PROGNOSTIC DISCUSSION FOR MONTHLY OUTLOOK NWS CLIMATE PREDICTION CENTER COLLEGE PARK MD 830 AM EST THU DEC 15 2016 30-DAY OUTLOOK DISCUSSION FOR JANUARY 2017 THE JANUARY 2017 TEMPERATURE AND PRECIPITATION OUTLOOKS ARE BASED ON DYNAMICAL MODEL OUTPUTS, STATISTICAL TOOLS, TYPICAL PATTERNS ASSOCIATED WITH TROPICAL SST VARIABILITY, AND THE LIKELY STATES OF PATTERNS OF EXTRATROPICAL VARIABILITY. LA NINA CONDITIONS CONTINUE OVER THE TROPICAL PACIFIC, AND ARE EXPECTED TO CONTINUE THROUGH JANUARY 2017, THOUGH IMPACTS ON THE MONTHLY TIMESCALE FROM ENSO ARE LESS ROBUST THAN SEASONAL IMPACTS. CLIMATE SIGNALS ASSOCIATED WITH LA NINA ARE CONSIDERED AS A PORTION OF THE OUTLOOK. THE MJO IS NOT CURRENTLY ACTIVE, AND THE UNCERTAINTY FOR INTRASEASONAL VARIABILITY IS HIGH, SO THE MJO DID NOT PLAY A ROLE IN THE OUTLOOK. ITS EVOLUTION WILL BE CLOSELY MONITORED FOR THE REVISED OUTLOOK AT THE END OF DECEMBER. THE DYNAMICAL MODEL OUTLOOKS FOR JANUARY 2017 EXHIBITED GOOD AGREEMENT, WHERE AS LAST MONTH THE OUTLOOKS FOR DECEMBER HAD BETTER AGREEMENT, SO THE CONFIDENCE IN THE OUTLOOK IS SLIGHTLY LOWER, RESULTING IN LOW TO MODERATE COVERAGE. LA NINA CONDITIONS WOULD FAVOR ABOVE NORMAL TEMPERATURES OVER THE SOUTHERN CONUS WITH BELOW NORMAL TEMPERATURES OVER MUCH OF THE NORTHERN CONUS. THE SPATIAL COVERAGE OF WHERE BELOW NORMAL TEMPERATURES ARE FAVORED OVER THE NORTHERN ROCKIES AND NORTHERN GREAT PLAINS IS SMALLER THAN A TYPICAL SEASONAL FOOTPRINT OF LA NINA, DUE TO LOWER PREDICTABILITY AND DYNAMICAL MODEL GUIDANCE. SOME STATISTICAL TOOLS FAVOR BELOW NORMAL TEMPERATURES EXTENDING INTO NORTHERN COLORADO. SOME DYNAMICAL MODELS INDICATE A SLIGHT TILT TOWARD A NEGATIVE ARCTIC OSCILLATION THROUGHOUT THE WINTER, WHICH FAVORS PERIODS OF COLDER AIR MOVING SOUTHWARD OVER THE GREAT PLAINS, SO PROBABILITIES FOR ABOVE NORMAL TEMPERATURES ARE LOWER THAN INDICATED IN MODEL GUIDANCE OVER THE GREAT PLAINS AND MID-ATLANTIC. ABOVE NORMAL SSTS FAVOR ABOVE NORMAL TEMPERATURES FOR WESTERN ALASKA AND THE ALEUTIANS. THE PRECIPITATION OUTLOOK FOR JANUARY 2017 REFLECTS CALIBRATED NMME OUTPUT AND IS CONSISTENT WITH TRADITIONAL LA NINA IMPACTS DURING DJF AND JFM. COVERAGE AND PROBABILITIES FOR THE CATEGORIES ARE LOWER THAN IF LA NINA WAS THE ONLY FACTOR, AS SIGNALS IN THE DYNAMICAL MODELS ARE WEAKER, AND LA NINA IMPACTS ON A SINGLE MONTH OF A SEASON ARE LESS PRONOUNCED THAN IMPACTS ON AN ENTIRE SEASON. BELOW MEDIAN PRECIPITATION IS FAVORED FOR THE SOUTHERN CONUS, WITH ABOVE MEDIAN PRECIPITATION FAVORED ALONG THE ROCKIES AND OVER THE GREAT LAKES REGION, WITH A MORE ACTIVE NORTHERN STORM TRACK. ABOVE NORMAL SSTS, BELOW NORMAL SEA ICE COVERAGE IN THE BERING SEA, AND MODEL GUIDANCE FAVOR ABOVE MEDIAN PRECIPITATION FOR WESTERN ALASKA. FORECASTER: MATTHEW ROSENCRANS THE CLIMATIC NORMALS ARE BASED ON CONDITIONS BETWEEN 1981 AND 2010, 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 JAN WILL BE ISSUED ON SAT DECEMBER 31 2016 THESE OUTLOOKS ARE BASED ON DEPARTURES FROM THE 1981-2010 BASE PERIOD. $$