TS 19W(CHANTHU). WARNING 41 ISSUED AT 16/09UTC.SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. HOWEVER, THE CURRENT FORECAST INCLUDES THE POTENTIAL OF AN ALTERNATE SCENARIO. FORECAST DISCUSSION: HAVING NOW BEGUN ITS TRACK TOWARDS THE NORTHEAST, TS 19W IS FORECAST TO CONTINUE ACCELERATING NORTHEASTWARD, TURNING MORE EASTWARD THROUGH THE DURATION OF THE FORECAST, AHEAD OF AN APPROACHING MID-LATITUDE TROUGH AND ALONG THE NORTHERN PERIPHERY OF THE DEEP SUBTROPICAL RIDGE TO THE SOUTHEAST. THE SYSTEM IS EXPECTED TO MAKE LANDFALL ALONG THE NORTHWESTERN COAST OF KYUSHU NEAR 24H, TRACK OVER THE INLAND SEA AND CROSS JUST SOUTH OF TOKYO BETWEEN 48H AND 60H. THERE REMAINS A SHORT WINDOW OF OPPORTUNITY FOR INTENSIFICATION OVER THE NEXT 12-18 HOURS AS THE VERTICAL WIND SHEAR(VWS) REMAINS RELATIVELY LOW WHILE AT THE SAME TIME THE SYSTEM CONTINUES TO TAP INTO ROBUST POLEWARD OUTFLOW. GOING INTO THE DIURNAL MAXIMUM THIS EVENING, THE SYSTEM SHOULD INTENSIFY UP TO 60 KNOTS BY 12H. ONCE OVER LAND AND TRAVERSING THE INLAND SEA, THE SYSTEM IS EXPECTED TO STEADILY WEAKEN DUE TO INCREASING VWS AND TERRAIN INTERACTION. AS TS 19W MAKES LANDFALL IT IS EXPECTED TO BEGIN INTERACTING WITH A WEAK BAROCLINIC ZONE CURRENTLY LYING ACROSS SOUTHERN KOREA AND JAPAN, AND BEGIN TO EXTRA-TROPICAL TRANSITION (ETT). AS THE SYSTEM COMPLETES ETT, THE WIND FIELD IS FORECAST TO INCREASE AND BECOME INCREASINGLY ASYMMETRIC, WHILE THE LLCC WILL BROADEN OUT AND DEEP CONVECTION WILL RAPIDLY DECAY. THE SYSTEM IS EXPECTED TO COMPLETE ETT BY 48H AS A GALE-FORCE LOW AS IT TRANSITS THE SOUTHERN COAST OF HONSHU. THERE ALSO EXISTS THE POTENTIAL FOR AN ALTERNATE SCENARIO BASED ON THE LATEST GLOBAL MODEL FIELDS, MANY OF WHICH NOW INDICATE A SIGNIFICANTLY WEAKER SYSTEM UNDERGOING ETT WHILE MOVING WELL SOUTH OF TOKYO AND BECOMING QUASI-STATIONARY TO THE SOUTH-SOUTHEAST OF TOKYO. IN THIS SCENARIO THE VORTICITY ASSOCIATED WITH TS 19W SPLITS AFTER LANDFALL, WITH AN AREA MOVING TO THE NORTH OF HONSHU AND BECOMING EXTRA-TROPICAL, WHILE THE REMAINDER TRACKS THROUGH THE INLAND SEA AND REMAINS TROPICAL. THE REMNANTS OF THIS AREA OF VORTICITY THEN TRACK SOUTH OF TOKYO, BUT LACKING DEEP CORE OF CONVECTION, DOES NOT STRONGLY INTERACT WITH THE MID-LATITUDE TROUGH TO THE NORTH, AND THUS SIMULTANEOUSLY DISSIPATES WHILE COMPLETING ETT.
