490  
FXUS05 KWBC 201331  
PMD90D  
PROGNOSTIC DISCUSSION FOR LONG-LEAD SEASONAL OUTLOOKS  
NWS CLIMATE PREDICTION CENTER COLLEGE PARK MD  
830 AM EST THU NOV 20 2025  
 
SUMMARY OF THE OUTLOOK FOR NON-TECHNICAL USERS  
 
LA NIñA CONDITIONS CONTINUE WITH SEA SURFACE TEMPERATURES (SSTS) BELOW AVERAGE  
ACROSS THE CENTRAL AND EASTERN EQUATORIAL PACIFIC OCEAN. LA NIñA IS SLIGHTLY  
FAVORED TO PERSIST THROUGH DECEMBER-JANUARY-FEBRUARY BUT IS LIKELY TO REMAIN  
WEAK. A TRANSITION TO ENSO-NEUTRAL CONDITIONS IS EXPECTED BY EARLY SPRING 2026.  
 
THE DECEMBER-JANUARY-FEBRUARY (DJF) 2025-26 TEMPERATURE OUTLOOK FAVORS  
ABOVE-NORMAL TEMPERATURES ACROSS MUCH OF THE EAST COAST, SOUTHEAST, GULF COAST,  
TEXAS, THE SOUTHWEST, AND CALIFORNIA. THE DJF TEMPERATURE OUTLOOK LEANS TOWARDS  
BELOW-NORMAL TEMPERATURES FROM THE UPPER MISSISSIPPI VALLEY AND NORTHERN TO  
CENTRAL GREAT PLAINS WEST TO PARTS OF THE PACIFIC NORTHWEST. AN INCREASED  
CHANCE OF BELOW (ABOVE)-NORMAL TEMPERATURES IS FORECAST FOR SOUTHEASTERN  
(NORTHWESTERN) ALASKA.  
 
THE DJF PRECIPITATION OUTLOOK DEPICTS ELEVATED BELOW-NORMAL PRECIPITATION  
PROBABILITIES FOR PORTIONS OF THE MID-ATLANTIC, SOUTHEAST, GULF COAST, TEXAS,  
THE SOUTHWEST, AND CALIFORNIA. ABOVE-NORMAL PRECIPITATION IS FAVORED FROM THE  
UPPER MISSISSIPPI VALLEY AND GREAT LAKES SOUTH TO THE OHIO VALLEY ALONG WITH  
THE NORTHERN GREAT PLAINS, NORTHERN ROCKIES, AND PARTS OF THE PACIFIC  
NORTHWEST. AN INCREASED CHANCE OF BELOW (ABOVE)-NORMAL PRECIPITATION IS  
FORECAST FOR SOUTHEASTERN (NORTHWESTERN) ALASKA.  
 
AREAS DEPICTED IN WHITE AND LABELED "EQUAL-CHANCES" OR "EC" ARE REGIONS WHERE  
CLIMATE SIGNALS ARE WEAK, AND SO THERE ARE EQUAL CHANCES FOR EITHER ABOVE-,  
NEAR- OR BELOW-NORMAL SEASONAL MEAN TEMPERATURES OR TOTAL PRECIPITATION AMOUNTS.  
 
BASIS AND SUMMARY OF THE CURRENT LONG-LEAD OUTLOOKS  
NOTE: FOR GRAPHICAL DISPLAYS OF THE FORECAST TOOLS DISCUSSED BELOW SEE:  
HTTP://WWW.CPC.NCEP.NOAA.GOV/PRODUCTS/PREDICTIONS/90DAY/TOOLS/BRIEFING  
 
