173  
FXUS02 KWBC 240727  
PMDEPD  
 
EXTENDED FORECAST DISCUSSION  
NWS WEATHER PREDICTION CENTER COLLEGE PARK MD  
327 AM EDT THU OCT 24 2024  
 
VALID 12Z SUN OCT 27 2024 - 12Z THU OCT 31 2024  
   
..GENERAL OVERVIEW
 
 
A DIGGING TROUGH IN THE WEST WILL PRODUCE RAIN, HIGH ELEVATION  
SNOW, HIGH WINDS AND COOLER TEMPERATURES ACROSS MUCH OF THAT REGION  
NEXT WEEK. THIS TROUGH MAY GO ON TO GENERATE ADDITIONAL HEAVY  
RAINFALL, THUNDERSTORMS AND HIGH WINDS OVER PARTS OF THE GREAT  
PLAINS AND MISSISSIPPI VALLEY MID-TO-LATE NEXT WEEK AS WELL. A  
DOWNSTREAM RIDGE, CENTERED OVER THE BAJA PENINSULA, WILL SUPPORT  
ABOVE AVERAGE TEMPERATURES FROM THE PLAINS TO EVENTUALLY THE EAST  
COAST.  
 
   
..GUIDANCE/PREDICTABILITY ASSESSMENT
 
 
MODELS WERE FAIRLY WELL CLUSTERED AROUND THE OVERALL SYNOPTIC  
EVOLUTION ACROSS THE LOWER 48 NEXT WEEK. THERE'S SOME UNCERTAINTY  
AROUND WHETHER THE UPPER PATTERN WILL SPLIT WITH A SOUTHERN STREAM  
TROUGH PROPAGATING THROUGH FOUR CORNERS AND INTO THE PLAINS, WHILE  
A NORTHERN STREAM TROUGH GLIDES ACROSS SOUTHERN CANADA. THE  
DETERMINISTIC 12Z CANADIAN BECOMES A NOTABLE OUTLIER DUE TO ITS  
ATTEMPT TO CREATE AN ANOMALOUS CLOSED LOW OVER THE FRONT RANGE  
NEXT WEDNESDAY. THUS, IT WASN'T INCLUDED IN THE BLEND BEYOND DAY 5.  
IT'S WORTH NOTING THAT THE AIFS, FUXI AND PANGU ML MODELS ALSO  
SIGNAL A SPLIT FLOW PATTERN OVER THE WEST BEGINNING ON TUESDAY.  
 
A COMBINATION OF THE DETERMINISTIC 12Z ECMWF/CMC/UKMET AND 18Z GFS  
WERE UTILIZED IN THE DAYS 3 AND 4 BLENDS WITH THE EC AND GFS  
FAVORED. BY DAY 5 THE CANADIAN AND UK ARE REMOVED AND THE 12Z  
ECE/CMCE AND 18Z GEFS ARE INTRODUCED TO THE BLEND TO MITIGATE SOME  
OF THE MOST ANOMALOUS SPLIT FLOW SIGNALS SEEN IN SOME OF THE  
DETERMINISTIC GUIDANCE. A MORE ENSEMBLE MEAN WEIGHTED BLEND IS  
CONTINUED THROUGH DAY 7 DUE TO RELATIVELY GOOD RUN-TO-RUN  
CONSISTENCY AND NOT MUCH MODEL SPREAD AROUND THE MID-LEVEL TROUGH  
OVER THE CENTRAL CONUS..  
 
   
..WEATHER/HAZARDS HIGHLIGHTS
 
 
 
A LOW PRESSURE SYSTEM WILL ARRIVE OVER THE PACIFIC NORTHWEST ON  
SATURDAY, BRINGING WITH IT RAIN, HIGH ELEVATION SNOW TO THE REGION  
THROUGH SUNDAY. HIGH WINDS WILL IMPACT THE LEE OF THE NORTHERN  
ROCKIES THIS WEEKEND AS WELL. RAIN, SNOW AND HIGH WINDS EXPAND INTO  
THE ROCKIES ON MONDAY AND TUESDAY.  
 
CYCLOGENESIS OVER THE LEE OF THE ROCKIES WILL SUPPORT HIGH WIND  
CONCERNS ACROSS PORTIONS OF THE GREAT PLAINS AND MISSISSIPPI  
VALLEY EARLY NEXT WEEK. DEPENDING ON HOW DEEP THE UPPER TROUGH GETS  
OVER THE PLAINS NEXT WEEK, THERE COULD BE SOME POTENTIAL FOR GULF  
OF MEXICO MOISTURE TO INTERACT WITH AN ATTENDANT COLD FRONT OVER  
THE PLAINS/MISSISSIPPI VALLEY POSSIBLY GENERATING HEAVY RAINFALL  
AND THUNDERSTORMS.  
 
THE DIGGING TROUGH IN THE WEST WILL BE MIRRORED BY A STAUNCH  
DOWNSTREAM RIDGE OVER THE SOUTHERN AND CENTRAL U.S. NEXT WEEK. THIS  
RIDGE WILL SUPPORT TEMPERATURES BETWEEN 20-30 DEGREES ABOVE AVERAGE  
ACROSS THE PLAINS ON MONDAY BEFORE SPREADING INTO THE MISSISSIPPI  
VALLEY AND EAST ON TUESDAY, WEDNESDAY AND THURSDAY. THERE'S ALSO A  
POTENTIAL FOR WIDESPREAD HIGH TEMPERATURE RECORDS TO BE TIED OR  
BROKEN ACROSS FROM ARIZONA TO TEXAS ON SUNDAY FOLLOWED BY  
AN EXPANSION INTO THE PLAINS AND UPPER MIDWEST ON MONDAY.  
 
KEBEDE  
 
ADDITIONAL 3-7 DAY HAZARD INFORMATION CAN BE FOUND ON THE WPC MEDIUM  
RANGE HAZARDS OUTLOOK CHART AT:  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/THREATS/THREATS.PHP  
 
WPC MEDIUM RANGE 500MB HEIGHTS, SURFACE SYSTEMS, WEATHER GRIDS,  
QUANTITATIVE PRECIPITATION FORECAST (QPF), EXCESSIVE RAINFALL  
OUTLOOK (ERO), WINTER WEATHER OUTLOOK (WWO) PROBABILITIES, HEAT  
INDICES, AND KEY MESSAGES CAN BE ACCESSED FROM:  
 
HTTPS://WWW.WPC.NCEP.NOAA.GOV/MEDR/5DAYFCST500_WBG.GIF  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/MEDR/5DAYFCST_WBG_CONUS.GIF  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/5KM_GRIDS/5KM_GRIDSBODY.HTML  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/QPF/DAY4-7.SHTML  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/#PAGE=ERO  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/WWD/PWPF_D47/PWPF_MEDR.PHP?DAY=4  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/HEAT_INDEX.SHTML  
HTTPS://WWW.WPC.NCEP.NOAA.GOV/#PAGE=OVW  
 

 
 
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