PROGNOSTIC DISCUSSIONS FOR 6 TO 10 AND 8 TO 14 DAY OUTLOOKS NWS CLIMATE PREDICTION CENTER CAMP SPRINGS MD 300 PM EST WED DEC 24 2003 6 TO 10 DAY OUTLOOK FOR DEC 30 2003 - JAN 3 2004 . . . . . . . . THE MODELS ARE IN FAIRLY GOOD AGREEMENT ON DAILY 500-HPA HEIGHT FORECASTS OUT THROUGH DAY 5... WITH THE EXPECTED INCREASE IN UNCERTAINTY IN DETAILS OF THE SHORT WAVES WHICH BECOME NOTICEABLE BY DAY 4 AND GROW THROUGH DAY 5 BUT DO NOT SERIOUSLY IMPACT THE LONG WAVE PATTERN. THE RIDGE INITIALLY OVER THE PLAINS PROGRESSES TO THE EAST COAST BY DAY 5 AND A STRONG MEAN TROUGH MOVES INTO THE WESTERN U.S. FROM THE PACIFIC... WITH MULTIPLE SHORT WAVES ROTATING THROUGH IT. THE DIFFERENCES IN LOCATION OF THE STRONGEST SHORT WAVES ON DAY 5 CARRY OVER INTO THE 6-10 DAY MEANS AS TO THE LOCATION OF THE NEGATIVE ANOMALY CENTER ASSOCIATED WITH THE WESTERN MEAN TROUGH. DURING THE 6-10 DAY PERIOD THE MODELS CONTINUE TO HAVE GENERALLY GOOD AGREEMENT ON THE FORECAST LARGE-SCALE FEATURES OF THE LONG-WAVE PATTERN... WHICH CONSISTS OF A STRONG POSITIVE ANOMALY OVER NORTHEAST CANADA WITH SPLIT FLOW AND A TROUGH AND NEGATIVE ANOMALY CENTER SOUTH OF NOVA SCOTIA OVER THE WESTERN ATLANTIC. THERE IS A SUBTLE INCREASE IN UNCERTAINTY DUE TO INCREASING DIFFERENCES IN THE LOCATIONS OF THE STRONGEST POSTIVE HEIGHT ANOMALIES... WITH SOME MODELS (MOSTLY THE GFS RUNS) BUILDING THE RIDGE OVER THE GULF OF ALASKA THE MOST... WHILE THE ECMWF AND DAVA MAINTAIN MORE OF THE ORIGINAL POSITIVE ANOMALY OVER NORTHEASTERN CANADA AND BUILD A STRONG BLOCK OVER THE ARCTIC OCEAN NORTHWEST OF THE CANADIAN ARCHIPELAGO. TELECONNECTIONS FROM EITHER THE GULF OF ALAKSA POSITIVE HEIGHT ANOMALY CENTER OR THE NEGATIVE ANOMALY CENTER NEAR THE PACIFIC NORTHWEST COAST FAVOR A STRONG RIDGE OVER THE SOUTHEASTERN U.S. THE ECMWF MODEL... WHICH IS SOMEWHAT OF AN OUTLIER TODAY... COMES CLOSEST TO DEPICTING THIS TYPE OF PATTERN... ALTHOUGH THE BLOCK OVER EASTERN CANADA AND THE NORTHWESTERN ATLANTIC TELECONNECTS WELL WITH ONLY THE NEGATIVE ANOMALY TO ITS SOUTH OVER THE WESTERN ATLANTIC. FOR THIS REASON THE ECMWF MODEL WAS GIVEN A HIGHER WEIGHT THAN USUAL IN THE BLEND. MODEL OF THE DAY: GFS ENSEMBLE MEAN AND ECMWF (TIED) THE OFFICIAL HEIGHT PROG FOR TODAY CONSISTS OF 25 PERCENT OF TODAYS GFS ENSEMBLE MEAN CENTERED ON DAY 8... 25 PERCENT OF THE HIGH RESOLUTION ECMWF CENTERED ON DAY 7... 