CURRENT ATMOSPHERIC AND OCEANIC CONDITIONS  
 
WEEKLY OBSERVED SEA SURFACE TEMPERATURES (SSTS) IN THE NIñO 3.4 REGION ARE  
BELOW AVERAGE THROUGHOUT THE CENTRAL AND EASTERN EQUATORIAL PACIFIC. THE LATEST  
WEEKLY SST DEPARTURE, CENTERED ON NOVEMBER 12, IS -0.7 DEGREES C. THE NEGATIVE  
SST ANOMALIES RECENTLY EXPANDED EASTWARD ACROSS THE EQUATORIAL PACIFIC TO THE  
SOUTH AMERICAN COAST. SINCE THE BEGINNING OF SEPTEMBER, SUBSURFACE TEMPERATURE  
ANOMALIES (AVERAGED FROM 180-100W AND 0-300 METERS DEPTH) HAVE REMAINED  
NEGATIVE WITH LITTLE CHANGE IN MAGNITUDE.  
 
FROM OCTOBER 17 TO NOVEMBER 11, NEGATIVE OUTGOING LONGWAVE RADIATION (OLR)  
ANOMALIES (ENHANCED CONVECTION AND PRECIPITATION) CONTINUED OVER INDONESIA,  
SOUTHEAST ASIA, THE PHILIPPINES, AND PARTS OF NORTHERN AUSTRALIA. CONVERSELY,  
POSITIVE OLR ANOMALIES (SUPPRESSED CONVECTION AND PRECIPITATION) WERE OBSERVED  
AT AND NEAR THE DATE LINE. LOW-LEVEL (850-HPA) WIND ANOMALIES WERE EASTERLY  
FROM THE WESTERN TO THE EAST-CENTRAL EQUATORIAL PACIFIC OCEAN, WHILE  
UPPER-LEVEL (200-HPA) WIND ANOMALIES WERE WESTERLY OVER MOST OF THE EQUATORIAL  
PACIFIC. THESE ATMOSPHERIC AND OCEANIC CONDITIONS REFLECT LA NIñA CONDITIONS.  
 
THE MADDEN-JULIAN OSCILLATION (MJO) SLOWED AND WEAKENED DURING MID-NOVEMBER AS  
IT DESTRUCTIVELY INTERFERED WITH THE LA NIñA BACKGROUND STATE. DYNAMICAL MODEL  
REALTIME MULTIVARIATE MJO (RMM) FORECASTS DEPICT A STRENGTHENING MJO WITH  
EASTWARD PROPAGATION OVER THE WEST PACIFIC FROM LATE NOVEMBER TO THE BEGINNING  
OF DECEMBER. THE EXTRATROPICAL RESPONSE, ASSOCIATED WITH A WEST PACIFIC MJO,  
FAVORS AN AMPLIFYING 500-HPA RIDGE (TROUGH) OVER ALASKA (WEST-CENTRAL CONUS) BY  
THE END OF NOVEMBER WHICH WOULD PROMOTE ANOMALOUS COLD TO SHIFT SOUTHEAST INTO  
THE LOWER 48 STATES.  
 
PROGNOSTIC DISCUSSION OF SST FORECASTS  
 
THE CPC SST CONSOLIDATION FORECAST FOR NIñO 3.4 DEPICTS LA NIñA CONDITIONS  
PERSISTING THROUGH AT LEAST DJF AS THE SST ANOMALY REMAINS NEAR -0.5 DEGREES C.  
THE DYNAMICAL MODELS AND THE CONSTRUCTED ANALOG ARE IN GOOD AGREEMENT THAT SSTS  
BECOME CLOSER TO AVERAGE BY LATER IN THE WINTER OR EARLY NEXT SPRING. THE  
INTERNATIONAL MULTIMODEL ENSEMBLE (C3S) MEMBERS DEPICT A SIMILAR TIMING OF WHEN  
THE TRANSITION TO ENSO-NEUTRAL CONDITIONS HAPPENS. THE CPC ENSO OUTLOOK  
INDICATES THAT LA NIñA IS FAVORED TO PERSIST THROUGH DJF BEFORE A TRANSITION TO  
ENSO-NEUTRAL CONDITIONS DURING JANUARY-FEBRUARY-MARCH. ENSO-NEUTRAL IS STRONGLY  
FAVORED (NEAR OR MORE THAN A 70 PERCENT CHANCE) THROUGH THE 2026 SPRING.  
 
