dynamic lift and considerable elevated instability.
0600-1200 UTC (Midnight to 6 am CST)
During this period strong convective precipitation transitioned slowly to stratiform rainfall as instability decreased
with time and synoptic lift waned slightly. Initial rainfall rates up to 1 inch per hour occurred between 0600 and 0900
UTC but tapered to below one half inch toward 1200 UTC. Cloud-to-ground lightning was considerable between
0600 and 0800 UTC across the
Moderate surface winds produced frequent wind gusts to 35 mph across the near-shore waters and Coastal
Bend where a strong MSL pressure gradient had developed north of a surface low in deep South
vort lobe sheared apart in the divergent flow aloft with part of the energy moving into the Gulf of America and another
portion that rotated into south central
Bend. The axis of heavy rain (rates of half inch per hour) followed this convergence, but also increased across
the Brush Country and
shaped structure to the cold cloud tops (see satellite loops above).
850 mb moisture transport at 1200 UTC | Deep moisture convergence at 1200 UTC | Storm Total Precipitation at 1244 UTC |
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1200-1800 UTC (6 am to Noon CST)
Dry air and subsidence entered the southern Coastal Bend as a main vorticity center moved directly over this
region and consolidated with prior energy. This produced a dry slot as depicted in radar reflectivity loops which
slowly expanded northward into the northern Coastal Bend towards 1800 UTC. The axis of 850-mb convergence
pivoted and organized heavier rainfall persisted across the Brush Country and Interior Coastal Plain, and expanded
within moderate surface convergence from Baffin Bay to
over the northern Coastal Bend tapered off during this period but continued across the Brush Country. Rainfall
rates of around 1 inch per hour caused flooding near Kingsville. Rainfall persisted in the
tapered off in an area of lighter wrap-around precipitation.
HPC 1200 UTC 14 January total QPF | HPC day 1 QPF January 15 |
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1200 UTC 15 January analysis
SBCAPE and CIN | 925 mb height, temperature and wind | 700 mb height, temperature and wind |
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500 mb height, temperature, and wind | 300 mb wind and divergence | Surface moisture convergence |
KCRP 2-day storm total at 1244 UTC 15 January | 0600 UTC NCEP-ARW model reflectivity |
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1800-0000 UTC (Noon to 6 pm CST)
The axis of heavy rain over the Brush Country persisted, intensified and further expanded southward towards Kingsville
and Baffin Bay, while rainfall also continued over the Victoria Crossroads but mostly ended along the Coastal Bend
in the dry slot and subsidence over the northern Coastal Bend (see loop). Upper-level divergence also depicted
its axis inland and northward. The increased rainfall rates along a northwest to southeast oriented axis west of
I-37 were similar to NAM model run placement, and increased to a narrow region of one half to 1 inch per hour
(see radar loop). Rainfall rapidly dissipated at 0000 UTC 16 January as much drier and colder air filtered across
the region and the low to mid-level low shifted over the Gulf of America.
1900 UTC 15 January
850 and 250 mb cross-over wind | SBCAPE and CIN | Surface plot over South Texas |
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850 mb height, wind and temperature | 500 mb height, wind and temperature | 300 mb wind and divergence |
0000 UTC 16 January
NAM 0000 UTC 16 January 4-panel analysis |
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LSR (Local Storm Report)
PRELIMINARY LOCAL STORM REPORT...SUMMARY
NATIONAL WEATHER SERVICE CORPUS CHRISTI TX
315 PM CST FRI JAN 15 2010
..TIME... ...EVENT... ...CITY LOCATION... ...LAT.LON...
..DATE... ....MAG.... ..COUNTY LOCATION..ST.. ...SOURCE....
..REMARKS..
0249 PM FLOOD 4 ESE ORANGE GROVE 27.93N 97.88W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
FM 70 IS CLOSED AT FM 624 DUE TO FLOODING.
0245 PM FLOOD 8 SSW PORT LAVACA 28.50N 96.65W
01/15/2010 CALHOUN TX EMERGENCY MNGR
HWY 238 CLOSED DUE TO HIGH WATER OVER A BRIDGE CROSSING.
0215 PM FLOOD 5 SSW SKIDMORE 28.16N 97.72W
01/15/2010 BEE TX DEPT OF HIGHWAYS
FM 796 CLOSED AT CR533 DUE TO FLOODING.
0208 PM FLOOD 7 ESE MATHIS 28.06N 97.72W
01/15/2010 SAN PATRICIO TX DEPT OF HIGHWAYS
SH 188 CLOSED FROM IH 37 TO FM 796 DUE TO LOW WATER
CROSSINGS FLOODED.