10 PERCENT ON EACH OF THE MOST RECENT FOUR (INITIALIZED AT 12Z AND 18Z YESTERDAY AND 00Z AND 06Z TODAY) OPERATIONAL GFS RUNS CENTERED ON DAY 8... AND 10 PERCENT OF THE DAVA CENTERED ON DAY 8. FORECAST CONFIDENCE FOR THE 6 TO 10 DAY PERIOD HAS DECLINED TO AVERAGE TODAY ... 3 ON A SCALE FROM 1 TO 5 FOR THE REASONS DISCUSSED ABOVE. THERE IS A CORRESPONDING DECREASE IN THE AGREEMENT AMONG THE ANALOG TEMPERATURE AND PRECIPITATION SPECIFICATIONS BASED ON THE VARIOUS MODELS. THE D+8 TEMPERATURE PROG IS BASED ON KLEIN AND NEURAL NET SPECIFICATIONS FROM THE OFFICIAL HEIGHT BLEND CHART... ANALOGS TO THE BLENDED HEIGHT FIELD AND THE INDIVIDUAL MODELS... AND THE BIAS CORRECTED 850-HPA TEMPERATURES FROM THE 00Z OPERATIONAL GFS. THE MOS TEMPERATURE FORECAST FROM THE GFS ENSEMBLE WAS AVAILABLE... BUT WAS NOT WEIGHTED MUCH INTO THE TEMPERATURE FORECAST BECAUSE IT APPEARED TO BE TOO WARM IN MANY PLACES... ESPECIALLY THE FAR WEST. THE D+8 PRECIPITATION PROG IS BASED ON GFS ENSEMBLE CALIBRATED PRECIPITATION PERCENTAGES... ANALOGS TO THE BLENDED HEIGHT FIELD... THE NEURAL NET SPECIFI- CATIONS FROM THE OFFICIAL HEIGHT BLEND... THE CALIBRATED PRECIPITATION FROM THE 0Z OPERATIONAL GFS AND THE BIAS CORRECTED PRECIPITATION FROM THE 0Z OPERA- TIONAL GFS. . . . . . . . . 8 TO 14 DAY OUTLOOK FOR JAN 1 - JAN 7 2004 THE CIRCULATION PATTERNS PREDICTED BY THE VARIOUS MODELS DIVERGE A BIT MORE TODAY BUT ALL ARE FORECASTING A GENERALLY COLD PATTERN FOR MOST OF THE CONUS... ESPECIALLY THE GREAT PLAINS REGION. AT THE SAME TIME THE BLOCK OVER NORTHEAST- ERN CANADA IS PREDICTED TO WEAKEN ALTHOUGH THERE IS MUCH DISAGREEMENT AMONG THE MODELS AS TO HOW FAST THIS WILL HAPPEN. IN ANY CASE A MAJOR ARCTIC AIRMASS WILL BE BUILDING OVER NORTHWESTERN CANADA AND WILL LIKELY BEGIN TO AFFECT THE CONUS SOMETIME DURING THE WEEK TWO PERIOD. THERE IS A TREND FOR THE RIDGE OVER THE GULF OF ALASKA TO STRENGTHEN FURTHER AND BEGIN TO RETROGRADE TOWARDS THE BERING STRAITS... AS SEEN MOST STRONGLY IN SOME THE THE INDIVIDUAL GFS OPAERATIONAL RUNS. THE BLOCK OVER THE ARCTIC IS INDICATED BY MOST OF THE MODELS... BUT THERE IS ALSO A LOT OF UNCERTAINTY AS TO HOW STRONG IT WILL BE AND THUS ITS POSSIBLE INFLUENCE ON TEMPERATURES OVER THE CONUS IS UNCERTAIN. THE OFFICIAL 500-HPA HEIGHT PROG FOR TODAY CONSISTS OF 20 PERCENT OF TODAYS GFS ENSEMBLE MEAN CENTERED ON DAY 11... 10 PERCENT OF EACH OF THE MOST RECENT FOUR GFS OPERATIONAL RUNS CENTERED ON DAY 11... 15 PERCENT OF TODAYS 5-DAY MEAN ECMWF CENTERED ON DAY 7... 