632  
FXUS05 KWBC 181231  
PMD90D  
PROGNOSTIC DISCUSSION FOR LONG-LEAD SEASONAL OUTLOOKS  
NWS CLIMATE PREDICTION CENTER COLLEGE PARK MD  
830 AM EDT THU JUN 18 2026  
 
SUMMARY OF THE OUTLOOK FOR NON-TECHNICAL USERS  
 
EL NINO CONDITIONS HAVE RECENTLY DEVELOPED IN THE TROPICS AND ARE EXPECTED TO  
STRENGTHEN IN THE BOREAL SUMMER AND AUTUMN OF 2026. THE NOAA EL NINO SOUTHERN  
OSCILLATION (ENSO) OUTLOOK PREDICTS A GREATER THAN 40 PERCENT CHANCE OF THIS EL  
NINO EVENT BECOMING STRONG BY THE JULY-AUGUST-SEPTEMBER (JAS) SEASON, AS  
DETERMINED BY THE RELATIVE ANOMALY OF THE NINO 3.4 REGION TO THE GLOBAL  
TROPICAL SEA SURFACE TEMPERATURE ANOMALY.  
 
THE JAS SEASONAL OUTLOOK FOR TEMPERATURE FAVORS ABOVE NORMAL TEMPERATURES  
ACROSS MOST OF ALASKA, EXCLUDING PARTS OF THE NORTHEASTERN MAINLAND. ABOVE  
NORMAL TEMPERATURES ARE LIKELY FOR MUCH OF THE WESTERN CONTIGUOUS UNITED STATES  
(CONUS), WITH THE HIGHEST PROBABILITIES FOR ABOVE NORMAL TEMPERATURES ACROSS  
THE PACIFIC NORTHWEST. ABOVE NORMAL TEMPERATURES ARE FAVORED FOR THE LOWER  
MISSISSIPPI VALLEY, THE SOUTHEAST, AND THE EASTERN SEABOARD, WITH HIGHEST  
PROBABILITIES ALONG THE COAST OF NEW ENGLAND AND ENHANCED PROBABILITIES ALONG  
THE REMAINDER OF THE EAST COAST AND FLORIDA.  
 
THE JAS SEASONAL OUTLOOK FOR PRECIPITATION FAVORS ABOVE NORMAL PRECIPITATION  
FOR NORTHWESTERN MAINLAND ALASKA AND THE ALEUTIAN ISLANDS, WHILE BELOW NORMAL  
PRECIPITATION IS FAVORED FOR SOUTHERN AREAS OF SOUTHEAST ALASKA. BELOW NORMAL  
PRECIPITATION IS ALSO FAVORED FOR A SMALL AREA OF THE PACIFIC NORTHWEST, PARTS  
OF THE SOUTHERN PLAINS AND LOWER MISSISSIPPI VALLEY, AND THE WESTERN GREAT  
LAKES REGION. ABOVE NORMAL PRECIPITATION IS FAVORED FOR AN EXPANDED AREA OF THE  
WEST, AND SLIGHTLY FAVORED FOR COASTAL AREAS OF THE MID-ATLANTIC AND NORTHEAST.  
 
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  
 
THE MOST RECENT WEEKLY MEAN SEA SURFACE TEMPERATURE (SST) ANOMALY FOR THE NINO  
3.4 REGION RELATIVE TO THE GLOBAL TROPICS IS +0.9 DEGREES C, INDICATING WEAK EL  
NINO CONDITIONS. SST ANOMALIES HAVE INCREASED ACROSS THE CENTRAL AND EASTERN  
EQUATORIAL PACIFIC OCEAN IN RECENT WEEKS. POSITIVE OCEAN TEMPERATURE ANOMALIES  
PERSIST ACROSS MOST OF THE EQUATORIAL PACIFIC OCEAN FROM THE SURFACE TO DEPTHS  
OF 200 METERS OR GREATER IN THE EASTERN PACIFIC. NEGATIVE OUTGOING LONGWAVE  
RADIATION (OLR) ANOMALIES ARE PRESENT NEAR THE DATE LINE AND OVER PARTS OF THE  
EASTERN PACIFIC TO THE NORTH OF THE EQUATOR, INDICATING ENHANCED CONVECTION AND  
PRECIPITATION. POSITIVE OLR ANOMALIES, INDICATING SUPPRESSED CONVECTION AND  
PRECIPITATION, ARE PRESENT TO THE SOUTH OF THE EQUATOR FROM PARTS OF THE  
MARITIME CONTINENT TO THE DATE LINE. LOW LEVEL (850-HPA) EASTERLY WIND  
ANOMALIES WERE PRESENT OVER THE WESTERN AND CENTRAL EQUATORIAL PACIFIC OCEAN IN  
RECENT WEEKS. THESE ATMOSPHERE AND OCEAN ANOMALY PATTERNS INDICATE EL NINO  
CONDITIONS ARE PRESENT.  
 
