535  
FXUS07 KWBC 181331  
PMD30D  
PROGNOSTIC DISCUSSION FOR MONTHLY OUTLOOK  
NWS CLIMATE PREDICTION CENTER COLLEGE PARK MD  
300 PM EST THU DEC 18 2025  
 
30-DAY OUTLOOK DISCUSSION FOR JANUARY 2026  
 
THE JANUARY 2026 MONTHLY TEMPERATURE AND PRECIPITATION OUTLOOKS ARE CONSTRUCTED  
BY CONSIDERING THE LA NIñA BASE STATE, AS WELL AS DYNAMICAL CLIMATE MODELS AND  
INTEGRATED STATISTICAL TOOLS. EQUATORIAL SEA SURFACE TEMPERATURES (SSTS) REMAIN  
BELOW AVERAGE ACROSS THE CENTRAL AND EAST-CENTRAL PACIFIC OCEAN, WITH SST  
DEPARTURES IN THE NIñO 3.4 REGION REACHING -0.7 DEGREES C. THESE BELOW-AVERAGE  
SSTS HAVE PERSISTED SINCE SEPTEMBER 2025, AND WE ARE FIRMLY WITHIN WEAK LA NIñA  
TERRITORY. FURTHERMORE, ATMOSPHERIC ANOMALIES OVER THE TROPICAL PACIFIC OCEAN  
ARE CONSISTENT WITH LA NIñA, CONSEQUENTLY, WE EXPECT LA NIñA TELECONNECTIONS  
DURING JANUARY 2026. IN CONTRAST, THE MADDEN-JULIAN OSCILLATION (MJO) REMAINS  
MORE UNCERTAIN, AS MODELS SUGGEST DESTRUCTIVE INTERFERENCE FROM A STRONG KELVIN  
WAVE MAY HINDER ITS RE-EMERGENCE. THE JANUARY 2026 OUTLOOKS ARE PRIMARILY  
SHAPED BY THE LA NIñA BACKGROUND STATE, DYNAMICAL CLIMATE MODELS, LOCAL SST  
ANOMALIES, SEA ICE, AND LAND SURFACE CONDITIONS (WHERE APPROPRIATE). AN  
EXPERIMENTAL MULTIPLE LINEAR REGRESSION (MLR) TOOL WHICH ESTIMATES THE  
INFLUENCES OF THE EL NIñO SOUTHERN OSCILLATION (ENSO), MJO, AND DECADAL TRENDS  
IS UTILIZED, AS IS A CONSOLIDATION THAT INCLUDES INFLUENCE OF ENSO, DECADAL  
TRENDS, AND CALIBRATED NORTH AMERICAN MULTI-MODEL ENSEMBLE (NMME) OUTPUT. WEEKS  
3-4 FORECASTS FROM THE GLOBAL ENSEMBLE FORECAST SYSTEM VERSION 12 (GEFSV12),  
THE EUROPEAN CENTRE FOR MEDIUM-RANGE WEATHER FORECASTS (ECMWF), AND COUPLED  
FORECAST SYSTEM VERSION 2 (CFSV2) MODELS THAT COVER THE PERIOD TO ABOUT  
MID-JANUARY WERE ALSO CONSIDERED. IMPACTS FROM THE MJO, ALONG WITH LAND SURFACE  
VARIABLES SUCH AS SNOW COVER, WILL BE RE-EVALUATED AT THE END OF THE MONTH FOR  
THE UPDATED VERSION OF THIS OUTLOOK.  
 