15 PERCENT OF THE 06Z OPERATIONAL GFS RUN... AND 10 PERCENT OF THE 12Z OPERATIONAL GFS RUN. THE LATTER THREE MODEL MEANS WERE INCLUDED IN ORDER TO RAISE HEIGHTS SOMEWHAT OVER THE SOUTHEASTERN U.S. MORE IN ACCORD WITH THE MODAL TELECONNECTIONS FROM THE PACIFIC POSITIVE AND WEST COAST NEGATIVE ANOMALY CENTERS. FORECAST CONFIDENCE FOR THE 8 TO 14 DAY PERIOD IS ABOUT AVERAGE TODAY... RATED A 3 ON A SCALE FROM 1 TO 5... DUE TO THE FAIRLY GOOD AGREEMENT AMONG THE MODELS OFFSET SOMEWHAT BY RATHER LARGE SPREAD IN THE GFS ENSEMBLE MEMBERS... AND UNCERTAINTIES IN WHICH OF THE RIDGES WILL BE THE STRONGEST. THE D+11 TEMPERATURE PROG IS BASED ON THE KLEIN AND NEURAL NET SPECIFICATIONS TO THE BLEND... ANALOGS TO THE GFS ENSEMBLE MEAN AND 06Z GFS HEIGHT FIELDS... AND THE 850-HPA BIAS CORRECTED TEMPERATURES FROM THE 00Z OPERATIONAL GFS. THE D+11 PRECIPITATION PROG IS BASED ON THE GFS ENSEMBLE CALIBRATED PRECIPITATION PERCENTAGES... NEURAL NET SPECIFICATIONS TO THE BLEND... ANALOGSTO THE OFFICIAL FORECAST AND THE VARIOUS MODELS FOR THE WEEK TWO PERIOD... AND THE BIAS CORRECTED PRECIPITATION FROM THE 00Z OPERATIONAL GFS. FORECASTER: A. J. WAGNER . . . . . . . NOTES: AUTOMATED FORECASTS ARE ISSUED ON SATURDAY AND SUNDAY. OTHERWISE - FORECASTS INCORPORATE FORECASTER INPUT. THE NOTATION FOR THE CATEGORICAL FORECAST INDICATED ON THE MAPS IS THE SAME AS THAT IN THE TABLES: A-ABOVE N-NEAR NORMAL B-BELOW IN THE SOUTHWEST AND OTHER CLIMATOLOGICALLY DRY REGIONS - THERE WILL BE A GREATER THAN 33.3% CHANCE OF NO PRECIPITATION AND OCCASIONALLY EVEN A NORMAL (I.E. MEDIAN) VALUE OF ZERO - ESPECIALLY DURING THE DRY SEASONS. IN SUCH CASES A FORECAST OF NEAR NORMAL IS EFFECTIVELY A FORECAST OF LITTLE OR NO PRECIPITATION. THE NARRATIVE DESCRIPTION OF THE FORECAST PATTERNS FOR TEMPERATURE AND PRECIPITATION FOR BOTH THE 6-10 OR 8-14 DAY PERIODS HAS BEEN DISCONTINUED. THE STATE TABLES FOR BOTH THE 6-10 AND 8-14 DAY PERIODS ARE NOW CONTAINED IN THIS MESSAGE...AVAILABLE AS PMDMRD ON AWIPS. . . . . . . . GLOSSARY AND DEFINITIONS:--------------------------------------------- AC - ANOMALY CORRELATION - A MEASURE OF HOW WELL A MODEL FORECASTS THE HEIGHT OR HEIGHT ANOMALY FIELD OBTAINED BY CORRELATING THE IMPLIED GRADIENTS OF THE TWO ANOMALY PATTERNS BEING COMPARED. ANALOG (NATURAL ANALOG) - A WEATHER MAP THAT RESEMBLES ANOTHER WEATHER MAP - USUALLY FROM DIFFERENT YEARS BUT THE SAME SEASON IN THE HISTORICAL RECORD. THE CRITERION