PROGNOSTIC TOOLS USED FOR U.S. TEMPERATURE AND PRECIPITATION OUTLOOKS  
 
THE TEMPERATURE AND PRECIPITATION OUTLOOKS FOR DJF 2025-26 WERE BASED ON LA  
NIñA COMPOSITES, EXPECTATIONS FOR PERIODS OF A NEGATIVE ARCTIC OSCILLATION, THE  
NORTH AMERICAN MULTI-MODEL ENSEMBLE (NMME), AND THE COPERNICUS (C3S)  
MULTI-MODEL ENSEMBLE SYSTEM. A CALIBRATION, BRIDGING, AND MERGING (CBAM)  
VERSION OF THE NMME WAS ALSO CONSIDERED. AN OBJECTIVE, HISTORICAL  
SKILL-WEIGHTED CONSOLIDATION THAT INCLUDES THE NMME ALONG WITH STATISTICAL  
TOOLS SUCH AS THE SST-BASED CONSTRUCTED ANALOG AND THE ENSO-OCN WAS USED  
THROUGH APRIL-MAY-JUNE 2026. BEYOND THAT TIME, THE CONSOLIDATION ONLY INCLUDES  
STATISTICAL TOOLS. LONG-TERM CLIMATE TRENDS WERE CONSIDERED FOR ALL LEADS, BUT  
WERE RELIED UPON MOST DURING THE SUMMER AND FALL 2026.  
 
