788  
FXUS63 KEAX 171732  
AFDEAX  
 
AREA FORECAST DISCUSSION  
NATIONAL WEATHER SERVICE KANSAS CITY/PLEASANT HILL MO  
1232 PM CDT SAT MAY 17 2025  
   
..18Z AVIATION UPDATE  
 
   
KEY MESSAGES  
 
- QUIET WEATHER THROUGH SATURDAY LATE AFTERNOON  
 
- RAIN SHOWERS AND THUNDERSTORMS SUNDAY; CONDITIONAL SEVERE THREAT  
 
- SEVERE THUNDERSTORMS EXPECTED MONDAY, TUESDAY THREAT SHIFTED  
SOUTHEASTWARD  
 
- HEAVY RAINFALL LIKELY LEADS TO FLOODING ISSUES MONDAY AND TUESDAY  
 
 
   
DISCUSSION  
 
ISSUED AT 350 AM CDT SAT MAY 17 2025  
 
CLOSED-LOW SYSTEM IS STARTING TO MOVE INTO THE NORTHERN GREAT LAKES  
REGION. AN AREA OF MID-LEVEL TROUGHING OVER THE EASTERN PACIFIC AND  
ANOTHER AREA OF TROUGHING NEAR THE BAJA PENINSULA HAVE PROMPTED AN  
H5 HEIGHT RISE RESPONSE ACROSS THE CENTRAL CONUS THROUGH THE  
OVERNIGHT HOURS THAT WILL EVENTUALLY LEAD TO A RIDGE AXIS PASSING  
THROUGH THE AREA. SUBTLE DCVA STARTS IN THE FRONT RANGE INTO THE  
TEXAS PANHANDLE THIS AFTERNOON THAT WILL KICK OFF SURFACE  
CYCLOGENESIS BROADLY ACROSS THE HIGH PLAINS. THIS KEEPS LOW-LEVEL  
FLOW SOUTHERLY AND SOUTHWESTERLY FROM THE SOUTHERN PLAINS INTO THE  
LOWER MISSOURI RIVER VALLEY FOR SATURDAY, HELPING TO AMPLIFY THE H5  
HEIGHTS. THIS THERMAL RIDGE AXIS PASSES THROUGH, BRINING  
TEMPERATURES BACK INTO THE UPPER 70S AND LOWER 80S, EVEN AFTER THE  
PASSAGE OF THE COLD FRONT TRAILING THE CLOSED-LOW SYSTEM WELL NORTH  
OF THE AREA FROM LAST NIGHT. MAY SEE A FEW CLOUDS THIS AFTERNOON  
WITH SOME UPPER-LEVEL MOISTURE THAT MOVES THROUGH BUT MOST OF THIS  
SHOULD MOVE EAST, AND SUBSIDENCE WITH THE H5 HEIGHT RISES SHOULD  
LEAD TO MOSTLY SUNNY CONDITIONS ACROSS OUR FORECAST AREA, FOR THE  
EXCEPTION OF FAR NORTHERN MISSOURI WHICH MAY SEE LINGERING CLOUD  
COVER. BY LATE EVENING, THE TROUGH AXIS OVER PACIFIC ACCELERATES  
INLAND AND PHASES WITH THE WITH SOUTHERN TROUGH AXIS, STRENGTHENING  
DCVA AND SURFACE CYCLOGENESIS OVER THE FRONT RANGE. STRONGER THETA-E  
TRANSPORT OCCURS ACROSS THE SOUTHERN PLAINS INTO THE EASTERN PLAINS  
OF KANSAS, ALONG WITH THE WARM FRONT SURGING NORTHWARD. EXPECTING TO  
SEE ISENTROPIC UPGLIDE AS THIS MOVES NORTHWARD, AND WILL BE ENOUGH  
TO GENERATE RAIN SHOWERS AND PERHAPS ISOLATED THUNDERSTORM ACTIVITY  
INTO OUR SOUTHWESTERN FORECAST AREA, AND COULD CLIP PORTIONS OF THE  
KC METRO. H5 LEVEL WILL STILL LARGELY BE CHARACTERIZED BY A RIDGING  
REGIME WHICH COULD HINDER LIFT WITH THE SURGING WARM FRONT, BUT CAMS  
ARE SHOWING SOME HINTS OF A FEW LOCALIZED, THOUGH WEAK, VORT MAXIMA  
MOVING THROUGH. LLJ DEVELOPMENT COULD INCREASE SOME CONVERGENCE, BUT  
OVERALL FORCING AND KINEMATIC SUPPORT IS NOT IMPRESSIVE, THEREFORE  
NOT EXPECTING ACTIVITY LATE TONIGHT AND VERY EARLY SUNDAY MORNING TO  
POSE A SEVERE RISK. THAT RISK WILL LIKELY REMAIN ALONG AND SOUTH OF  
THE U.S. HWY. 400 CORRIDOR.  
 