FOR SELECTING AN ANALOG IS OFTEN THE PATTERN CORRELATION BETWEEN THE MAPS. TWO MAPS WILL JUST BEGIN TO RESEMBLE EACH OTHER TO THE HUMAN EYE AT A PATTERN CORRELATION OF ABOUT 40%. TO BE USEFUL - ANALOGS NEED TO HAVE MUCH HIGHER CORRELATIONS TO THE ORIGINAL MAP THAN THAT - 80% OR MORE. ANALOGS ARE INCREASINGLY DIFFICULT TO FIND AS THE GEOGRAPHIC REGION BEING STUDIED INCREASES IN SIZE. PERFECT ANALOGS TO THE ENTIRE NORTHERN HEMISPHERE SIMPLY DO NO EXIST - FOR PRACTICAL PURPOSES. THIS IS WHY SIMPLE NATURAL ANALOG FORECAST METHODS DO NOT WORK VERY WELL. ANOMALY - THE ARITHMETIC DIFFERENCE BETWEEN THE VALUE OF A VARIABLE AT A GIVEN PLACE AND TIME AND THE LONG-TERM AVERAGE OF THAT VARIABLE AT THAT PLACE AND TIME OF YEAR. AO - ARCTIC OSCILLATION - A MEASURE OF THE DIFFERENCE BETWEEN THE MEAN MID-TROPOSPHERIC HEIGHT OR SEA LEVEL PRESSURE ANOMALY OVER THE POLAR BASIN AND THE CORRESPONDING AVERAGE ANOMALY IN A RING SURROUNDING THE POLAR BASIN AT MIDDLE LATITUDES. THE AO IS CONSIDERED TO BE THE LEADING MODE OF CLIMATE VARIABILITY OF THE EXTRATROPICAL NORTHERN HEMISPHERE. THE AO CAN ALSO BE CONSIDERED TO INCLUDE THE NAO (NORTH ATLANTIC OSCILLATION) WITH WHICH IT IS POSITIVELY CORRELATED - BUT NOT IDENTICAL. THE PHASE OF THE AO IS CONSIDERED TO BE POSITIVE WHEN HEIGHTS OR PRESSURES ARE BELOW NORMAL OVER THE ARCTIC BASIN AND ABOVE NORMAL OVER SURROUNDING MID- LATITUDES - AND IS NEGATIVE FOR THE REVERSE ANOMALY PATTERN. BLEND - A WEIGHTED AVERAGE OF 500-HPA HEIGHT FORECAST MAPS FROM SEVERAL MODELS. WEIGHTS ARE CURRENTLY ASSIGNED SUBJECTIVELY BY THE FORECASTER. THE SUM OF THE WEIGHTS MUST BE 1. WEIGHTS ARE APPLIED BY MULTIPLYING EACH 500-HPA MAP BY ITS WEIGHT AND ADDING ALL OF THE WEIGHTED MAPS TOGETHER TO MAKE THE OFFICIAL 500-HPA FORECAST. CONUS - CONTERMINOUS UNITED STATES. DAVA - DIVERGENT ANOMALY VORTICITY ADVECTION MODEL. THIS IS A BAROTROPIC MODEL WITH DIVERGENCE IN IT TO ALLOW MORE ACCURATE PREDICTION OF LONG WAVES THAN A STANDARD BAROTROPIC MODEL. REFERENCE: QIN J. AND H.M. VAN DEN DOOL - 1996: SIMPLE EXTENSIONS OF AN NWP MODEL. MON. WEA. REV. - VOL 124 - PP 277-287. EL NINO - THE WARM PHASE OF ENSO. ENSO - EL NINO/SOUTHERN OSCILLATION. FLOW PATTERN - THE PATTERN OF WIND INFERRED BY THE 500-HPA CONTOURS - THE WIND TENDS TO BLOW PARALLEL TO THE CONTOURS WITH LOW HEIGHT ON THE LEFT - IN THE NORTHERN HEMISPHERE - THE OPPOSITE IS TRUE IN THE SOUTHERN HEMISPHERE. WIND SPEED IS INVERSELY