481  
FXUS07 KWBC 201331  
PMD30D  
PROGNOSTIC DISCUSSION FOR MONTHLY OUTLOOK  
NWS CLIMATE PREDICTION CENTER COLLEGE PARK MD  
830 AM EST THU NOV 20 2025  
 
30-DAY OUTLOOK DISCUSSION FOR DEC 2025  
 
THE DECEMBER 2025 MONTHLY OUTLOOK WAS MADE WITH ONGOING LA NIñA CONDITIONS  
EXPECTED TO CONTINUE INTO WINTER. THE MOST RECENT WEEKLY NIñO 3.4 SEA SURFACE  
TEMPERATURE (SST) ANOMALY IS ABOUT -0.7 DEGREES CELSIUS. SST ANOMALIES IN THE  
CENTRAL AND EAST-CENTRAL EQUATORIAL PACIFIC OCEAN REMAIN NEGATIVE. OUTGOING  
LONGWAVE RADIATION (OLR) ANOMALIES WERE NEGATIVE OVER THE FAR WESTERN PACIFIC  
OCEAN, ASSOCIATED WITH ENHANCED CONVECTION AND PRECIPITATION OVER PARTS OF THE  
MARITIME CONTINENT. POSITIVE OLR ANOMALIES, INDICATING SUPPRESSED CONVECTION  
AND PRECIPITATION, WERE PRESENT NEAR THE INTERNATIONAL DATE LINE, CONSISTENT  
WITH LA NIñA CONDITIONS. LOW-LEVEL (850-HPA) EASTERLY TRADE WINDS WERE ENHANCED  
OVER THE WESTERN AND EAST-CENTRAL EQUATORIAL PACIFIC, ALSO CONSISTENT WITH LA  
NIñA CONDITIONS. UPPER-LEVEL (200-HPA) WIND ANOMALIES WERE WESTERLY OVER MOST  
OF THE EQUATORIAL PACIFIC OCEAN IN RECENT WEEKS. NEGATIVE SUBSURFACE OCEAN  
TEMPERATURE ANOMALIES PERSISTED NEAR THE SURFACE IN THE CENTRAL AND EASTERN  
EQUATORIAL PACIFIC OCEAN, INCREASING THE LIKELIHOOD OF PERSISTENT LA NIñA  
CONDITIONS. DYNAMICAL MODEL FORECASTS AND THE CPC EL NIñO SOUTHERN OSCILLATION  
(ENSO) OUTLOOK PREDICT LA NIñA CONDITIONS ARE MOST LIKELY TO PERSIST FOR THE  
DECEMBER-JANUARY-FEBRUARY WINTER SEASON WITH A PROBABILITY SLIGHTLY GREATER  
THAN 50 PERCENT. HOWEVER, LA NIñA CONDITIONS ARE MOST LIKELY TO END IN THE  
JANUARY-FEBRUARY-MARCH SEASON WITH A PROBABILITY GREATER THAN 60 PERCENT.  
ALTHOUGH THIS LA NIñA IS LIKELY TO REMAIN WEAK AND BE OF SHORT DURATION,  
PREDICTABILITY OF THE DECEMBER CLIMATE OUTLOOK IS LARGELY DUE TO CURRENT LA  
NIñA CONDITIONS.  
 
RECENTLY, THE UPPER-LEVEL POLAR VORTEX HAS BECOME DISPLACED FROM THE POLE AND  
ELONGATED OVER NORTH AMERICA. RECENT FORECASTS FROM THE ECMWF MODEL PREDICT  
ENHANCED PROBABILITIES OF A RARE NOVEMBER SUDDEN STRATOSPHERIC WARMING (SSW),  
AND PROPAGATION OF ATMOSPHERIC TEMPERATURE ANOMALIES TO THE SURFACE IN POLAR  
REGIONS, RESULTING IN A NEGATIVE ARCTIC OSCILLATION (AO). FORECASTS OF THE  
POTENTIAL SSW EVENT REMAIN UNCERTAIN AND CHANGE FROM MODEL RUN TO RUN. ALTHOUGH  
THERE IS STILL SUBSTANTIAL UNCERTAINTY, AN SSW COULD GREATLY IMPACT THE CLIMATE  
OUTLOOK FOR DECEMBER OVER NORTH AMERICA.  
 
THE MADDEN JULIAN OSCILLATION (MJO) HAS RECENTLY BEEN ACTIVE WITH ENHANCED  
CONVECTION CURRENTLY OVER THE FAR WESTERN PACIFIC OCEAN. DYNAMICAL MODELS SUCH  
AS THE ECMWF PREDICT THE POTENTIAL PROPAGATION OF THE MJO SIGNAL EASTWARD INTO  
THE WESTERN PACIFIC. THE MJO IN THIS PHASE ENHANCES THE CHANCES OF COLD AIR  
INTRUSION INTO THE NORTH-CENTRAL CONTIGUOUS UNITED STATES (CONUS) IN EARLY  
DECEMBER EXTENDING INTO THE NORTHEAST WITH TIME. THE COMBINED INFLUENCE OF THE  
MJO, LA NIñA, AND A POSSIBLE SSW WERE CONSIDERED IN THE DECEMBER CLIMATE  
OUTLOOK.  
 