THE JANUARY 2026 TEMPERATURE OUTLOOK FEATURES INCREASED CHANCES OF BELOW-NORMAL  
TEMPERATURES FOR MUCH OF MAINLAND ALASKA, ALL OF SOUTHEAST ALASKA, AND  
STRETCHING FROM THE NORTHERN ROCKIES TO THE UPPER MISSISSIPPI VALLEY.  
ABOVE-NORMAL TEMPERATURES ARE MORE LIKELY FOR THE SOUTHERN TIER OF THE  
CONTIGUOUS UNITED STATES (CONUS), COVERING MUCH OF THE SOUTHWEST, FOUR CORNERS,  
SOUTHERN PLAINS, SOUTHEAST, AND MID-ATLANTIC. EQUAL CHANCES (EC) OF ABOVE-,  
NEAR-, AND BELOW-NORMAL TEMPERATURES ARE FORECAST FOR WESTERN AND NORTHERN  
ALASKA, THE NORTHWEST, MUCH OF NORTHERN AND CENTRAL CALIFORNIA, THE CENTRAL  
PLAINS, GREAT LAKES, AND NEW ENGLAND. A MID-LEVEL HEIGHT PATTERN TYPICAL OF LA  
NIñA HAS BEEN ESTABLISHED AND IS FORECAST TO PERSIST INTO AT LEAST MID-JANUARY  
PER WEEK 3-4 DYNAMICAL MODELS. A BLOCKING HIGH HAS BEEN A SIGNIFICANT FEATURE  
OVER THE NORTH PACIFIC AND ALEUTIANS, WITH DOWNSTREAM MID-LEVEL LOW PRESSURE  
RESIDING OVER EASTERN ALASKA AND PORTIONS OF THE NORTHWEST. ABOVE-AVERAGE  
MID-LEVEL HEIGHTS COVER MUCH OF THE SOUTHERN TIER AND EASTERN CONUS. THE  
PATTERN REFLECTED IN THE JANUARY 2026 TEMPERATURE OUTLOOKS IS CONSISTENT WITH  
LA NIñA EXPECTATIONS, THOUGH IT HAS BEEN MODIFIED BASED ON AVAILABLE GUIDANCE.  
 
PROBABILITIES FOR BELOW-NORMAL TEMPERATURES ARE HIGHEST OVER SOUTHEAST ALASKA  
AND ADJACENT AREAS OF SOUTHEASTERN MAINLAND ALASKA, REACHING 50 TO 60%, GIVEN  
CONSISTENCY AMONG VARIOUS TOOLS. MONTHLY FORECASTS FOR ALASKA FROM NMME, C3S,  
AND CFSV2 ALIGN WITH SHORTER-TERM WEEK 3-4 FORECASTS IN FAVORING THESE COOLER  
CONDITIONS. PROBABILITIES ARE ALSO ENHANCED, REACHING 50 TO 60%, OVER SOUTHERN  
NEW MEXICO, TEXAS, LOUISIANA, AND FLORIDA. THIS IS DRIVEN BY STRONG AGREEMENT  
BETWEEN DYNAMICAL MODELS AND HIGHER-PROBABILITY SIGNALS IN THE SHORTER-TERM  
WEEK 3-4 FORECASTS.  
 
WHILE DECADAL TRENDS AND CERTAIN TOOLS LIKE THE CFSV2 TILT TOWARD ABOVE-NORMAL  
TEMPERATURES OVER THE NORTHERN COAST OF ALASKA, EC IS INDICATED BECAUSE EARLY  
TO MID-JANUARY IS FORECAST TO BE AT LEAST SLIGHTLY BELOW-NORMAL, AND SEA ICE IS  
PRESENT ALONG THE COAST. SIMILARLY, WHILE LA NIñA OFTEN BRINGS BELOW-NORMAL  
TEMPERATURES TO THE NORTHERN TIER OF THE CONUS, SOMETIMES INCLUDING THE  
NORTHWEST, THE NMME, C3S, AND CFSV2 MONTHLY OUTLOOKS ARE GENERALLY ABOVE-NORMAL  
ALONG THE WESTERN THIRD OF THE COUNTRY. FURTHERMORE, SHOULD THE MJO BECOME MORE  
COHERENT, IT COULD INTRODUCE MORE VARIABILITY, SUCH AS COOLER TEMPERATURES IN  
THE WEST, THOUGH THIS INFLUENCE IS CURRENTLY HIGHLY UNCERTAIN. EC IS THUS  
FAVORED OVER MUCH OF THE WEST AND NORTHWEST AS WE CANNOT DISCOUNT THE  
POSSIBILITY OF COOLER AIR EXTENDING FURTHER WEST AND SOUTH.  
 
SIMILARLY, MODELS ARE WARM OVER THE CENTRAL CONUS, HOWEVER, IT IS NOT UNHEARD  
OF DURING JANUARY AND LA NIñA YEARS TO SEE COLD AIR INTRUSIONS REACH FURTHER  
SOUTH, AS SUCH WE TILT TOWARD EC OVER THE CENTRAL CONUS AND WILL RE-ASSESS IN  
THE MONTHLY UPDATE. IN ADDITION, UNCERTAINTY IS HIGH IN THE CENTRAL CONUS IN A  
CONSOLIDATION OF STATISTICAL TOOLS (WHICH INCLUDE INFLUENCE OF TREND AND ENSO),  
AND NMME, WHICH ADDS TO OUR UNCERTAINTY HERE. FINALLY, GUIDANCE WAS MIXED AND  
INCONSISTENT OVER THE GREAT LAKES AND NEW ENGLAND, WHICH ALSO LED TO A TILT  
TOWARD EC. BECAUSE THIS LA NIñA IS CURRENTLY WEAK, INCREASED VARIABILITY AND  
UNCERTAINTY ARE POSSIBLE FOR SOME REGIONS, WHICH ALSO SUPPORTS EC.  
 
