National Weather Service Text Product
AFOS product AFDMLB
Dates interpreted at 00:00 UTCDisplaying AFOS PIL: AFDMLB
Product Timestamp: 1998-10-07 06:20 UTC
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224 FXUS62 KMLB 070620 AFDMLB AREA FORECAST DISCUSSION NATIONAL WEATHER SERVICE MELBOURNE FL 220 AM EDT WED OCT 7 1998 CURRENTLY...RATHER STRONG HIGH PRESSURE OVER THE NORTHEAST PART OF THE COUNTRY WITH RIDGE EXTENDING ALONG THE EASTERN SEABOARD PRODUCING SLIGHTLY MORE GRADIENT FLOW THAN LAST NIGHT. SATELLITE/MODEL THETA E FIELDS INDICATE REMAINS OF BACKDOOR FRONT EAST AND NORTHEAST OF THE AREA. SLOWING FRONT OVER THE LOWER MISSISSIPPI VALLEY. JUST A FEW SHOWERS ON RADAR DESPITE PRECIPITABLE WATER RUNNING ABOVE CLIMO. DISCUSSION...THERE IS NOT A LOT OF DIFFERENCE IN THE MODELS HANDLING OF SYNOPTIC FEATURES THIS FORECAST PERIOD. SOUTHERN END OF FRONT WILL CONTINUE TO MAKE VERY SLOW EASTWARD PROGRESS WHILE HIGH PRESSURE RIDGE AXIS PUSHES SOUTH TO ACROSS THE PENINSULA BY THURSDAY. FOR TODAY I EXPECT A SLIGHT CHANCE OF SHOWERS OVER COASTAL SECTIONS AND AFTERNOON SHOWERS/TSTMS FOR THE INTERIOR COUNTIES. NGM POPS LOOK WAY TOO HIGH AS ITS 6 AND 12 HOUR PRECIP FIELDS ARE NOT GOING TO COME CLOSE TO VERIFYING...THE SAME FOR THE ETA. THETA E FIELDS SHOW SLIGHT WEST SOUTHWEST DRIFT OF WEAK BACKDOOR FRONT BUT DO NOT FEEL THIS IS ENOUGH TO WARRANT GOOD CHANCE OR LIKELY POPS THAT THE FWCS INDICATE. LOW LEVEL FLOW BEGINS TO VEER TO SOUTHEAST TONIGHT SO THE CONVERGENCE LINES OFF THE BAHAMAS SHOULD ORIENT THEMSELVES MORE TOWARDS THE EAST CENTRAL FLORIDA COAST. THEREFORE EXPECT A SLIGHT INCREASE IN COASTAL POPS...WHICH IS ALREADY INDICATED IN THE CURRENT PACKAGE. BY THURSDAY THE WEAKENING FRONT SHOULD BE PUSHING INTO THE NORTHWEST PART OF THE STATE WITH HIGH PRESSURE RIDGE EXTENDING ACROSS THE CENTRAL PENINSULA. MOISTURE NOT FORECAST TO CHANGE APPRECIABLY WITH MODELS SHOWING JUST A SLIGHT LOWERING OF HEIGHTS. BEST LIFT WILL REMAIN NEAR FRONTAL BOUNDARY. SLIGHTLY HIGHER POPS IN THE CURRENT FORECAST LOOK GOOD...ESPECIALLY FOR THE NORTH PART OF THE AREA SINCE THERE MAY BEGIN TO BE SOME EFFECT FROM OUTFLOW BOUNDARIES. LASCODY