THE DECEMBER TEMPERATURE AND PRECIPITATION OUTLOOKS WERE BASED PRIMARILY ON  
DYNAMICAL MODEL AND STATISTICAL MODEL FORECASTS. DYNAMICAL MODEL FORECASTS FOR  
THE MONTH OF DECEMBER ARE FROM THE NORTH AMERICA MULTIMODEL ENSEMBLE (NMME). IN  
ADDITION TO THE NMME, A CONSOLIDATION OF MODEL FORECASTS WAS UTILIZED, WHICH  
INCLUDES THE FOLLOWING STATISTICAL TOOLS: THE CANONICAL CORRELATION ANALYSIS  
(CCA), THE CONSTRUCTED ANALOG (CA), AND AN ENSO OCN TOOL, THAT COMBINES THE  
IMPACT OF ENSO, BASED ON THE CPC SST CONSOLIDATION PREDICTED MEDIAN NIñO 3.4  
SST ANOMALY, WITH THE OPTIMUM CLIMATE NORMAL (OCN) TO REPRESENT DECADAL TRENDS.  
DAILY INITIALIZED FORECASTS FROM THE CLIMATE FORECAST SYSTEM (CFSV2) DYNAMICAL  
MODEL FOR THE MONTH OF DECEMBER AND THE MOST RECENT ECMWF AND GEFS DYNAMICAL  
MODEL FORECASTS FOR THE WEEK 3-4 PERIOD THAT OVERLAPS THE BEGINNING OF THE  
MONTH OF DECEMBER WERE ALSO CONSIDERED. RECENT BOUNDARY CONDITIONS, INCLUDING  
COASTAL SSTS, AND SOIL MOISTURE ANOMALIES, WERE ADDITIONAL FACTORS CONSIDERED  
IN THE OUTLOOK.  
 
THE DECEMBER OUTLOOK FAVORS ABOVE NORMAL TEMPERATURES FOR THE EASTERN  
ALEUTIANS, WESTERN MAINLAND ALASKA, AND THE NORTH SLOPE, CONSISTENT WITH  
DYNAMICAL MODEL GUIDANCE FROM THE NMME AND CFSV2, AS WELL AS DECADAL CLIMATE  
TRENDS. BELOW NORMAL TEMPERATURES ARE FAVORED FOR PARTS OF SOUTHEASTERN  
MAINLAND ALASKA AND SOUTHEAST ALASKA, CONSISTENT WITH DYNAMICAL MODEL FORECASTS  
FROM THE NMME AND CFSV2, AS WELL AS THE COMBINED IMPACTS OF LA NIñA AND THE  
PREDICTED PROPAGATION OF THE MJO INTO THE WESTERN PACIFIC. THE TEMPERATURE  
PATTERN OVER THE CONUS IN THE DECEMBER OUTLOOK IS CONSISTENT WITH THE LA NIñA  
BASE STATE MODIFIED BY THE IMPACTS OF MJO AND A POTENTIAL SSW. ABOVE NORMAL  
TEMPERATURES ARE FAVORED ACROSS THE SOUTHERN TIER FROM CALIFORNIA, ACROSS THE  
SOUTHWEST, INTO THE GULF COAST REGION AND SOUTHEAST. PROBABILITIES EXCEED 50  
PERCENT OVER PARTS OF THE DESERT SOUTHWEST AND RIO GRANDE VALLEY, CONSISTENT  
WITH RECENT TEMPERATURE FORECASTS FROM THE CFSV2, THE CONSOLIDATION, AND  
DECADAL TRENDS. PROBABILITIES FOR ABOVE NORMAL TEMPERATURES FOR THIS REGION ARE  
ALSO ENHANCED BY THE CORRELATION BETWEEN PREDICTED BELOW NORMAL PRECIPITATION  
AND ABOVE NORMAL TEMPERATURES. PROBABILITIES FOR ABOVE NORMAL TEMPERATURES OVER  
MUCH OF CALIFORNIA AND NEVADA ARE REDUCED, DUE TO UNCERTAINTY RELATED TO AN  
ACTIVE MJO AND ECMWF AND GEFS FORECASTS FOR THE FIRST HALF OF THE MONTH THAT  
SHOW WEAK SIGNALS OVER MUCH OF THE WEST. PROBABILITIES FAVORING ABOVE NORMAL  
TEMPERATURES OVER THE SOUTHEAST AND PARTS OF THE MID-ATLANTIC COAST ARE  
CONSISTENT WITH THE IMPACTS OF LA NIñA. BELOW NORMAL TEMPERATURES ARE FAVORED  
FOR THE NORTHERN CONUS FROM NORTHERN WASHINGTON ACROSS THE NORTHERN ROCKIES  
INTO THE NORTHERN GREAT PLAINS, THE GREAT LAKES REGION, AND ALONG THE CANADIAN  
BORDER OF THE NORTHEAST, BASED ON RECENT FORECASTS FROM THE CFSV2 MODEL FOR  
DECEMBER, AS WELL AS FORECASTS FOR THE FIRST HALF OF DECEMBER FROM THE ECMWF  
MODEL. THE PREDICTED TEMPERATURE PATTERN IS LARGELY CONSISTENT WITH THE  
COMBINED INFLUENCES OF LA NIñA AND MJO PROPAGATION INTO THE WESTERN PACIFIC.  
DEVELOPMENT OF AN SSW WOULD SUBSTANTIALLY INCREASE THE PROBABILITIES OF BELOW  
NORMAL TEMPERATURES OVER THE CENTRAL CONUS.  
 