POSITIVE SST ANOMALIES ARE OBSERVED NEAR THE COAST OF SOUTHERN CALIFORNIA.  
NEGATIVE SST ANOMALIES ARE PRESENTLY NEAR THE CENTRAL GULF AND MID-ATLANTIC  
COASTS. PERSISTENT COASTAL SST ANOMALIES MAY INFLUENCE SEASONAL TEMPERATURES OF  
ADJACENT AREAS.  
 
PROGNOSTIC DISCUSSION OF SST FORECASTS  
 
MOST SST FORECASTS FROM THE NORTH AMERICAN MULTI-MODEL ENSEMBLE (NMME) AND THE  
COPERNICUS CLIMATE CHANGE SERVICE (C3S) MULTI-MODEL ENSEMBLE PREDICT THAT  
RELATIVE NINO 3.4 ANOMALIES WILL EXCEED +1.0 DEGREES C BY JAS 2026. THE NMME  
MULTI-MODEL MEAN FORECAST EXCEEDS +2.0 DEGREES C BY THE  
OCTOBER-NOVEMBER-DECEMBER (OND) 2026 SEASON. THE CPC SST CONSOLIDATION FORECAST  
FOR THE RELATIVE NINO 3.4 INDEX INCREASES THROUGH SUMMER AND AUTUMN TO A PEAK  
MEDIAN VALUE OF +1.9 DEGREES C IN THE NOVEMBER-DECEMBER-JANUARY (NDJ) 2026-27  
SEASON, BEFORE DECREASING THEREAFTER. THE CONTINUATION OF AN EL NINO EVENT IS  
LIKELY THROUGH FMA 2027, ACCORDING TO THE SST CONSOLIDATION, AND THE CPC ENSO  
OUTLOOK PREDICTS THAT THE LIKELIHOOD OF A VERY STRONG EVENT WITH A PEAK  
SEASONAL RELATIVE NINO 3.4 INDEX GREATER THAN +2.0 DEGREES C EXCEEDS 60  
PERCENT.  
 
PROGNOSTIC TOOLS USED FOR U.S. TEMPERATURE AND PRECIPITATION OUTLOOKS  
 
THE SEASONAL TEMPERATURE AND PRECIPITATION OUTLOOKS ARE BASED PRIMARILY ON  
FORECAST TOOLS DERIVED FROM THE NMME, INCLUDING CALIBRATED VERSIONS, SUCH AS  
THE PROBABILITY ANOMALY CORRELATION (PAC) AND THE CALIBRATION, BRIDGING AND  
MERGING (CBAM), WHICH CALIBRATES THE DYNAMICAL MODEL FORECASTS USING BAYESIAN  
JOINT PROBABILITY (BJP) MODELS, AS WELL AS GENERATING STATISTICAL OR BRIDGING  
BJP MODELS OF TEMPERATURE AND PRECIPITATION FROM DYNAMICAL MODEL NINO 3.4  
ANOMALY FORECAST PREDICTORS. AN ENSO-OCN FORECAST TOOL IS USED TO REPRESENT THE  
COMBINED INFLUENCE OF THE EL NINO SOUTHERN OSCILLATION (ENSO) AND DECADAL  
TIMESCALE TRENDS IN TEMPERATURE AND PRECIPITATION, BASED ON THE OPTIMUM CLIMATE  
NORMAL (OCN). IMPACTS OF A PREDICTED MODERATE EL NINO MAY INFLUENCE THE  
TEMPERATURE AND PRECIPITATION PATTERNS IN THE SUMMER SEASONS FOR SOME REGIONS.  
HOWEVER, THE IMPACTS OF EL NINO ON THE CLIMATE OF NORTH AMERICA IS WEAKER IN  
SUMMER THAN AUTUMN AND ESPECIALLY WINTER SEASONS. THE SPATIAL PATTERNS OF  
TEMPERATURE AND PRECIPITATION ARE INDICATIVE OF A STRONG EL NINO EVENT FROM  
AUTUMN THROUGH WINTER AND THE JANUARY-FEBRUARY-MARCH (JFM) 2026 SEASON. DECADAL  
VARIABILITY IN TEMPERATURE AND PRECIPITATION ARE GENERALLY THE LARGEST  
PREDICTABLE SIGNAL FOR THE SEASONAL FORECASTS, FOLLOWING DIMINISHING IMPACTS OF  
EL NINO IN THE SPRING OF 2027. DECADAL VARIABILITY AND TRENDS ARE DETERMINED  
FROM THE OCN, CALCULATED FROM THE DIFFERENCE BETWEEN THE MOST RECENT 15-YEAR  
PERIOD AVERAGE SEASONAL TEMPERATURE OR PRECIPITATION AND THE AVERAGE FOR THE  
CLIMATOLOGY PERIOD FROM 1991-2020. CONSOLIDATIONS OF MULTIPLE STATISTICAL TOOLS  
AND WHEN AVAILABLE DYNAMICAL FORECAST TOOLS THAT UTILIZE PAC CALIBRATION ARE  
USED THROUGHOUT THE OUTLOOKS FROM JAS 2026 TO JAS 2027.  
 
