NOCN03 CWAO 091830 GENOT NO. 014 GENOT NO. 013 EST LA VERSION FRANCAISE DE CE GENOT. ON TUESDAY DECEMBER 13, 2005, AT 12 UTC (EXACT TIME TO BE CONFIRMED), THE CANADIAN METEOROLOGICAL CENTRE WILL IMPLEMENT A MAJOR CHANGE TO THE ENSEMBLE PREDICTION SYSTEM (EPS). SOME NEW TYPES OF OBSERVATIONS WILL START BEING USED BY THE ENSEMBLE KALMAN FILTER (ENKF) DATA-ASSIMILATION SYSTEM WHICH ITSELF WILL ALSO BENEFIT FROM SOME STRUCTURAL IMPROVEMENTS. THE ENSEMBLE OF FORECAST MODELS HAS BEEN REVISED TO ARRIVE AT A BETTER SIMULATION OF THE DIURNAL CYCLE AND TO HAVE A REDUCTION IN MODEL BIASES. THE FORECASTS WILL BE PERFORMED TWICE DAILY AND THE FORECAST PERIOD WILL BE EXTENDED FROM 10 DAYS TO 16 DAYS. MOTIVATION THE REGULAR ADDITION OF NEW TYPES OF OBSERVATIONS IS NECESSARY IN ORDER TO MAINTAIN A STABLE ANALYSIS QUALITY AS OLD SATELLITE-BASED OBSERVING PLATFORMS ARE BEING REPLACED BY NEW ONES. IN ADDITION, CHANGES TO THE ANALYSIS ALGORITHM ARE NEEDED IN PREPARATION TO AN UPCOMING ASSIMILATION OF OBSERVATIONS AT THE PROPER TIME (AS OPPOSED TO ASSUMING THAT ALL OBSERVATIONS ARE VALID AT SYNOPTIC TIMES). THE MODEL CHANGES HAVE BEEN MOTIVATED BY THE ESTABLISHMENT OF THE NORTH AMERICAN ENSEMBLE FORECAST SYSTEM (NAEFS) IN WHICH THE CANADIAN AND AMERICAN MEDIUM-RANGE ENSEMBLES WILL BE COMBINED INTO A LARGER 'NORTH AMERICAN' ENSEMBLE. TO PARTICIPATE IN THE NAEFS, WHICH WILL FEATURE FORECAST PRODUCTS FOR WEEK TWO, WE MUST EXTEND THE FORECAST RANGE TO 16 DAYS AS WELL AS REDUCE FORECAST BIASES IN ORDER TO MAINTAIN AN ACCEPTABLE QUALITY IN THE SECOND WEEK. ASSIMILATION IN THE ENKF, THE FOLLOWING TYPES OF OBSERVATIONS WILL BE ADDED: - MODIS WINDS FROM THE AQUA AND TERRA SATELLITES IN THE POLAR REGIONS, - AMSU-A RADIANCES FROM THE AQUA SATELLITE, - DEWPOINT DEPRESSION AT THE SURFACE. TO ARRIVE AT A BETTER BALANCE IN THE TRIAL FIELDS, A FEW CHANGES WILL BE MADE TO THE ENKF ALGORITHM. FIRST, THE PARAMETERIZED ERROR FIELDS, WHICH ARE NOW ADDED TO THE 6H FORECASTS, WILL BE ADDED TO THE ANALYSIS. CONSEQUENTLY, THESE PERTURBATIONS WILL EVOLVE FOR 6 HOURS WITH THE MODEL DYNAMICS BEFORE THEY ARE USED IN THE ANALYSIS. THE MODEL WILL THUS FILTER SOME OF THE UNBALANCED COMPONENTS THAT ARE PRESENT IN THE PARAMETERIZED ERROR FIELDS. IN PREPARATION FOR A FUTURE IMPLEMENTATION OF TIME INTERPOLATION IN THE ENKF, A DIGITAL FILTER INITIALISATION HAS BEEN INTRODUCED. THIS FURTHER REDUCES THE IMBALANCE IN THE ENSEMBLE OF 6H FORECASTS THAT IS USED TO DETERMINE THE