PROGNOSTIC DISCUSSION OF OUTLOOKS - DJF 2025 TO DJF 2026  
 
TEMPERATURE  
 
THE DJF TEMPERATURE OUTLOOK WAS BASED LARGELY ON LA NIñA COMPOSITES, THE  
CALIBRATED NMME WHERE IT IS MORE SKILLFUL OVER PREVIOUS WINTER SEASONS, AND THE  
CONSOLIDATION TOOL. HIGH-LATITUDE BLOCKING HAS BEEN QUITE PREVALENT SINCE  
MID-OCTOBER WITH THE ARCTIC OSCILLATION (AO) IN A NEGATIVE PHASE FOR MUCH OF  
THE PAST MONTH. THE GEFS AND ECENS FAVOR A PERSISTENCE OF A NEGATIVE AO INTO  
THE BEGINNING OF DECEMBER. THE MADDEN-JULIAN OSCILLATION IS FORECAST TO  
STRENGTHEN AND PROPAGATE EAST OVER THE WEST PACIFIC (PHASE 7). THIS MJO  
EVOLUTION CAN LEAD TO AN AMPLIFYING MID-LEVEL RIDGE OVER ALASKA AND AN OUTBREAK  
OF ANOMALOUSLY COLD TEMPERATURES SHIFTING SOUTHEAST FROM THE NORTH-CENTRAL TO  
EASTERN CONUS. DUE TO A PERSISTENT NEGATIVE AO AND AN EXPECTED MJO INFLUENCE,  
EARLY DECEMBER IS LIKELY TO BE COLDER-THAN-NORMAL ACROSS THE MIDWEST AND THE  
DECEMBER OUTLOOK DEPICTS ELEVATED BELOW-NORMAL TEMPERATURE PROBABILITIES FOR  
THIS REGION. THIS FAVORED COLDER-THAN-NORMAL FORECAST FOR DECEMBER WAS A FACTOR  
IN EXPANDING THE SLIGHT LEAN TOWARDS BELOW SOUTHEASTWARD COMPARED TO THE DJF  
OUTLOOK RELEASED IN OCTOBER. IN ADDITION TO THE NEGATIVE AO AND MJO INFLUENCES,  
THE STRATOSPHERIC POLAR VORTEX IS FORECAST TO BECOME STRETCHED AND DISPLACED  
OFF THE NORTH POLE. ALTHOUGH A MAJOR SUDDEN STRATOSPHERIC WARMING (SSW) IS NOT  
FORECAST BY THE GEFS, THE ECMWF ENSEMBLE MEAN FROM NOVEMBER 18 DEPICTS A SLIGHT  
REVERSAL OF 10-HPA ZONAL WINDS AT 60N CONSISTENT WITH A SSW, WHICH COULD  
PROLONG THE NEGATIVE AO. A SSW WOULD BE VERY RARE FOR THIS TIME OF YEAR. EVEN  
IF A SSW DOES NOT OCCUR DURING LATE NOVEMBER, THIS MAY SET THE STAGE FOR  
ADDITIONAL POLAR VORTEX DISRUPTIONS AND A MAJOR SSW WITH IMPACTS TO THE  
TROPOSPHERE LATER THIS WINTER. TEMPERATURES ARE EXPECTED TO BE HIGHLY VARIABLE  
ALONG AND NORTH OF THE 40TH PARALLEL THIS WINTER WHICH IS TYPICAL DURING LA  
NIñA. THE DJF OUTLOOK LEANS TOWARDS BELOW-NORMAL TEMPERATURES FROM THE UPPER  
MISSISSIPPI VALLEY AND NORTHERN TO CENTRAL GREAT PLAINS WEST TO THE NORTHERN  
ROCKIES AND PARTS OF THE PACIFIC NORTHWEST WHERE BELOW-NORMAL TEMPERATURES  
OCCUR MOST FREQUENTLY DURING LA NIñA WINTERS AND THERE IS ADDITIONAL SUPPORT  
FROM THE CONSOLIDATION TOOL. THE CALIBRATED NMME SUPPORTS AN INCREASED CHANCE  
OF ABOVE-NORMAL TEMPERATURES FOR MUCH OF CALIFORNIA, THE SOUTHWEST, RIO GRANDE  
VALLEY, GULF COAST, SOUTHEAST, MID-ATLANTIC, AND SOUTHERN NEW ENGLAND. DUE TO  
GOOD AGREEMENT AND CONSISTENCY AMONG THE TOOLS, THE HIGHEST FORECAST CONFIDENCE  
IN THE DJF TEMPERATURE OUTLOOK IS FOR ABOVE-NORMAL TEMPERATURES (50-60 PERCENT  
CHANCE) ACROSS THE FLORIDA PENINSULA AND PARTS OF THE SOUTHWEST. IN BETWEEN THE  
FAVORED ABOVE ACROSS THE SOUTHERN TIER AND BELOW FARTHER TO THE NORTH, EQUAL  
CHANCES OF BELOW, NEAR, OR ABOVE-NORMAL TEMPERATURES ARE FORECAST AS THESE  
AREAS ARE EXPECTED TO HAVE THE MOST TEMPERATURE VARIABILITY THIS WINTER. THE  
ALASKA TEMPERATURE OUTLOOK IS QUITE CONSISTENT WITH LA NIñA COMPOSITES AND  
DYNAMICAL MODELS WHICH CALL FOR AN INCREASED CHANCE OF BELOW (ABOVE)-NORMAL  
TEMPERATURES FOR SOUTHEASTERN (NORTHWESTERN) ALASKA.  
 