SUNDAY LATE MORNING THROUGH AFTERNOON, DEEP H5 TROUGH AXIS AND  
ASSOCIATED JET STREAK HEADS TOWARD THE HIGH PLAINS THAT WILL BEGIN  
TO LIFT THE TROUGH, ACQUIRING A NEGATIVE TILT AS SUNDAY AFTERNOON  
PROGRESSES. THE DCVA ACROSS THE HIGH PLAINS DRASTICALLY STRENGTHENS  
AT THIS TIME, AND EXPECTING A MATURING CYCLONE TO BEGIN MOVING  
EASTWARD. STRONG WAA ALONG WITH FAVORABLE MOISTURE TRANSPORT OCCURS  
FROM EAST-CENTRAL KANSAS TO THE MIDDLE MISSISSIPPI RIVER VALLEY,  
WITH WARM FRONT SURGING TOWARD THE IOWA-MISSOURI STATE LINE AND  
PUSHING PRIMARY H5 RIDGE AXIS COMPLETELY ACROSS THE AREA.  
DETERMINISTIC GUIDANCE SOLUTIONS STILL DEMONSTRATE SOME DISCREPANCY  
WITH HOW FAR NORTH THIS BOUNDARY EVENTUALLY TRAVELS, CONTINUING SOME  
UNCERTAINTY WITH HOW THE MESOSCALE ENVIRONMENT EXACTLY EVOLVES.  
STRONG MIXING OVER THE HIGH PLAINS OF KANSAS WILL ALLOW A DRY LINE  
TO PROPAGATE FROM WESTERN KANSAS INTO CENTRAL KANSAS THROUGH THE  
AFTERNOON, AND CAMS CONTINUE TO FAVOR STRONG CONVERGENCE ALONG THIS  
FEATURE AS IT PUSHES UP AGAINST A HIGH THETA-E AIRMASS EAST OF  
INTERSTATE 135/U.S. HWY. 81. ACROSS CENTRAL AND SOUTHEASTERN KANSAS,  
SURFACE TROUGHING EXTENDS EASTWARD AND MID-LEVEL VORT MAXIMA EJECT  
FROM THE PRIMARY TROUGH, WHICH BEGINS TO STALL OVER THE HIGH PLAINS  
OF NEBRASKA AS IT ATTEMPTS TO CLOSE-OFF. CONVECTION INITIATION FROM  
CENTRAL KANSAS TO EAST-CENTRAL KANSAS IS DEPICTED BETWEEN 18Z-21Z IN  
THE HRRR ALONG WITH A FEW OTHER CAMS. HOWEVER, THE EASTWARD MIXING  
OF THE DRYLINE IS STILL NOT CONSISTENT AMONGST ALL AVAILABLE  
GUIDANCE, AND THE SURGING OF THE WARM FRONT IS ALSO PLAYING A FACTOR  
IN WHERE THE FAVORABLE FORCING/CONVERGENCE ALONG A DRY LINE  
ENCOUNTERS A FAVORABLE SEGMENT OF THE AMBIENT WARM-SECTOR. ONCE  
CONVECTION DOES GET GOING IN EASTERN KANSAS, 0-6KM BULK SHEAR VALUES  
OF 30 KTS SHOULD ALLOW UPDRAFTS TO ORGANIZE EFFICIENTLY, ORIENTED  
PERPENDICULAR TO THE DRYLINE FEATURE. THIS CAN FAVOR A DISCRETE  
STORM MODE IN EASTERN KANSAS, WITH THE SHEAR ENVIRONMENT SUPPORTING  
SUPERCELL DEVELOPMENT. IF CONVECTION TAKES LONGER TO INITIATE AND IS  
CLOSER TO THE ONSET OF THE LLJ, DISCRETE STORM MODE MAY NOT LAST  
LONG, AND CONGEAL MORE INTO AN MCS LIKE FEATURE. THIS EVENTUALLY  
WILL START TO MOVE TOWARD WESTERN MISSOURI INTO OUR FORECAST AREA.  
OUR COUNTIES SHOULD HAVE PLENTY OF MOISTURE BY THIS TIME, WITH  
DEWPOINTS PUSHING INTO THE 60S, AND EXPECTING MUCAPE VALUES TO START  
TO PUSH ABOVE 3000 J/KG. HOWEVER, AREAS ALONG THE KANSAS-MISSOURI  
STATELINE STILL APPEARED CAPPED, WITH MOST AREAS AROUND -100 J/KG  
CIN WITHIN THE AREA OF FAVORABLE FORCING. WHILE EASTERN KANSAS MAY  
SEE QUITE A BIT OF ACTIVITY, WHERE THE ENHANCED RISK IS IN THE  
SWODY2 OUTLOOK, INITIATION MAY NOT BE POSSIBLE IN MISSOURI. CURRENT  
THINKING IS THAT ANY ACTIVITY THAT MAKES IT TO CENTRAL MISSOURI MAY  
COME IN THE FORM OF AN ORGANIZED MCS OF SOME KIND THAT INITIATES IN  
KANSAS AND IS THEN ABLE TO SUSTAIN ITSELF AS IT ENCOUNTERS A CAPPED  
ENVIRONMENT THROUGH MISSOURI. THE WILD CARD FOR FORCING WILL BE IF  
THE DRYLINE FEATURE CAN CONTINUE TO MIX EASTWARD AND PROVIDE ENOUGH  
CONVERGENCE TO BREAK THROUGH THE CAP IN WESTERN MISSOURI. THEREFORE,  
THINKING DAMAGING WIND GUSTS AND HAIL WOULD BE THE PRIMARY THREAT IF  
A STRONGER MCS IS ABLE TO MATERIALIZE. LOW-LEVEL SHEAR ENVIRONMENT  
COULD SUPPORT A TORNADO, BUT THE ONLY WAY FOR THIS TO HAPPEN IS IF  
THE CURRENTLY EXPECTED CAP ERODES AND OUR AREA IS ABLE TO ACHIEVE CI  
OF DISCRETE STORMS. THEREFORE, THIS MAKES ANY PROBABILITIES FOR  
TORNADIC ACTIVITY ON SUNDAY EXTREMELY CONDITIONAL FROM THE STATE KS-  
MO STATELINE AND EASTWARD. FINE MESOSCALE DETAILS WILL LARGELY  
DETERMINE THE EASTWARD EXTENT OF SEVERE CONVECTION FOR SUNDAY  
EVENING AND VERY EARLY MONDAY MORNING.  
 
