PROGNOSTIC DISCUSSIONS FOR 6 TO 10 AND 8 TO 14 DAY OUTLOOKS NWS CLIMATE PREDICTION CENTER CAMP SPRINGS MD 300 PM EDT TUE SEP 9 2003 6 TO 10 DAY OUTLOOK FOR SEP 15 - SEP 19 2003 . . . . . . . DURING THE 1 TO 5 DAY PERIOD... A TROUGH IN THE NORTHWEST AND A RIDGE IN THE EAST ARE SHOWN BY ALL MODELS. ALL MODELS HAVE THE NW TROUGH PROGRESSING EAST WITH TIME AND LOCATED IN THE CENTER OF THE COUNTRY BY DAY 5. THE 0Z AND 6Z GFS SHOW A LOW TRACKING UP THE EAST COAST AT DAY 5 AND THIS FEATURE IS SUPPORTED BY THE UKMET AND NOGAPS. THE 0Z GFS ALSO SHOWS A TROUGH MOVING INTO THE NW BY DAY 6. AN ANALYSIS OF THE ENSEMBLE SPAGHETTI CHARTS SHOWS ON DAY 5 THAT THE ECMWF IS IN LINE WITH MOST ENSEMBLE MEMBERS IN THE EAST WHILE THE 0Z GFS IS IN LINE WITH THE MAJORITY OF ENSEMBLE MEMBERS IN THE WEST. DURING THE 6 TO 10 DAY PERIOD... THE 0Z AND 6Z GFS ARE IN GOOD AGREEMENT IN ESTABLISHING A BROAD TROUGH OVER THE NORTHERN TIER OF THE U.S. CENTERED IN THE WESTERN GREAT LAKES STATES. THE ECMWF SHOWS A TROUGH IN THE NW WHILE THE 0Z AND 6Z GFS ARE MORE ZONAL IN THAT REGION. THE 0Z... AND ESPECIALLY THE 6Z GFS EXTENDS AN ATLANTIC RIDGE INTO THE EAST COAST WHILE THE ECMWF FEATURES A ZONAL PATTERN THERE. OF GREAT IMPORTANCE FOR EAST COAST PRECIPITATION AMOUNTS IS WHETHER A BLOCKING HIGH OVER THE CANADIAN MARITIMES WILL SLOW THE PROGRESSION OF AN EASTWARD MOVING TROUGH FROM THE GREAT LAKES. A SLOWER PROGRESSION OF SUCH A TROUGH FAVORS HIGHER PRECIPITATION AMOUNTS ALONG THE EAST COAST. THE ECMWF IS IN MUCH BETTER AGREEMEMT TODAY WITH ITS PREVIOUS RUN THAN IT WAS YESTERDAY AND WAS GIVEN MORE WEIGHT IN TODAYS BLEND THAN YESTERDAY. HOWEVER... THE 0Z GFS HAS BEEN ENJOYING HIGHER 500 MB ANOMALY CORRELATIONS WITH THE OBSERVED PATTERN RELATIVE TO THE ECMWF OVER NORTH AMERICA... AND ANOMALY CORRELATIONS FOR THE ECMWF HAVE BEEN TRENDING DOWNWARDS FOR THE LAST MONTH. THEREFORE... THE 0Z GFS WAS CHOSEN AS THE MODEL OF THE DAY. AS WAS THE CASE YESTERDAY... THE 5 DAY MEAN GFS ENSEMBLE SPAGHETTI CHARTS SHOW A GREAT DEGREE OF VARIABILITY IN BOTH THE EAST AND THE WEST FOR THE 5820 METER CONTOUR. MODEL OF THE DAY: 0Z GFS FORECAST CONFIDENCE FOR THE 6 TO 10 DAY PERIOD IS BELOW AVERAGE TODAY ... 2 ON A SCALE FROM 1 TO 5 DUE TO LARGE SPREAD AMONG GFS ENSEMBLE MEMBERS. THE OFFICIAL HEIGHT PROG FOR TODAY CONSISTS OF 50 PERCENT OF TODAYS 00Z GFS CENTERED ON DAY 8... 20 PERCENT OF TODAYS GFS ENSEMBLE MEAN CENTERED ON DAY 8... AND 30 PERCENT OF THE ECMWF SOLUTION CENTERED ON DAY 7. THE TEMPERATURE PROG IS BASED ON THE KLEIN SPECIFICATIONS... THE CPC 0Z GFS BIAS CORRECTED TEMPERATURES... MOS TEMPERATURES FROM THE GFS ENSEMBLES... AND ANALOGS TO THE 500 MB BLENDED HEIGHT FIELDS. THE CDC CALIBRATED TEMPERATURES OFF THE 0Z GFS WERE UNAVAILABLE TODAY. THE PRECIPITATION PROG IS BASED ON THE CPC 0Z GFS CALIBRATED PRECIPITATION... THE GFS ENSEMBLE MEAN CALIBRATED PRECIPITATION AND PERCENTAGES... ANALOGS OF THE 500 MB BLENDED HEIGHT FIELDS AND NEURAL NET SPECIFICATIONS. THE CDC CALIBRATED PRECIPITATION TOOLS OFF THE 0Z GFS WERE UNAVAILABLE TODAY. . . . . . . . 