THE JANUARY-FEBRUARY-MARCH (JFM) AND FEBRUARY-MARCH-APRIL TEMPERATURE OUTLOOKS  
HEDGED SLIGHTLY COLDER THAN THE DYNAMICAL MODEL GUIDANCE ACROSS THE GREAT  
PLAINS DUE TO THE POTENTIAL FOR ADDITIONAL PERIODS OF A NEGATIVE AO PHASE AND  
AT LEAST ONE ARCTIC AIR OUTBREAK IN JANUARY AND/OR FEBRUARY. IT SHOULD BE NOTED  
THAT PROBABILITIES FOR BELOW OR ABOVE-NORMAL TEMPERATURES ARE LESS THAN 50  
PERCENT THROUGHOUT THE FORECAST DOMAIN DURING JFM AS FORECAST CONFIDENCE IS  
TEMPERED DUE TO THE EXPECTATION OF A HIGHLY VARIABLE PATTERN WITHIN THIS  
THREE-MONTH PERIOD. BY APRIL-MAY-JUNE, ABOVE-NORMAL TEMPERATURES BECOME THE  
MOST LIKELY CATEGORY FOR A MAJORITY OF THE LOWER 48 STATES AND ALASKA, AND THEN  
THE ENTIRE FORECAST DOMAIN IS FAVORED TO HAVE ABOVE-NORMAL TEMPERATURES DURING  
SEPTEMBER-OCTOBER-NOVEMBER CONSISTENT WITH LONG-TERM TRENDS.  
 
PRECIPITATION  
 
THE DJF PRECIPITATION OUTLOOK IS CONSISTENT WITH LA NIñA COMPOSITES AS THE  
SOUTHERN TIER OF THE CONUS IS TYPICALLY DRIER-THAN-NORMAL WITH ABOVE-NORMAL  
PRECIPITATION MORE LIKELY FOR THE NORTHERN ROCKIES, NORTHERN GREAT PLAINS,  
UPPER MISSISSIPPI VALLEY, AND FROM THE GREAT LAKES SOUTH TO THE OHIO AND  
TENNESSEE VALLEYS. DESPITE A WET SIGNAL IN LA NIñA COMPOSITES FOR WESTERN PARTS  
OF OREGON AND WASHINGTON, EQUAL CHANCES (EC) FOR BELOW, NEAR, OR ABOVE-NORMAL  
PRECIPITATION ARE FORECAST BASED ON THE NMME AND CONSOLIDATION TOOL. COMPARED  
TO THE PREVIOUS MONTH'S RELEASE, BELOW-NORMAL PRECIPITATION PROBABILITIES WERE  
DECREASED TO BELOW 40 PERCENT FOR SOUTHERN CALIFORNIA AND THE SOUTHWEST AS THE  
SST-CONSTRUCTED ANALOG HAS A WETTER SIGNAL FOR THESE AREAS. ALSO, THE UNUSUALLY  
WET OCTOBER AND NOVEMBER DECREASE FORECAST CONFIDENCE THAT BELOW-NORMAL  
PRECIPITATION WILL VERIFY DURING DJF. THE HIGHEST CONFIDENCE IN BELOW-NORMAL  
PRECIPITATION ACROSS THE SOUTHERN TIER OF THE CONUS EXISTS FOR PORTIONS OF THE  
SOUTHEAST WHERE DRIER-THAN-NORMAL WINTERS ARE VERY RELIABLE DURING LA NIñA.  
BELOW-NORMAL PRECIPITATION PROBABILITIES DECREASE TO THE SOUTH ACROSS THE  
FLORIDA PENINSULA DUE IN PART TO THE DRIER WINTER CLIMATOLOGY. ELEVATED  
BELOW-NORMAL PRECIPITATION PROBABILITIES EXTEND NORTHWARD TO THE MID-ATLANTIC  
AS THE PRIMARY STORM TRACK IS EXPECTED TO BE FARTHER TO THE WEST ACROSS THE  
OHIO VALLEY. THIS FAVORED WINTER STORM TRACK RESULTS IN ENHANCED ABOVE-NORMAL  
PRECIPITATION PROBABILITIES FOR THE OHIO VALLEY. IT IS TYPICAL TO HAVE A TIGHT  
GRADIENT BETWEEN ABOVE AND BELOW NORMAL PRECIPITATION FROM THE TENNESSEE VALLEY  
SOUTH TO THE GULF COAST DURING LA NIñA WINTERS. BASED ON LA NIñA COMPOSITES AND  
GOOD MODEL AGREEMENT, THE LARGEST ABOVE-NORMAL PRECIPITATION PROBABILITIES  
(MORE THAN 50 PERCENT) ARE FORECAST ACROSS THE NORTHERN ROCKIES AND NORTHERN  
HIGH PLAINS. GOOD MODEL CONSISTENCY SUPPORTS AN INCREASED CHANCE OF  
ABOVE-NORMAL PRECIPITATION FOR WESTERN MAINLAND ALASKA. OVERALL THE  
PRECIPITATION TOOLS HAVE TRENDED WETTER FOR SOUTHEASTERN ALASKA WHERE NOW THE  
DJF OUTLOOK ONLY SLIGHTLY LEANS TOWARDS THE DRIER SIDE.  
 