PROPORTIONAL TO THE SPACING BETWEEN THE CONTOURS. GFS - GLOBAL FORECAST SYSTEM. THIS REFERS TO ANY OF THE GLOBAL MODELS RUN AT NCEP FOUR TIMES A DAY THAT USED TO BE REFERRED TO AS THE MRF AND AVN MODELS. THE MODEL RUN INITIATED AT 00Z (00 GMT) IS CURRENTLY THE ONLY ONE USED BY CPC IN ITS OFFICIAL BLEND FORECAST - ALTHOUGH THE OTHERS CAN BE CONSIDERED BY THE FORECASTER IN FORMULATING THE TEMPERATURE AND PRECIPITATION FORECASTS. GFS ENSEMBLE - A SET OF GFS FORECASTS WHICH ARE ALL VALID AT THE SAME TIME BUT WHOSE STARTING CONDITIONS DIFFER BY SMALL AMOUNTS. THERE ARE CURRENTLY 25 MEMBERS IN THE GFS ENSEMBLE. THE AVERAGE OF THESE IS THE GFS ENSEMBLE MEAN. 500-HPA HEIGHT IS THE HEIGHT - IN METERS - ABOVE MEAN SEA LEVEL - WHICH ABOUT HALF OF THE MASS OF THE ATMOSPHERE LIES ABOVE AND BELOW - AS MEASURED BY THE PRESSURE. UPPER AIR STORM SYSTEMS TEND TO BE STEERED IN THE DIRECTION OF THE WINDS AT 500-HPA. 500-HPA SYSTEMS CORRELATE STRONGLY WITH SURFACE WEATHER. HPA - HECTO-PASCALS. 1 HPA = 1 MILLIBAR. LA NINA - THE COLD PHASE OF ENSO. MERIDIONAL FLOW PATTERN - OCCURS WHEN 500-HPA CONTOURS EXHIBIT LARGE NORTHWARD AND SOUTHWARD EXCURSIONS WITH EXTENSIVE AREAS OF SOUTHERLY AND NORTHERLY FLOW. MODEL BIAS - THE DIFFERENCE BETWEEN THE MODEL CLIMATOLOGY AND THE OBSERVED CLIMATOLOGY - EXPRESSED AS BIAS = MODEL CLIMO - OBSERVED CLIMO. MODEL OF THE DAY - FOR 6-10 DAYS - IS THE MODEL WHOSE SOLUTION IS CONSIDERED TO BE MORE RELIABLE THAN USUAL - AND MAY BE GIVEN HIGHER THAN TYPICAL WEIGHT IN THE BLEND. NO MODEL OF THE DAY IS CHOSEN FOR 8-14 DAYS. MOS - MODEL OUTPUT STATISTICS - A STATISITCAL TOOL FOR SPECIFYING THE SURFACE TEMPERATURE (AND ITS ANOMALY) FROM MODEL FIELDS - CORRECTING AUTOMATICALLY FOR BOTH BIASES IN THE MODEL FIELDS AND THE SPECIFICATION METHOD. IT IS VALID AS LONG AS A GIVEN CONFIGURATION OF A MODEL IS NOT CHANGED OR MODIFIED. MJO - MADDEN-JULIAN OSCILLATION - ALSO CALLED TROPICAL INTRA-SEASONAL OSCILLATION - A SERIES OF WAVES WITH A PERIOD AVERAGING 50 DAYS THAT MOVES SLOWLY EASTWARD NEAR THE EQUATOR ALTERNATELY ENHANCING AND SUPRESSING PRECIPITATION. NAO - NORTH ATLANTIC OSCILLATION TELECONNECTION PATTERN. IT CAN ALSO BE VIEWED AS THE ATLANTIC HALF OF THE AO (ARCTIC OSCILLATION) TELECONNECTION PATTERN - STRONGLY INFLUENCES TEMPERATURES OVER EUROPE AND MUCH OF NORTH AMERICA - ESPECIALLY DURING THE COLD SEASONS - AND DETERMINES THE MEAN LATITUDE OF THE PREVAILING STORM TRACKS ACROSS