821  
AWUS01 KWNH 090913  
FFGMPD  
MSZ000-LAZ000-ARZ000-091501-  
 
MESOSCALE PRECIPITATION DISCUSSION 0007  
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD  
412 AM EST FRI JAN 09 2026  
 
AREAS AFFECTED...CENTRAL MISSISSIPPI...EASTERN AND NORTHEASTERN  
LOUISIANA...  
 
CONCERNING...HEAVY RAINFALL...FLASH FLOODING POSSIBLE  
 
VALID 090911Z - 091501Z  
 
SUMMARY...FLATTENING STEERING FLOW TO SUPPORT SEGMENTED TRAINING  
CORRIDORS ACROSS THE LOWER MISSISSIPPI RIVER VALLEY.  
STRENGTHENING CONVERGENCE AND MODESTLY UNSTABLE AND SEASONABLY  
MOIST AIR SHOULD SUPPORT RAIN RATES TO 1.75" AND LOCALIZED STREAKS  
OF 2-4" IN 1-3HRS. SUGGESTING LOCALIZED FLASH FLOODING IS  
POSSIBLE THIS MORNING TO START A LONGER DAY OF REPEAT  
THUNDERSTORMS.  
 
DISCUSSION...GOES-E WV SUITE SHOWS MATURE/DECAYING SHORTWAVE  
RAPIDLY ELONGATING AND SLIDING NORTHEAST THROUGH THE CENTRAL GREAT  
LAKES WITH A WELL DEFINED BROADLY ANTICYCLONICALLY CURVED  
SUBTROPICAL JET STREAK ACROSS TEXAS THROUGH KY/TN WITH A STRONGER  
BASE OF THE NORTHERN STREAM SYNOPTIC TROUGH WELL UPSTREAM EMERGING  
INTO THE SOUTHERN HIGH PLAINS. THE STRONG FLOW AND UPPER-LEVEL  
DYNAMIC SUPPORT HAS RESULTED IN WELL ABOVE NORMAL MOISTURE FLUX  
ACROSS THE MISSISSIPPI RIVER VALLEY INTO THE GREAT LAKES; CIRA LPW  
DENOTES CORE OF HIGHER MOISTURE/THETA-E AIR OVER THE WEST GULF IS  
ADVANCING INTO THE ENTRANCE OF THE EASTERN US ATMOSPHERIC RIVER  
STREAM. SURFACE TO 850MB VALUES ARE NEARING 1" AND IS NOTED WITH  
SURFACE TDS IN THE UPPER 60S TO EVEN SPOTS OF 70 ACROSS THE LOWER  
MS VALLEY.  
 
THE OVERALL ORIENTATION OF THE UPPER-LEVEL FLOW IS SUPPORTING A  
PRE-FRONTAL CONFLUENCE ZONE ACROSS E LA AT THIS TIME, PROVIDING  
SUFFICIENT DEEP LAYER CONVERGENCE TO TAP THE WEAKLY UNSTABLE AIR.  
MLCAPES ARE ANALYZED FROM 500-1000 J/KG THROUGH THE SABINE RIVER  
VALLEY INTO THE DELTA REGION OF SE AR AND W MS. FLUX CONVERGENCE  
OF 30-35KTS AT ABOUT 30 DEGREES OF CONVERGENCE OVERLAPS WITH THE  
CORE OF THE MOISTURE AXIS WITH TPW NEAR 1.7". AS SUCH, RADAR  
DENOTES A FEW CLUSTERS OF THUNDERSTORMS DEVELOPING ACROSS NE LA AS  
WELL AS FURTHER NORTH ACROSS NE LA INTO W MS, THE LATTER DEEPER  
INTO THE MORE IDEAL UNIDIRECTIONAL FLOW AND MAY SUPPORT SOME  
TRAINING ELEMENTS AS THE OVERALL CONVECTIVE DEVELOPMENT EXPANDS  
AND INTENSIFIES OVER THE NEXT FEW HOURS. THE STRONG MOISTURE FLUX  
CONVERGENCE MAINLY BELOW 700MB WILL SUPPORT RATES OF 1.75"; AND  
WHILE THE FORWARD SPEEDS WILL LIMIT ANY SPECIFIC CORE, THE  
UPSTREAM DIVERGENCE ALOFT AND STRENGTH OF LOW LEVEL FLOW  
CONVERGENCE WILL SUPPORT BACK-BUILDING AND REDEVELOPMENT UPSTREAM  
THROUGH CENTRAL LA THROUGHOUT THE MORNING.  
 
LOCALIZED STORM OUTFLOWS MAY BE THE KEY TO ESTABLISHING THE MOST  
IDEAL TRAINING PROFILES, BUT EVEN 1-2 HOURS OF THESE RATES COULD  
SUPPORT 2-3" TOTALS AND LOCALLY HIGHER VALUES TO 4" WOULD THEN  
BEGIN TO EXCEED THE HIGH (3"/3HRS) FFG VALUES IN THE AREA.  
00Z/06Z HREF PROBABILITY OF 3"/3HRS PEAK AROUND 30% IN SW TO  
CENTRAL MS. STILL EVEN WITH DORMANT GROUND CONDITIONS, THESE  
RATES/TOTALS WILL HAVE THE GREATEST POTENTIAL FOR FLASH  
FLOODING/RAPID INUNDATION CONDITIONS WHERE INTERSECTING URBAN  
CENTERS. IN ANY CASE, THESE CELLS WILL SATURATE THE UPPER SOIL  
PROFILES PRIOR TO FURTHER CONVECTIVE ACTIVITY EXPECTED THROUGHOUT  
THE DAY AND EVENING. AS SUCH, FLASH FLOODING IS ONLY CONSIDERED  
POSSIBLE AND LIMITED TO WIDELY SCATTERED IN COVERAGE THROUGH THE  
EARLY MORNING PERIOD.  
 
GALLINA  
   
..PLEASE SEE WWW.WPC.NCEP.NOAA.GOV FOR GRAPHIC PRODUCT
 
 
ATTN...WFO...JAN...LCH...LIX...MEG...SHV...  
 
ATTN...RFC...ALR...ORN...NWC...  
 
LAT...LON 34138908 34058839 33498829 32868864 32288915  
31568980 30709050 30919161 30929254 31469279  
32169248 33289103 33719020  
 
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