877  
ACUS02 KWNS 161728  
SWODY2  
SPC AC 161726  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1126 AM CST SAT NOV 16 2024  
 
VALID 171200Z - 181200Z  
 
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS OF  
WESTERN INTO CENTRAL TEXAS...  
   
..SUMMARY  
 
STRONG TO SEVERE THUNDERSTORMS ARE EXPECTED TO DEVELOP ACROSS PARTS  
OF WESTERN, CENTRAL AND NORTHWEST TEXAS FROM SUNDAY EVENING THROUGH  
DAYBREAK ON MONDAY, POSING A RISK FOR SEVERE GUSTS AND POSSIBLY A  
FEW TORNADOES.  
   
..SYNOPSIS  
 
A NEGATIVELY TILTED MID-LEVEL TROUGH WILL EJECT INTO THE SOUTHERN  
PLAINS TOMORROW (SUNDAY) INTO TOMORROW NIGHT AS A SECOND MID-LEVEL  
TROUGH IMPINGES ON THE INTERIOR WEST. BY TOMORROW NIGHT INTO EARLY  
MONDAY MORNING, SURFACE LOW DEVELOPMENT IS EXPECTED ACROSS WESTERN  
TX AS STRONG UPPER SUPPORT AND AN 80 KT MID-LEVEL SPEED MAX  
OVERSPREAD THE SOUTHERN PLAINS. LOW-LEVEL WARM-AIR ADVECTION  
ACCOMPANYING THE DEVELOPING SURFACE LOW WILL SUPPORT MODEST  
BOUNDARY-LAYER DESTABILIZATION ACROSS CENTRAL TX INTO SOUTHERN OK,  
WHERE ADEQUATE LIFT AND SHEAR WILL SUPPORT SOME POTENTIAL FOR SEVERE  
THUNDERSTORMS.  
   
..SOUTHERN PLAINS - SUNDAY NIGHT INTO EARLY MONDAY MORNING  
 
BY AROUND 06Z MONDAY MORNING, A SURFACE LOW SHOULD BEGIN TO  
MATERIALIZE JUST SOUTH OF THE TX PANHANDLE WITH THE EJECTION OF THE  
AFOREMENTIONED MID-LEVEL TROUGH. DESPITE POOR LOW AND MID-LEVEL  
LAPSE RATES, MODEST SURFACE-850 MB THETA-E ADVECTION WILL SUPPORT A  
CORRIDOR OF 500-750 J/KG SBCAPE ACROSS CENTRAL TX INTO EXTREME  
SOUTHERN OK DURING THE 06-12Z TIME FRAME. GIVEN STRONG FORCING FOR  
ASCENT AND SOUTH-SOUTHWESTERLY 500 MB FLOW ORIENTED ROUGHLY PARALLEL  
WITH AN APPROACHING COLD FRONT, A SQUALL LINE IS EXPECTED TO DEVELOP  
AND ADVANCE NORTHEAST IN TANDEM WITH THE SURFACE LOW. MODEST VEERING  
BUT RAPID STRENGTHENING WITH HEIGHT OF THE VERTICAL WIND PROFILE  
WILL SUPPORT LARGE, CURVED HODOGRAPHS AHEAD OF THE SQUALL LINE.  
0-500 M SRH MAY EXCEED 200 M2/S2, WITH 0-3 KM SRH REACHING 400 M2/S2  
IN SPOTS. HOWEVER, QUESTIONS REMAIN REGARDING HOW MUCH SRH CAN BE  
EFFECTIVELY INGESTED INTO THUNDERSTORM UPDRAFTS GIVEN SCANT BUOYANCY  
PROFILES. STILL, EFFECTIVE DOWNWARD MOMENTUM TRANSPORT OF THE STRONG  
SYNOPTIC FLOW ALOFT MAY SUPPORT SEVERE GUSTS WITHIN THE SQUALL LINE.  
FURTHERMORE, IF STRONG ENOUGH LOW-LEVEL WAA CAN APPRECIABLY  
DESTABILIZE THE NOCTURNAL BOUNDARY-LAYER, THEN ISOLATED QLCS  
TORNADOES MAY ALSO OCCUR. ANY QLCS TORNADOES THAT CAN DEVELOP WILL  
MOST LIKELY OCCUR WITH ANY LEWPS OR MESOVORTICES WITHIN PORTIONS OF  
THE SQUALL LINE PRECEDING THE SURFACE LOW TRACK, WHERE LOW-LEVEL  
WINDS WILL BE MOST BACKED AND LOW-LEVEL SHEAR WILL BE STRONGEST.  
 
..SQUITIERI.. 11/16/2024  
 
 
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