WHILE SOME REGIONS IN THE JANUARY TEMPERATURE OUTLOOK REMAIN UNCERTAIN DUE TO  
THE VARIABILITY OF WEAK LA NIñA TELECONNECTIONS, THE PRECIPITATION PATTERN IS  
MORE CONSISTENT ACROSS VARIOUS TOOLS, CLOSELY RESEMBLING THE EXPECTED LA NIñA  
SIGNATURE. ABOVE-NORMAL PRECIPITATION IS FAVORED FOR THE NORTHWEST, NORTHERN  
ROCKIES, GREAT LAKES, AND MUCH OF THE OHIO AND MIDDLE MISSISSIPPI VALLEYS.  
WESTERN ALASKA ALSO LEANS ABOVE-NORMAL. DRIER CONDITIONS ARE MORE LIKELY ACROSS  
THE SOUTHWEST, SOUTHERN PLAINS, AND MUCH OF THE SOUTHEAST. A WEAK TILT TOWARD  
BELOW-NORMAL PRECIPITATION IS ALSO INDICATED OVER MUCH OF THE SOUTHERN COAST OF  
MAINLAND ALASKA AND ALL OF SOUTHEAST ALASKA. WHILE THE NMME AND C3S FAVOR  
BELOW-NORMAL PRECIPITATION UP MUCH OF THE WEST COAST, REACHING INTO THE  
NORTHWEST IN SOME MODELS, RECENT FORECASTS FROM CFSV2 TILT ABOVE-NORMAL FOR THE  
MONTH OF JANUARY OVER THE NORTHWEST. MOREOVER, WEEK 3 AND WEEK 4 DYNAMICAL  
MODELS FORECAST AT LEAST 40 TO 50% CHANCES OF ABOVE-NORMAL PRECIPITATION OVER  
THE NORTHWEST. AS SUCH, WE HAVE MINIMIZED THE REGION OF BELOW-NORMAL  
PRECIPITATION FORECAST BY SOME OF THE MULTI-MODEL ENSEMBLES, CONFINING IT MORE  
TO SOUTHEASTERN CALIFORNIA. GIVEN THE UNCERTAINTY REGARDING HOW FAR SOUTH THE  
MOISTURE MAY REACH, MUCH OF CALIFORNIA IS DESIGNATED AS EC. ABOVE-NORMAL  
PRECIPITATION IS ALSO INDICATED FOR THE GREAT LAKES, OHIO VALLEY, AND PARTS OF  
THE MIDDLE AND LOWER MISSISSIPPI VALLEYS AND THE TENNESSEE VALLEY , WHICH IS A  
TYPICAL LA NIñA SIGNATURE. THESE TWO AREAS OF ABOVE-NORMAL PRECIPITATION ARE  
CONNECTED BY A WEAK (33 TO 40%) CHANCE OF ABOVE-NORMAL PRECIPITATION THAT IS  
SUPPORTED BY THE NMME AND C3S. THE BELOW-NORMAL PRECIPITATION FAVORED OVER THE  
SOUTHERN TIER IS CONSISTENT WITH MODELS AND LA NIñA, THOUGH SOME UNCERTAINTY  
EXISTS OVER PARTS OF TEXAS AND LOUISIANA AS IT IS CURRENTLY UNCLEAR HOW FAR  
SOUTH ANY ABOVE-NORMAL PRECIPITATION MIGHT REACH. FINALLY, OVER ALASKA, DECADAL  
TRENDS AND LA NIñA SUPPORT THE FORECAST FOR BELOW-NORMAL PRECIPITATION OVER THE  
SOUTHERN COAST OF THE MAINLAND AND SOUTHEAST ALASKA, WHILE DYNAMICAL MODELS  
LIKE THE NMME, C3S, AND CFSV2 FAVOR ABOVE-NORMAL PRECIPITATION FOR MUCH OF THE  
WESTERN MAINLAND.  
 
FORECASTER: JOHNNA INFANTI  
 
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.  
 
THE NEXT MONTHLY OUTLOOK...FOR FEB ... WILL BE ISSUED ON THU JAN 15 2026.  
 
THESE OUTLOOKS ARE BASED ON DEPARTURES FROM THE 1991-2020 BASE PERIOD.  
 
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