THE NORTH ATLANTIC. THE PHASE OF THE NAO IS CONSIDERED POSITIVE WHEN PRESSURES AND HEIGHTS ARE BELOW NORMAL OVER GREENLAND AND ICELAND (STRONG ICELANDIC LOW) AND ABOVE NORMAL AT MIDDLE AND SUBTROPICAL LATITUDES (STRONG BERMUDA-AZORES HIGH) - AND NEGATIVE FOR THE REVERSE ANOMALIES. PNA - PACIFIC NORTH AMERICAN TELECONNECTION PATTERN. PROG - PROGNOSIS - OR FORECAST. PROGRESSION OR PROGRESSIVE MOTION - THE NORMAL MOVEMENT OF ATMOSPHERIC WEATHER SYSTEMS (HIGHS... LOWS... RIDGES... OR TROUGHS) FROM WEST TO EAST IN THE MIDDLE LATITUDES. RETROGRESSION OR RETROGRADE MOTION - A TYPE OF MOTION SOMETIMES OBSERVED IN WEATHER SYSTEMS WHEN THEY END UP IN POSITIONS FURTHER TO THE WEST THAN THEIR ORIGINAL LOCATIONS - CONTRARY TO THEIR USUAL WEST TO EAST MOTION. RIDGE - A REGION OF UNUSUALLY HIGH 500-HPA HEIGHT. SHORT WAVES - RELATIVELY LOW-AMPLITUDE - FAST-MOVING DISTURBANCES OF THE 500-HPA FIELD. SOUTHERN STREAM - A FLOW PATTERN WITH UNUSUALLY STRONG FLOW ACROSS THE SOUTHERN U.S. - ACCOMPANIED BY UNUSUAL STORMINESS IN THE SOUTH AND SOUTHEAST. SPECIFICATIONS - KLEIN AND NEURAL NETWORK SPECIFICATIONS GIVE THE HISTORICAL RELATIONSHIP BETWEEN 500-HPA HEIGHT ANOMALIES AND SURFACE TEMPERATURE AND PRECIPITATION. KLEIN SPECIFICATIONS TEND TO EMPHASIZE REGIONAL TELECONNECTIONS WHILE THOSE FROM THE NEURAL NETWORK WORK FROM GLOBAL TELECONNECTIONS. . . . . . . . TELECONNECTIONS GIVE THE HISTORICAL RELATIONSHIP BETWEEN THE 500-HPA HEIGHT AT A GIVEN POINT AND ALL OTHER POINTS ON A MAP FOR A GIVEN TIME OF YEAR. WE AVERAGE THE TOP/BOTTOM 10% OF DAILY MAPS FROM 1950-1999 FOR THE SAME TIME OF YEAR HAVING THE HIGHEST/LOWEST 500-HPA HEIGHT AT THE SPECIFIED POINT. TROUGH - A REGION OF UNUSUALLY LOW 500-HPA HEIGHT. UTC - UNIVERSAL TIME COORDINATED - SAME AS GREENWICH MEAN TIME (GMT). WESTERLY WIND - WIND BLOWING FROM WEST TO EAST. EASTERLY WIND - WIND BLOWING FROM EAST TO WEST. NORTHERLY WIND - WIND BLOWING FROM NORTH TO SOUTH SOUTHERLY WIND - WIND BLOWING FROM SOUTH TO NORTH. ZONAL FLOW PATTERN - OCCURS WHEN 500-HPA CONTOURS LIE IN AN EAST-WEST DIRECTION PARALLEL TO LATITUDE CIRCLES WITH NEARLY PURE WEST-TO-EAST FLOW. ---------------------------------------------------------------------- THE NEXT MONTHLY AND SEASONAL OUTLOOKS WILL BE RELEASED ... THURSDAY JAN 15 2004. ANALOGS TO THE 5 DAY MEAN OBSERVED PATTERN CENTERED 3 DAYS AGO (D-3) FOR THE REGION FROM 20N TO 70N LATITUDE AND 175E TO 60W LONGITUDE INCLUDE THE 