MONDAY, HIGHER CONFIDENCE IN THE OCCURRENCE OF SEVERE THUNDERSTORMS  
ACROSS MUCH OF THE AREA, BUT STILL UNCERTAINTY WITH RESPECT THE  
PRIMARY HAZARD AND DOMINANT STORM MODE FOR THE DAY. ALTHOUGH H5  
TROUGH TRANSITIONS INTO A CLOSED-LOW SYSTEM, MOST OF THE FLOW ACROSS  
THE AREA REMAINS SOUTHWESTERLY, CONTINUING THETA-E TRANSPORT INTO  
THE ENTIRE LOWER MISSOURI RIVER VALLEY. STILL UNCERTAIN AS TO WHERE  
THE WARM-FRONT SURGES TO, AND WHERE IT MAY EVENTUALLY STALL. SURFACE  
CYCLONE WILL BE MAKING PROGRESS ACROSS KANSAS DURING THIS TIME, A  
CORRIDOR OF SURFACE PRESSURE FALLS AND TROUGHING EXTENDING EASTWARD  
AS FAR AS EASTERN MISSOURI AND WESTERN ILLINOIS. MULTIPLE MID-LEVEL  
VORT MAXIMA SHOULD EJECT FROM THE MAIN TROUGH OVER THE PLAINS,  
PROVIDING BROADSCALE LIFT OVER THE WARM SECTOR, WHILE NOSE OF H5 JET  
STREAK WORKS TOWARD MISSOURI, AND AT SOME POINT DURING THE DAY MOST  
OF THE AREA EXPERIENCES THE LEFT-EXIT REGION OF THE JET STREAK.  
SBCAPE VALUES ARE PROGGED TO CLIMB ABOVE 3000 J/KG, WITH DEWPOINTS  
CLIMBING INTO THE UPPER 60S AND PERHAPS EVEN LOWER 70S. ADDITIONAL  
CONVERGENCE SHOULD OCCUR AS COLD FRONT MOVES ACROSS KANSAS TRAILING  
THE SURFACE CYCLONE. THERE WILL BE TWO AREAS OF INTEREST WITH THIS  
SYSTEM. THE FIRST WILL BE THE WARM FRONT, WHICH LIKELY COINCIDES  
WITH AREA OF SURFACE PRESSURE FALLS THROUGH THE AFTERNOON HOURS OF  
MONDAY. WITH PASSING MID-LEVEL VORT MAXIMA AND INCREASING DEEP LAYER  
SHEAR, DISCRETE CELL DEVELOPMENT IF ACHIEVED WILL HAVE A FAVORABLE  
SHEAR ENVIRONMENT FOR THE DEVELOPMENT OF SUPERCELLS. DIRECTLY ALONG  
THE WARM FRONT, BACKING SURFACE WINDS SHOULD CYCLONICALLY CURVE LOW-  
LEVEL HODOGRAPHS SUFFICIENTLY TO HELP DEVELOP LOW-LEVEL MESOS, AND  
APPROACHING H5 JET STREAK SHOULD LENGTHEN MID AND UPPER-LEVEL  
PORTIONS OF THE HODOGRAPH, ALLOWING DISCRETE STORMS TO EASILY  
ORGANIZE. IN THIS ENVIRONMENT, ALL MODES OF HAZARDS ARE POSSIBLE.  
DEPENDING ON HOW EXPANSIVE THE WARM-SECTOR BECOMES, THERE MAY BE  
ENOUGH LIFT FOR STRONGER STORMS TO DEVELOP SOUTH OF ACTUAL WARM  
FRONT THAT COULD ALSO PRODUCE MULTIPLE HAZARDS WITH EXTENSIVE  
TRACKS ACROSS THE WARM SECTOR. FAILURE MODE FOR THIS SCENARIO WOULD  
BE IF THE TIMING OF BOUNDARY LAYER DESTABILIZATION AND MID-LEVEL  
LIFT DO NOT LINE UP. NEXT OPPORTUNITY, WILL BE ALONG THE COLD FRONT.  
THERE MAY BE A SHORT-WINDOW WHERE THE DEEP LAYER SHEAR VECTOR IS  
PERPENDICULAR TO THE COLD FRONT, ALLOWING FOR ADDITIONAL DISCRETE  
DEVELOPMENT. DEPENDING ON WHERE AGAINST THE WARM SECTOR THIS WOULD  
OCCUR WILL DETERMINE WHAT THE LOW-LEVEL WIND SHEAR PROFILE LOOKS  
LIKE, AND THEREFORE ALSO CONTROLS TORNADO THREAT WITH THIS. IF COLD  
FRONT INITIATED STORMS INGEST MORE CROSS-WISE VORTICITY, THIS MAY  
END UP BEING MORE OF HAIL AND WIND THREAT. EVENTUALLY, MONDAY  
EVENING LOW-LEVEL JET DEVELOPS, AND IF THERE ARE ANY DISCRETE  
STORMS, LIKELY CONGEAL INTO AN MCS. DEEP LAYER SHEAR VECTORS BECOME  
MORE PARALLEL TO THE COLD FRONT LATE MONDAY, FURTHER SUPPORTING  
UPSCALE GROWTH. THE 00Z CAMS THAT RUN TONIGHT MAY GIVE US BETTER  
INSIGHT INTO POTENTIAL STORM MODE EVOLUTION AS THEIR OUTPUT WILL  
START TO COVER MOST OF THE ACTIVITY FOR MONDAY. PERHAPS BY THIS TIME  
TOO, THERE WILL BE BETTER CONSENSUS ON THE WARM FRONT POSITION.  
HYDRO WILL ALSO BE A PROBLEM STARTING MONDAY, WITH PWATS STILL ABOVE  
1.5 INCHES ACROSS MOST OF THE FORECAST AREA. A STALLED BOUNDARY  
COULD RESULT IN TRAINING STORM POTENTIAL, ESPECIALLY IF MULTIPLE  
SHORT-WAVE PERTURBATIONS MOVE ACROSS THE WARM-SECTOR. RAINFALL RATES  
OF 1 TO 2 INCHES PER HOUR MAY BECOME POSSIBLE, RESULTING IN FLASH  
FLOODING AND RIVER FLOODING AS WELL. WHAT AREAS THIS IMPACTS WILL  
ALSO BE DETERMINED BY WHERE THE WARM FRONT EVENTUALLY POSITIONS.  
 