8 TO 14 DAY OUTLOOK FOR SEP 17 - SEP 23 2003 DURING THE 8 TO 14 DAY PERIOD THERE IS NO IMPROVEMENT IN THE HIGH DEGREE OF UNCERTAINTY ENCOUNTERED DURING YEATERDAYS FORECAST. THE D+11 GFS ENSEMBLE MEMBERS CONTINUE TO EXHIBIT AN ABNORMALLY HIGH AMOUNT OF SPREAD FOR THE 5820 METER CONTOUR. IN COMPARISON TO YESTERDAYS GFS ENSEMBLE SPAGHETTI DIAGRAMS... TODAYS SET APPEARS TO FAVOR MORE OF A TROUGH IN THE EAST AND BACKS OFF FROM DIGGING A TROUGH OFF THE WEST COAST. HOWEVER... DUE TO THE LARGE SPREAD BETWEEN GFS ENSEMBLE MEMBERS ... THESE TRENDS CANNOT BE STATED WITH MUCH CONFIDENCE. THIS UNCERTAINTY IS BORNE OUT BY THE DISCREPANCY BETWEEN THE 0Z AND 6Z GFS SOLUTIONS. THE 0Z GFS IS MAINLY ZONAL IN THE WEST WHILE THE 6Z GFS DIGS A TROUGH IN THE ROCKIES. MEANWHILE... THE 6Z GFS HAS A CUT-OFF LOW OFF THE EAST COAST WHICH IS ABSENT FROM THE 0Z GFS. DUE TO THE GREAT UNCERTAINTY TODAY... HIGH WEIGHT WAS GIVEN TO THE D+11 GFS ENSEMBLE MEAN. HIGH WEIGHT WAS ALSO GIVEN TO THE D+8 ECMWF DUE TO ITS RELATIVELY HIGH ANOMALY CORRELATIONS WITH THE OBSERVED 500 MB HEIGHTS. CONFIDENCE IN THE WEEK 2 FORECAST IS MUCH BELOW AVERAGE... 1 ON A SCALE OF 1 TO 5 DUE TO REMARKABLY LARGE SPREAD AMONG D+11 GFS ENSEMBLE MEMBERS. THE OFFICIAL 500-HPA HEIGHT PROG FOR TODAY CONSISTS OF 40 PERCENT OF TODAYS GFS ENSEMBLE MEAN CENTERED ON DAY 11... 40 PERCENT OF TODAYS 5-DAY MEAN ECMWF CENTERED ON DAY 7... 10 PERCENT OF TODAYS 00Z GFS CENTERED ON DAY 11 AND 10 PERCENT OF TODAYS DAVA CENTERED ON DAY 11. THE TEMPERATURE PROG IS BASED ON THE KLEIN... NEURAL NET... AND ANALOGS ON THE VARIOUS MODELS... AND CPC 0Z GFS BIAS CORRECTED TEMPERATURES. THE CDC 0Z GFS CALIBRATED TEMPERATURES WERE UNAVAILABLE TODAY. THE PRECIPITATION PROG IS BASED ON CALIBRATED PRECIPITATION OFF THE GFS ENSEMBLE MEAN AND 0Z GFS AS WELL AS ANALOGS AND NEURAL NET SPECIFICATIONS OFF THE INDIVIDUAL MODELS AND THE BLENDED HEIGHT FIELDS... AND THE CPC BIAS CORRECTED PRECIPITATION FROM THE 0Z GFS. THE CDC CALIBRATED 0Z GFS PRECIPITATION WAS NOT AVAILABLE TODAY. FORECASTER: S. HANDEL . . . . . . . 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 SEP 18 2003. 6 to 10 day Outlook Table STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON B A OREGON N N NRN CALIF N B SRN CALIF A B IDAHO N N NEVADA N B W MONTANA B N E MONTANA N N WYOMING N B UTAH N B ARIZONA A B COLORADO N B NEW MEXICO A B N DAKOTA N N S DAKOTA N N NEBRASKA N N KANSAS N B OKLAHOMA N B N TEXAS N B S TEXAS N N W TEXAS A B MINNESOTA N N IOWA N N MISSOURI N B ARKANSAS B B LOUISIANA B N WISCONSIN N N ILLINOIS N N MISSISSIPPI B N MICHIGAN N N INDIANA N N OHIO N N KENTUCKY N N TENNESSEE B N ALABAMA B N NEW YORK N N VERMONT A N NEW HAMP A A MAINE A A MASS A A CONN N A RHODE ISL A A PENN N A NEW JERSEY N A W VIRGINIA N N MARYLAND N A DELAWARE N A VIRGINIA N A N CAROLINA B A S CAROLINA B N GEORGIA B N FL PNHDL B N FL PENIN B N AK N SLOPE B N AK ALEUTIAN B N AK WESTERN B N AK INT BSN B A AK S INT B A AK S COAST B N AK PNHDL B A 8 to 14 day Outlook Table STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON B A OREGON N N NRN CALIF N B SRN CALIF A B IDAHO N B NEVADA N B W MONTANA N N E MONTANA A N WYOMING A B UTAH A B ARIZONA A B COLORADO A B NEW MEXICO A B N DAKOTA A N S DAKOTA A N NEBRASKA A B KANSAS A B OKLAHOMA A B N TEXAS A B S TEXAS A B W TEXAS A B MINNESOTA A A IOWA A N MISSOURI A N ARKANSAS A N LOUISIANA N N WISCONSIN A A ILLINOIS A N MISSISSIPPI N N MICHIGAN A A INDIANA A N OHIO N N KENTUCKY N N TENNESSEE N N ALABAMA B N NEW YORK N N VERMONT A N NEW HAMP N A MAINE A A MASS N A CONN N A RHODE IS N A PENN N N NEW JERSEY N N W VIRGINIA N N MARYLAND N N DELAWARE N N VIRGINIA N N N CAROLINA B N S CAROLINA B A GEORGIA B A FL PNHDL B A FL PENIN B N AK N SLOPE B B AK ALEUTIAN B B AK WESTERN B B AK INT BSN B N AK S INT B N AK SO COAST B A AK PNHDL B A 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. $$