DIRECTIONS IN WHICH ANALYSIS INCREMENTS ARE REQUIRED. FINALLY, THE 96 ENSEMBLE MEMBERS ARE NOW SPLIT INTO TWO SUB-ENSEMBLES OF 48 MEMBERS. THIS WAS SET UP SO THAT THE MEMBERS OF EACH SUB-ENSEMBLE COULD BE ASSIMILATED USING THE INDEPENDENT STATISTICS OF THE 48 MEMBERS FROM THE OTHER SUB-ENSEMBLE. A CONFIGURATION WITH FOUR 24 MEMBER SUB-ENSEMBLES WILL BE USED, PERMITTING STATISTICS TO BE COMPUTED FROM 72 INDEPENDENT MEMBERS. FORECAST: THE MEDIUM-RANGE ENSEMBLE FORECASTS WILL NOW BE RUN TWICE A DAY WITH THE FORECASTS EXTENDING UNTIL DAY 16. THE CONFIGURATIONS OF THE SEF AND GEM SUB-ENSEMBLES HAVE BEEN REVISED TO HAVE LESS BIAS IN THE SECOND FORECAST WEEK. TO FACILITATE THE MAINTENANCE AND TO IMPROVE THE QUALITY OF THE EPS, UPDATED PHYSICAL PARAMETERIZATIONS WILL BE USED FOR BOTH THE SEF AND THE GEM SUB-ENSEMBLES. NOTEWORTHY IS THE USE OF THE ISBA (INTERACTIONS SURFACE BIOSPHERE AND ATMOSPHERE) ALGORITHM FOR HALF OF THE ENSEMBLE MEMBERS. THE USE OF THIS ALGORITHM SIGNIFICANTLY IMPROVES THE RELIABILITY AND RESOLUTION OF THE SURFACE TEMPERATURE FORECASTS. SUMMARY OF THE OBJECTIVE EVALUATIONS EXTENSIVE TESTING OF THE NEW EPS, IN BOTH SUMMER AND WINTER CONDITIONS, WAS PERFORMED BY THE R&D TEAM PRIOR TO THE IMPLEMENTATION OF A PARALLEL RUN STARTING ON SEPTEMBER 2ND, 2005, ALLOWING ADDITIONAL VERIFICATION OF DIFFERENCES BETWEEN THE OPERATIONAL EPS AND THE NEW ONE. OBJECTIVE VERIFICATIONS OF AVERAGE 6-HOUR ENSEMBLE FORECASTS AGAINST UPPER AIR SOUNDING OBSERVATIONS FOR WIND SHOWED A STATISTICALLY SIGNIFICANT IMPROVEMENT TO THE RMS ERROR FOR ALL FORECAST PERIODS,. FOR GEOPOTENTIAL HEIGHT, TEMPERATURE AND DEW POINT DEPRESSION THE IMPROVEMENTS WERE FAIRLY MINOR. IT MUST BE NOTED, HOWEVER, THAT THE IMPROVEMENTS WERE RELATIVELY BIGGER DURING THE PARALLEL RUN AND CLEARLY SIGNIFICANT FOR ALL VARIABLES. COMPARISON OF THE OPERATIONAL AND THE NEW MEDIUM-RANGE ENSEMBLE PREDICTIONS SHOWS A SIGNIFICANT REDUCTION IN THE BIASES FOR TEMPERATURE AND GEOPOTENTIAL HEIGHT FOR ALL FORECAST PERIODS AND ALL REGIONS EXCEPT FOR THE ANTARCTIC CONTINENT. FOR SURFACE TEMPERATURE, THE NEW FORECAST ENSEMBLE, WHICH BENEFITS FROM THE ISBA PARAMETERIZATION, BETTER MODELS THE DIURNAL CYCLE. THIS RESULTS IN MORE RELIABLE AND MORE PRECISE TEMPERATURE FORECASTS. SIGNIFICANT IMPROVEMENTS IN BRIER SCORE WERE NOTICED FOR THE PRECIPITATION. THIS IS DUE TO AN IMPROVED, BUT STILL POOR, RELIABILITY IN THE PREDICTION OF SMALL PRECIPITATION AMOUNTS. SUMMARY OF THE SUBJECTIVE