TUESDAY, COLD FRONT SHOULD START TO PUSH THROUGH THE AREA, THOUGH  
THERE IS STILL SOME UNCERTAINTY WHICH HOW THE H5 CLOSED-LOW  
BEHAVES. WE STILL HAVE QUITE A BIT OF LARGE SCALE ASCENT, ALONG WITH  
CONVERGENCE WITH BOTH COLD FRONT AND SURFACE CYCLONE. WHAT LINGERS  
FROM MONDAY WILL CONTROL HOW MUCH INSTABILITY IS LEFT-OVER, AND HOW  
QUICKLY THE ENVIRONMENT RECOVERS BY TUESDAY MORNING AND AFTERNOON.  
BIGGEST QUESTION, HOW FAR WEST IS THERE A THREAT FOR STRONG TO  
SEVERE STORMS ON TUESDAY. SOME ENSEMBLE MEMBERS KEEP PROBABILITIES  
WEST OF THE KANSAS CITY METRO, WHILE OTHERS PUSH STUFF EAST OF HWY.  
65. AT THIS TIME, WILL NOT DIVE MUCH INTO POTENTIAL MESOSCALE  
OUTCOMES WITH TUESDAY, BUT BE PREPARED FOR ANOTHER ROUND OF SEVERE  
STORMS, OR FOR MONDAY ACTIVITY TO CONTINUE MUCH OF TUESDAY MORNING.  
ADDITIONAL RAINFALL WILL FURTHER AUGMENT FLOODING CONCERNS. BEYOND  
TUESDAY, COLD FRONT CLEARS THE AREA, BUT ADDITIONAL AREA OF WEAK  
FORCING THROUGH THE END OF NEXT WEEK MAY BRING ADDITIONAL  
PRECIPITATION CHANCES.  
 