PROGNOSTIC DISCUSSION OF OUTLOOKS - JAS 2026 TO JAS 2027  
 
TEMPERATURE  
 
THE JAS 2026 TEMPERATURE OUTLOOK FAVORS ABOVE NORMAL TEMPERATURES FOR MUCH OF  
ALASKA, EXCLUDING ONLY PARTS OF THE NORTHEASTERN MAINLAND, CONSISTENT WITH NMME  
DYNAMICAL MODEL FORECASTS, CBAM, AND THE CONSOLIDATION. THIS TEMPERATURE  
PATTERN IS ALSO CONSISTENT WITH POTENTIAL IMPACTS OF EL NINO. ABOVE NORMAL  
TEMPERATURES ARE FAVORED FOR MOST OF THE CONUS STARTING IN JAS 2026, TO SOME  
EXTENT INFLUENCED BY DECADAL TEMPERATURE TRENDS, WITH VARIATIONS MOSTLY  
ATTRIBUTABLE TO EL NINO IMPACTS. ABOVE NORMAL TEMPERATURES ARE LIKELY FOR THE  
NORTHWESTERN CONUS WITH PROBABILITIES EXCEEDING 60 PERCENT ACROSS THE PACIFIC  
NORTHWEST, WHERE THERE IS CONSISTENCY AMONG FORECAST TOOLS. ABOVE NORMAL  
TEMPERATURES ARE ALSO SUPPORTED IN THIS REGION BY POTENTIAL EL NINO IMPACTS AND  
NEGATIVE CORRELATIONS BETWEEN SUMMER SEASONAL TEMPERATURES AND PRECIPITATION.  
ABOVE NORMAL TEMPERATURES ARE FAVORED WITH WEAKER PROBABILITIES ACROSS THE  
SOUTHERN TIER OF THE CONUS SUPPORTED BY CALIBRATED DYNAMICAL MODEL FORECASTS,  
AS WELL AS THE ENSO-OCN STATISTICAL FORECAST. GREATER PROBABILITIES FAVORING  
ABOVE NORMAL TEMPERATURES OVER THE EASTERN SEABOARD ARE SUPPORTED BY DYNAMICAL  
AND STATISTICAL TOOLS, AND CONSISTENT WITH THE OCN REPRESENTATION OF DECADAL  
TRENDS. EQUAL CHANCES (EC) OF BELOW, NEAR AND ABOVE NORMAL TEMPERATURES ARE  
INDICATED FOR MUCH OF THE NORTHERN CENTRAL CONUS, THE CENTRAL MISSISSIPPI AND  
OHIO VALLEYS, AND THE GREAT LAKES REGION, WITH BELOW NORMAL TEMPERATURES  
SLIGHTLY FAVORED FOR PARTS OF THE CENTRAL MISSISSIPPI VALLEY. THE INCREASED  
PROBABILITY OF BELOW NORMAL TEMPERATURES IS RELATED TO POTENTIAL IMPACTS OF A  
DEVELOPING EL NINO, USING THE CBAM BRIDGING OF DYNAMICAL MODEL FORECASTS OF  
NINO 3.4 ANOMALIES.  
 