EVALUATIONS THE METEOROLOGISTS OF THE OPERATIONAL ANALYSIS AND PROGNOSIS DIVISION EVALUATED SUBJECTIVELY THE PARALLEL ENSEMBLE FORECAST SYSTEM DURING 65 DAYS. THE GEOPOTENTIAL HEIGHT AT 500 HPA, MEAN SEA LEVEL PRESSURE, AND THE QUANTITATIVE PRECIPITATION FORECAST (QPF) FIELDS WERE EVALUATED AT FORECAST TIMES OF 48, 72, 96 AND 120 HOURS. THESE FIELDS WERE EVALUATED ACROSS FOUR REGIONS: ARCTIC, WEST COAST, CENTER, AND EAST. QPF WAS NOT EVALUATED ACROSS THE ARCTIC DUE TO LACK OF DATA. OVERALL THE EVALUATION INDICATED A SLIGHT ADVANTAGE IN FAVOR OF THE NEW SYSTEM. THIS ADVANTAGE WAS MORE PRONOUNCED FOR THE 500MB GEOPOTENTIAL FIELD, ESPECIALLY IN THE EAST BUT ALSO IN THE ARCTIC. IN SPITE OF THE APPARENT OVERALL NEUTRALITY OF THE SIGNAL, SIGNIFICANT DIFFERENCES EVEN IN THE 48 HOUR FORECASTS WERE REGULARLY NOTED BOTH AT THE SURFACE AND ALOFT. FOR THE PRECIPITATION FORECAST THE OPERATIONAL SYSTEM WAS PREFERRED MORE FREQUENTLY THAN THE PARALLEL SYSTEM, ESPECIALLY ALONG THE WEST COAST. THE LIGHTER AMOUNTS OF PRECIPITATION FORECASTED BY THE NEW SYSTEM ALONG THE COASTAL MOUNTAINS WERE GENERALLY JUDGED NOT AS ACCURATE AS IN THE OPERATIONAL SYSTEM. HOWEVER THE HIGHER AMOUNTS FORECASTED IN THE OPERATIONAL SYSTEM WERE PRODUCED BY THE BIASED MANABE SCHEME. WE NOTED THAT THE INTRODUCTION OF THE ISBA SURFACE SCHEME IN 8 OF THE PARALLEL MEMBERS PRODUCED A DIURNAL VARIATION OF SURFACE TEMPERATURES WHICH WAS MORE REALISTIC AND ALSO RESULTED IN A BETTER VERIFICATION OF EXTREME TEMPERATURES OVER THE CONTINENT (COLD ZONES OVER THE CONTINENT IN PARTICULAR). A MORE REALISTIC REPRESENTATION OF BAROCLINIC ZONE TEMPERATURE GRADIENTS WAS SEEN, ESPECIALLY IN SITUATIONS WHERE WE HAD STRONG TEMPERATURE ADVECTION. IMPACTS THE SUITE OF PRODUCTS WILL NOT BE CHANGED IMMEDIATELY, BUT DURING THE WINTER. USERS OF ENSEMBLE DATA WILL NOTICE DELAYS IN THE AVAILABILITY OF 00Z PRODUCTS AFTER THE IMPLEMENTATION OF THE NEW SYSTEM IN OPERATIONS. THE SEF AND GEM MEMBERS RUN FOR ABOUT 15-30 MINUTES LONGER IN THE ENSEMBLE PARALLEL RUN. AS WELL, NCEP POST PROCESSING JOBS TAKE AN ADDITIONAL 10-20 MINUTES TO RUN. ENSEMBLE COLOR IMAGES SPAGHETTI PLOTS WILL BE AVAILABLE 20-30 MINUTES LATER WHILE NAEFS GRIB DATA WILL LIKELY BE AVAILABLE 30-50 MINUTES LATER. THE 12Z PRODUCTION RUN IS A PURE ADDITION. THE 12Z SUITE OF PRODUCTS, THE EXTENDED FORECASTS PAST DAY 10, AS WELL AS A SERIES OF NEW PRODUCTS, WILL BE MADE AVAILABLE ON THE WEB LATER THIS WINTER. EVERELL / ADMA / SMA-SMC TORONTO