5 DAY PERIODS CENTERED ON THE FOLLOWING DATES: 19580103 - 19911225 - 19610106 - 19580106 - 19860107 ANALOGS TO THE 7 DAY MEAN OBSERVED PATTERN CENTERED 4 DAYS AGO (D-4) FOR THE REGION FROM 20N TO 70N LATITUDE AND 175E TO 60W LONGITUDE INCLUDE THE 7 DAY PERIODS CENTERED ON THE FOLLOWING DATES: 19580103 - 19580106 - 19610105 - 19860106 - 19911225 6 to 10 day Outlook Table STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON B B OREGON B N NRN CALIF B N SRN CALIF B A IDAHO B A NEVADA B A W MONTANA B N E MONTANA B A WYOMING B A UTAH B A ARIZONA N A COLORADO N A NEW MEXICO N B N DAKOTA N B S DAKOTA N B NEBRASKA N B KANSAS N B OKLAHOMA N N N TEXAS N N S TEXAS N B W TEXAS N B MINNESOTA N N IOWA N A MISSOURI N A ARKANSAS N N LOUISIANA A N WISCONSIN N A ILLINOIS N A MISSISSIPPI A N MICHIGAN A A INDIANA A N OHIO A N KENTUCKY A N TENNESSEE A A ALABAMA A N NEW YORK A N VERMONT A N NEW HAMP A N MAINE A N MASS A N CONN A N RHODE IS A N PENN A N NEW JERSEY A N W VIRGINIA A A MARYLAND A N DELAWARE N N VIRGINIA A A N CAROLINA A A S CAROLINA A N GEORGIA A N FL PNHDL A B FL PENIN A B AK N SLOPE N N AK ALEUTIAN A N AK WESTERN N N AK INT BSN N N AK S INT B B AK SO COAST B B AK PNHDL B B 8 to 14 day Outlook Table STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON B B OREGON B A NRN CALIF B A SRN CALIF B N IDAHO B A NEVADA N A W MONTANA B N E MONTANA B N WYOMING B A UTAH N A ARIZONA N N COLORADO B A NEW MEXICO N B N DAKOTA B N S DAKOTA B A NEBRASKA B A KANSAS B N OKLAHOMA B N N TEXAS N B S TEXAS N B W TEXAS N B MINNESOTA B N IOWA B N MISSOURI B A ARKANSAS N A LOUISIANA N N WISCONSIN B N ILLINOIS N A MISSISSIPPI N A MICHIGAN N N INDIANA N A OHIO N A KENTUCKY N A TENNESSEE N A ALABAMA N N NEW YORK N N VERMONT A N NEW HAMP A N MAINE A N MASS N N CONN N N RHODE IS N N PENN N A NEW JERSEY N N W VIRGINIA N A MARYLAND N A DELAWARE N A VIRGINIA N A N CAROLINA N A S CAROLINA N N GEORGIA N N FL PNHDL N N FL PENIN A B AK N SLOPE A N AK ALEUTIAN N N AK WESTERN N B AK INT BSN N B AK S INT B B AK SO COAST B B AK PNHDL B B LEGEND TEMPS WITH RESPECT TO NORMAL PCPN WITH RESPECT TO MEDIAN A - ABOVE N - NEAR NORMAL A - ABOVE N - NEAR MEDIAN B - BELOW B - BELOW THE FORECAST CLASSES REPRESENT AVERAGES FOR EACH STATE. NORMAL VALUES - WHICH MAY VARY WIDELY ACROSS SOME STATES - ARE AVAILABLE FROM YOUR LOCAL WEATHER SERVICE FORECAST OFFICE. FOR ADDITIONAL INFORMATION SEE MESSAGE FXUS06 KWBC - ON AWIPS AS PMDMRD. $$