THE TEMPERATURE PATTERN OF THE SEASONAL OUTLOOK CONTINUES THROUGH  
AUGUST-SEPTEMBER-OCTOBER (ASO) BEFORE BEING MODIFIED BY CHANGING IMPACTS OF A  
PREDICTED STRONG EL NINO. THE TEMPERATURE OUTLOOKS FOR THE OND 2026 THROUGH JFM  
2027 SEASONS FAVOR ABOVE NORMAL TEMPERATURES ACROSS ALASKA, MOST OF THE WEST,  
AND THE NORTHERN TIER OF THE CONUS, SUPPORTED BY CALIBRATED DYNAMICAL MODELS  
AND STATISTICAL REPRESENTATIONS OF THE TYPICAL IMPACTS OF EL NINO. EC IS  
INDICATED ACROSS MOST OF THE SOUTHERN TIER OF THE CONUS IN THESE SEASONS, WHERE  
EL NINO IMPACTS INCREASE THE PROBABILITY OF NEAR TO BELOW NORMAL TEMPERATURES.  
SEASONAL TEMPERATURE PATTERNS IN THE OUTLOOKS FOR THE SPRING AND SUMMER SEASONS  
OF 2027 ARE PRIMARILY RELATED TO DECADAL TRENDS.  
 
PRECIPITATION  
 
THE JAS 2026 PRECIPITATION OUTLOOK FAVORS ABOVE NORMAL PRECIPITATION FOR  
WESTERN MAINLAND ALASKA AND THE ALEUTIANS, WHILE BELOW NORMAL PRECIPITATION IS  
FAVORED FOR A SMALL AREA IN SOUTHERN SOUTHEAST ALASKA, SUPPORTED BY DYNAMICAL  
MODEL TOOLS, AS WELL AS THE ENSO-OCN FORECAST. IN THE NEXT SEVERAL SEASONS  
THROUGH OND 2026, THE AREA OF FAVORED ABOVE NORMAL PRECIPITATION EXPANDS  
EASTWARD ACROSS MAINLAND ALASKA, WHILE THE AREA OF FAVORED BELOW NORMAL  
PRECIPITATION IN SOUTHEAST ALASKA DECREASES AND IS REPLACED BY EC. BELOW NORMAL  
PRECIPITATION IS FAVORED IN WESTERN WASHINGTON STATE IN JAS 2026, SUPPORTED BY  
DYNAMICAL MODEL FORECASTS. IN THE FOLLOWING SEASONS, THE AREA OF FAVORED BELOW  
NORMAL PRECIPITATION EXPANDS ACROSS MUCH OF THE NORTHWEST AND EASTWARD INTO  
NORTHERN PLAINS BY THE WINTER MONTHS, CONSISTENT WITH CANONICAL EL NINO  
IMPACTS. BEGINNING IN DECEMBER-JANUARY-FEBRUARY (DJF) 2026-27, THE AREA OF  
FAVORED BELOW NORMAL PRECIPITATION PERSISTS ONLY FROM THE NORTHERN ROCKIES  
EASTWARD, BEFORE REDUCING IN EXTENT AND RETURNING TO COVER THE NORTHWESTERN  
CONUS, CONSISTENT WITH THE EVOLUTION FROM EL NINO IMPACTS TO DECADAL TRENDS.  
ABOVE NORMAL PRECIPITATION IS FAVORED FOR A LARGE AREA OF THE WESTERN CONUS,  
FROM SOUTHERN CALIFORNIA AND THE DESERT SOUTHWEST INTO THE GREAT BASIN AND THE  
CENTRAL ROCKIES, CONSISTENT WITH NMME AND C3S FORECASTS, AS WELL AS ANOMALOUSLY  
WARM EASTERN PACIFIC SSTS AND A POTENTIAL INCREASE IN TROPICAL STORMS. THIS  
AREA OF FAVORED ABOVE NORMAL PRECIPITATION EXPANDS EASTWARD IN THE NEXT SEVERAL  
SEASONS, AS THE PRECIPITATION PATTERN EVOLVES TO A CANONICAL EL NINO PATTERN.  
ABOVE NORMAL PRECIPITATION IS FAVORED ACROSS MUCH OF THE SOUTHERN TIER OF THE  
CONUS IN OND 2026 THROUGH MARCH-APRIL-MAY (MAM) 2027. PROBABILITIES FAVORING  
ABOVE NORMAL PRECIPITATION EXCEED 60 PERCENT FOR PARTS OF THE SOUTHEAST IN NDJ  
2026 THROUGH JFM 2027, WHERE CORRELATIONS OF SEASONAL PRECIPITATION TO ENSO  
INDICES ARE GREATEST. BELOW NORMAL PRECIPITATION IS FAVORED FOR PARTS OF THE  
MIDWEST IN DJF 2026-27 THROUGH MAM 2027, RELATED TO EL NINO IMPACTS. FAVORED  
ABOVE NORMAL PRECIPITATION ALONG THE SOUTH COAST OF MAINLAND ALASKA IN THE  
WINTER SEASONS ARE CONSISTENT WITH EL NINO IMPACTS.  
 
FORECASTER: DAN COLLINS  
 
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 JUL 16 2026  
 
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