WDPN31 PGTW 050300 MSGID/GENADMIN/NAVPACMETOCCEN PEARL//JTWC// SUBJ/PROGNOSTIC REASONING FOR TYPHOON 02W (MITAG) WARNING NR 26// RMKS/ 1. FOR METEOROLOGISTS. 2. PROGNOSTIC REASONING FOR 050000Z5 TO 080000Z8 MAR 02. A. TYPHOON (TY) 02W (MITAG), LOCATED APPROXIMATELY 340 NM NORTHEAST OF DAPA, PHILIPPINES HAS TRACKED NORTHWESTWARD AT 11 KNOTS DURING THE PAST 6 HOURS. THE WARNING POSITION IS BASED ON 042330Z2 VISIBLE AND MULTI-SPECTRAL SATELLITE IMAGERY. THE WARNING INTENSITY IS BASED ON SATELLITE CURRENT INTENSITY ESTIMATES OF 115 TO 127 KNOTS. ANIMATED ENHANCED INFRARED IMAGERY INDICATES THAT THE SYSTEM IS STARTING TO BECOME SHEARED AND VERTICALLY TILTED AS IT ENTERS THE UPPER LEVEL WESTERLIES TO THE NORTH OF THE SYSTEM. ANIMATED INFRARED IMAGERY INDICATES A 25 NM IRREGULAR EYE IS STILL PRESENT. B. THE MID-LEVEL RIDGE LOCATED NEAR 16.0N7 153.0E9 REMAINS THE DOMINANT STEERING MECHANISM FOR TY 02W. THE WESTERN EXTENSION OF THIS RIDGE HAS CONTINUED TO ERODE DURING THE PAST 12 HOURS, RESULTING IN A MORE POLEWARD TRACK. A LOW TO MID-LEVEL RIDGE AT THE SAME LATITUDE OVER THE SOUTH CHINA SEA EXTENDING EAST OVER LUZON IS CREATING HORIZONTAL WIND SHEAR THAT IS EXPECTED TO SLOW THE TRACK SPEED. TY 02W (MITAG) IS BEGINNING TO ENCOUNTER THE UPPER LEVEL WESTERLIES TO THE NORTH, RESULTING IN INCREASED VERTICAL WIND SHEAR. THE DYNAMIC AIDS CONSIDERED INCLUDE NOGAPS, GFDN, UKMET OFFICE (EGRR), JMA GLOBAL, JMA TYPHOON, AND AVIATION (AVN) MODELS. MODEL FORECAST TRACKS ARE GROUPED INTO TWO CLUSTERS AND 1 OUTLIER. ONE CLUSTER INCLUDES EGRR, JTYM, AND JGSM OF WHICH ALL ARE IN GOOD AGREEMENT WITH A NORTHWESTWARD TRACK BETWEEN THE MID-LEVEL RIDGES TO THE EAST AND WEST OF THE SYSTEM UNTIL THE MID-PERIOD. INCREASING VERTICAL WIND SHEAR BEGINS TO WEAKEN THE SYSTEM AFTER THE FIRST 24 HOURS IN THIS CLUSTER OF MODELS. AVN AND GFDN, THE SECOND CLUSTER, TRACK THE SYSTEM NORTHWESTWARD BUT RECURVE THE SYSTEM SHARPLY TO THE NORTHEAST BEGINNING IN THE MID-PERIOD.THE OUTLIER CONSISTS OF NOGAPS, TRACKING TY 02W WEST-NORTHWESTWARD FOR THE FIRST 48 HOURS BEFORE TURNING SOUTHWESTWARD OVER THE CENTRAL PHILIPPINE ISLANDS. BASED ON RECENT TRENDS AND FIELD ANALYSIS, THE SOLUTIONS POSED BY NOGAPS, GFDN AND AVN ARE NOT FAVORED. OUR FORECAST IS BASED ON PERSISTENCE AND A BLEND USING THE AFOREMENTIONED MODEL CLUSTER. C. SLIGHT INTENSIFICATION IS FORECAST AS THE SYSTEM APPROACHES THE RIDGE AXIS. WEAKENING IS THEN FORECAST BASED ON INCREASED VERTICAL WIND SHEAR RELATED TO ENCOUNTERING THE UPPER LEVEL WESTERLIES TO THE NORTH OF THE SYSTEM. D. INITIAL WIND RADII ARE BASED ON IMAGERY AND SYNOPTIC DATA. FORECAST WIND RADII ARE BASED ON CLIMATOLOGY FOR AN AVERAGE- SIZED SYSTEM. FORECAST TEAM: BRYANT/JACOBS/SHERRY/KUMAGA//