 
   
AVIATION /18Z TAFS THROUGH 18Z SUNDAY/  
 
ISSUED AT 1229 PM CDT SAT MAY 17 2025  
 
VFR CONDITIONS EXPECTED TO CONTINUE ACROSS THE SITES WITH THIS  
ISSUANCE. A COUPLE OF ITEMS OF NOTE THOUGH. A FEW W/NW WIND  
GUSTS TO AROUND 20 KTS WILL CONTINUE FOR THE FIRST COUPLE/FEW  
HOURS OF THE PERIOD, EASING AND SHIFTING CLOCKWISE OUT OF THE  
NORTH AND THEN EAST. OVERNIGHT, A FEW SHOWERS MAY CLIP THE METRO  
SITES KIXD/KMKC/KCI, BUT CONFIDENCE IS LIMITED SO OPTED FOR  
PROB30. BEST CHANCES FROM SOUTH TO NORTH. LATE IN THE PERIOD,  
WINDS SHIFT FURTHER, TOWARD THE SE AND GUSTS TO AROUND 20KTS  
AGAIN POSSIBLE.  
 
 
   
EAX WATCHES/WARNINGS/ADVISORIES  
 
MO...NONE.  
KS...NONE.  
 
 
 
 
 
DISCUSSION...KRULL  
AVIATION...CURTIS  
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