1254 PM FLOOD 1 SE ROBSTOWN 27.79N 97.65W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
NORTH AND SOUTHBOUND FEEDER ROADS ON U.S. 77 CLOSED
BETWEEN CR44 AND TERRY SHEMISE BLVD DUE TO HIGH WATER.
1150 AM FLOOD BISHOP 27.58N 97.80W
01/15/2010 NUECES TX EMERGENCY MNGR
SEVERAL ROADS IN THE CITY WERE BEING CLOSED DUE TO HIGH
WATER.
1134 AM FLOOD 4 S ALICE 27.70N 98.06W
01/15/2010 JIM WELLS TX DEPT OF HIGHWAYS
WATER REPORTED OVER FM 1930 BETWEEN U.S. 281 AND FM 1352.
ROADWAY IS STILL PASSABLE.
1049 AM FLOOD 3 SSE WOODSBORO 28.19N 97.31W
01/15/2010 REFUGIO TX DEPT OF HIGHWAYS
FM 629 IS CLOSED FROM FM 3037 AND FM 136 DUE TO WATER
OVER THE ROAD.
1017 AM FLOOD 8 WNW SKIDMORE 28.29N 97.81W
01/15/2010 BEE TX DEPT OF HIGHWAYS
WATER OVER FM 1349 FROM US 59 TO FM 797.
1013 AM FLOOD 3 NW TYNAN 28.18N 97.77W
01/15/2010 BEE TX DEPT OF HIGHWAYS
WATER OVER ROAD ON FM 796 BETWEEN FM 888 AND SH 359.
0930 AM FLOOD 5 NNE ARANSAS PASS 27.97N 97.12W
01/15/2010 ARANSAS TX DEPT OF HIGHWAYS
WATER OVER FM 1069 AT VARIOUS LOCATIONS BETWEEN 1069 AND
SH 188.
0755 AM FLOOD 2 W CORPUS CHRISTI 27.77N 97.53W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OVER ROAD ON FM 2292 BETWEEN MCGLOIN ST. AND FM
665.
0753 AM FLOOD 5 NNW DRISCOLL 27.74N 97.79W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OF ROAD ON FM 2826 BETWEEN CR85 AND CR87.
0750 AM FLOOD 4 S CORPUS CHRISTI 27.71N 97.50W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OVER ROADWAY ON FM 763 BETWEEN FM 665 AND FM 0043.
1245 AM FLOOD 4 SE CORPUS CHRISTI 27.72N 97.46W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OVER SH 357 JUST WEST OF THE LA JOLLA CREEK BRIDGE.
1241 AM FLOOD PORT ARANSAS 27.83N 97.08W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER REPORTED OVER SH 361 AT VARIOUS LOCATIONS INSIDE
PORT ARANSAS CITY LIMITS.
1237 AM FLOOD 4 W ROBSTOWN 27.80N 97.72W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OVER ROAD ON SH 44 FROM BUSINESS 44 TO FM 1889.
1236 AM FLOOD ROCKPORT 28.04N 97.05W
01/15/2010 ARANSAS TX DEPT OF HIGHWAYS
WATER OVER FM 1781 NEAR FM 1069.
1235 AM FLOOD 5 NW CORPUS CHRISTI 27.83N 97.55W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
WATER OVER FM 2292 AND LEOPARD ST. INTERSECTION.
1226 AM FLOOD 2 NNE ARANSAS PASS 27.92N 97.14W
01/15/2010 ARANSAS TX DEPT OF HIGHWAYS
WATER OVER ROAD SOUTHBOUND LANE OF BUSINESS 35L NEAR
STAPP ST.
1210 AM FLOOD 1 N CHAPMAN RANCH 27.59N 97.45W
01/15/2010 NUECES TX DEPT OF HIGHWAYS
SH 286 CLOSED BETWEEN FM 2444 AND FM 70 DUE TO WATER OVER
THE ROAD...PARTICULARLY BETWEEN CR12 AND CR14. FM 70 FM
US 77 AND SH 286 IS ALSO CLOSED DUE TO THIS FLOODING
1209 AM FLOOD 1 S WOODSBORO 28.22N 97.32W
01/15/2010 REFUGIO TX DEPT OF HIGHWAYS
LOW WATER CROSSINGS ARE FLOODED WITH WATER OVER THE
ROADWAY ON FM 1360
Alex Tardy WFO Corpus Christi