THE DECEMBER OUTLOOK FAVORS ABOVE NORMAL PRECIPITATION FOR THE EASTERN  
ALEUTIANS, WESTERN MAINLAND ALASKA, AND PARTS OF THE NORTH SLOPE, CONSISTENT  
WITH THE CONSOLIDATION OF DYNAMICAL AND STATISTICAL MODEL PRECIPITATION  
FORECASTS AND DECADAL TRENDS. BELOW NORMAL PRECIPITATION IS FAVORED FOR THE  
SOUTHEASTERN COAST OF MAINLAND ALASKA INCLUDING SOUTHEAST ALASKA, CONSISTENT  
WITH DYNAMICAL MODEL FORECASTS FOR DECEMBER, LA NIñA, AND IMPACTS OF A WESTERN  
PACIFIC MJO. ABOVE NORMAL PRECIPITATION IS FAVORED OVER MUCH OF THE  
NORTHWESTERN CONUS FROM EASTERN AREAS OF THE PACIFIC NORTHWEST TO THE NORTHERN  
HIGH PLAINS, CONSISTENT WITH THE CFSV2 FORECAST FOR DECEMBER AND THE ECMWF  
FORECAST FOR THE FIRST HALF OF THE MONTH. EQUAL CHANCES (EC) OF ABOVE AND BELOW  
NORMAL PRECIPITATION IS INDICATED CLOSER TO THE COAST OF THE PACIFIC NORTHWEST,  
WHERE THE DECEMBER CONSOLIDATION FORECAST AND THE CPC WEEK 3-4 OUTLOOK INDICATE  
UNCERTAINTY IN THE PRECIPITATION SIGNAL. ABOVE NORMAL PRECIPITATION IS ALSO  
FAVORED FOR THE OHIO VALLEY, GREAT LAKES REGION, AND NORTHEAST, CONSISTENT WITH  
DYNAMICAL MODEL FORECASTS FOR THE FIRST TWO WEEKS OF DECEMBER AND POSSIBLE  
IMPACTS OF AN ACTIVE MJO IN THE WESTERN PACIFIC AND A POTENTIAL SSW. BELOW  
NORMAL PRECIPITATION IS FAVORED FOR EASTERN AREAS OF THE SOUTHWEST, INCLUDING  
PARTS OF ARIZONA, NEW MEXICO AND TEXAS, AND FOR PARTS OF THE SOUTHEAST GULF AND  
ATLANTIC COASTS, CONSISTENT WITH CANONICAL IMPACTS OF LA NIñA AND PREDICTED BY  
THE NMME AND CONSOLIDATION FORECASTS. THERE IS GREATER UNCERTAINTY, INDICATED  
BY EC, IN THE PRECIPITATION OUTLOOK FOR CALIFORNIA AND WESTERN AREAS OF THE  
SOUTHWEST.  
 
FORECASTER: DAN COLLINS  
 
THE CLIMATIC NORMALS ARE BASED ON CONDITIONS BETWEEN 1991 AND 2020, FOLLOWING  
THE WORLD METEOROLOGICAL ORGANIZATION CONVENTION OF USING THE MOST RECENT 3  
COMPLETE DECADES AS THE CLIMATE REFERENCE PERIOD. THE PROBABILITY ANOMALIES  
FOR TEMPERATURE AND PRECIPITATION BASED ON THESE NEW NORMALS BETTER REPRESENT  
SHORTER TERM CLIMATIC ANOMALIES THAN THE FORECASTS BASED ON OLDER NORMALS.  
 
AN UPDATED MONTHLY OUTLOOK... FOR DEC WILL BE ISSUED ON SUN NOVEMBER 30 2025  
 
THESE OUTLOOKS ARE BASED ON DEPARTURES FROM THE 1991-2020 BASE PERIOD.  

 
 
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