ALTHOUGH A TRANSITION TO ENSO-NEUTRAL CONDITIONS IS LIKELY TO OCCUR DURING  
JANUARY-FEBRUARY-MARCH 2026, A LA NIñA INFLUENCE ON THE MID-LATITUDE  
CIRCULATION PATTERN AND ANOMALOUS PRECIPITATION IS EXPECTED TO LINGER THROUGH  
THE LATE WINTER OR EVEN EARLY SPRING. THEREFORE, THE JFM AND  
FEBRUARY-MARCH-APRIL PRECIPITATION OUTLOOKS ARE SIMILAR TO LA NIñA COMPOSITES  
WITH MINOR ADJUSTMENTS BASED ON THE NMME, C3S, AND CONSOLIDATION. LATER IN THE  
SPRING AND INTO THE SUMMER 2026, THE COVERAGE OF EC INCREASES DUE TO WEAK  
AND/OR CONFLICTING SIGNALS AMONG FORECAST GUIDANCE. AT THE LONGER LEAD TIMES,  
LONG-TERM TRENDS WERE USED TO IDENTIFY ANY AREAS WITH EITHER FAVORED BELOW OR  
ABOVE-NORMAL PRECIPITATION.  
 
FORECASTER: BRAD PUGH  
 
THE CLIMATIC NORMALS ARE BASED ON CONDITIONS BETWEEN 1991 AND 2020, FOLLOWING  
THE WORLD METEROLOGICAL ORGANIZATION CONVENTION OF USING THE MOST RECENT 3  
COMPLETE DECADES AS THE CLIMATIC 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.  
 
FOR A DESCRIPTION OF OF THE STANDARD FORECAST TOOLS - THEIR SKILL- AND THE  
FORECAST FORMAT PLEASE SEE OUR WEB PAGE AT  
HTTP://WWW.CPC.NCEP.NOAA.GOV/PRODUCTS/PREDICTIONS/LONG_RANGE/TOOLS.HTML  
(USE LOWER CASE LETTERS)  
INFORMATION ON THE FORMATION OF SKILL OF THE CAS FORECASTS MAY BE FOUND AT:  
HTTP://WWW.CPC.NCEP.NOAA.GOV/PRODUCTS/SOILMST_MONITORING/US/OUTLOOK/OUTLOOK.SHTM  
L  
(USE LOWERCASE LETTERS)  
NOTES - THESE CLIMATE OUTLOOKS ARE INTENDED FOR USE PRIOR TO THE START OF THEIR  
VALID PERIOD. WITHIN ANY GIVEN VALID PERIOD OBSERVATIONS AND SHORT AND MEDIUM  
RANGE FORECASTS SHOULD BE CONSULTED.  
 
THIS SET OF OUTLOOKS WILL BE SUPERSEDED BY THE ISSUANCE OF THE NEW SET NEXT  
MONTH ON DEC 18 2025  
 
1991-2020 BASE PERIOD MEANS WERE IMPLEMENTED EFFECTIVE WITH THE MAY 20, 2021  
FORECAST RELEASE.  

 
 
CLICK HERE TO GO TO PREVIOUS BULLETINS.

The Nexlab HPC Page Main Text Page