1921090506 123N1397E 15
1921090512 126N1395E 20
1921090518 130N1389E 20
1921090600 135N1385E 20
1921090606 141N1382E 25
1921090612 148N1379E 35
1921090618 152N1373E 45
1921090700 156N1366E 50
1921090706 161N1357E 70
1921090712 163N1346E 95
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1921090800 160N1323E 130
1921090806 156N1313E 140
1921090812 155N1303E 135
1921090818 153N1291E 135
1921090900 155N1281E 140
1921090906 157N1272E 130
1921090912 161N1260E 120
1921090918 166N1250E 120
1921091000 171N1241E 130
1921091006 179N1235E 145
1921091012 187N1228E 150
1921091018 195N1223E 155
1921091100 204N1219E 145
1921091106 211N1216E 135
1921091112 218N1218E 120
1921091118 228N1220E 115
1921091200 238N1223E 110
1921091206 252N1223E 105
1921091212 263N1227E 95
1921091218 275N1232E 90
1921091300 290N1236E 85
1921091306 307N1234E 75
1921091312 310N1234E 65
1921091318 311N1236E 55
1921091400 313N1238E 50
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1921091412 305N1249E 40
1921091418 303N1253E 35
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1921091506 302N1262E 45
1921091512 301N1255E 45
1921091518 303N1252E 50
1921091600 304N1251E 55
1921091606 311N1254E 55
1921090512 126N1395E 20
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1921090600 135N1385E 20
1921090606 141N1382E 25
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1921090618 152N1373E 45
1921090700 156N1366E 50
1921090706 161N1357E 70
1921090712 163N1346E 95
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1921090800 160N1323E 130
1921090806 156N1313E 140
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1921090906 157N1272E 130
1921090912 161N1260E 120
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1921091000 171N1241E 130
1921091006 179N1235E 145
1921091012 187N1228E 150
1921091018 195N1223E 155
1921091100 204N1219E 145
1921091106 211N1216E 135
1921091112 218N1218E 120
1921091118 228N1220E 115
1921091200 238N1223E 110
1921091206 252N1223E 105
1921091212 263N1227E 95
1921091218 275N1232E 90
1921091300 290N1236E 85
1921091306 307N1234E 75
1921091312 310N1234E 65
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1921091400 313N1238E 50
1921091406 307N1243E 45
1921091412 305N1249E 40
1921091418 303N1253E 35
1921091500 303N1257E 35
1921091506 302N1262E 45
1921091512 301N1255E 45
1921091518 303N1252E 50
1921091600 304N1251E 55
1921091606 311N1254E 55
TS 19W(CHANTHU). SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: TROPICAL STORM 19W APPEARS TO HAVE FINALLY STARTED ITS LONG-AWAITED TRACK TOWARDS THE NORTHEAST. ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A VERY WELL DEFINED SWIRL OF LOW-LEVEL CLOUD BANDS WRAPPING INTO A LOW-LEVEL CIRCULATION CENTER (LLCC) OBSCURED BY FLARING CONVECTION EXTENDING SOUTHWARD FROM THE ASSESSED CENTER POSITION. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE ANIMATED VISIBLE IMAGERY, AND WITHIN THE CONGRUENCE OF AGENCY FIX POSITIONS. THE INITIAL INTENSITY REMAINS ASSESSED AT 55 KNOTS WITH MEDIUM CONFIDENCE BASED ON THE MEDIAN OF THE AGENCY CURRENT INTENSITY ESTIMATES, HEDGED SLIGHTLY HIGHER THAN THE ADT AND SATCON ESTIMATES. THE OVERALL STRUCTURE APPEARS SHEARED WITH AN AREA TO THE NORTH OF THE LLCC DEVOID OF ANY SIGNIFICANT CONVECTION. ANALYSIS OF A 160000Z UPPER-AIR SOUNDING FROM HEUKSANDO INDICATE THE PRESENCE OF VERY DRY AIR BETWEEN 300-600MB, WHICH SUPPORTS WHAT IS SEEN IN THE IMAGERY. ADDITIONALLY, WHILE HIGH-RESOLUTION HWRF SOUNDINGS AND CIMSS AUTOMATED UPPER-LEVEL ANALYSIS REVEALS LOW SOUTHERLY WIND SHEAR, THE SHARP NORTHERN EDGE OF THE CONVECTION FLARING NEAR THE CENTER CLEARLY SUPPORT A NORTHERLY SHEAR VECTOR OVER TOP OF THE SYSTEM, AND THE LATEST CIMSS ATMOSPHERIC MOTION VECTOR (AMV) ANALYSIS SUGGESTS THE PRESENCE OF A SMALL, WEAK ANTICYCLONE JUST NORTHWEST OF THE LLCC, WHICH WOULD SUPPORT A NORTHERLY WIND AT 200MB OVER TOP OF 19W. EXCEPTING THE DRY AIR AND THE NORTHERLY SHEAR, THE ENVIRONMENT OTHERWISE FAVORABLE WITH WARM SSTS AND ROBUST POLEWARD OUTFLOW.
TS 19W(CHANTHU). MODEL DISCUSSION: TRACK GUIDANCE IS IN VERY GOOD AGREEMENT THROUGH LANDFALL, WITH ALL GUIDANCE MEMBERS CLOSELY CLUSTERED ABOUT THE MEAN WITH A LANDFALL ALONG THE NORTHWEST COAST OF KYUSHU AT 24H. THEREAFTER THE GUIDANCE DIVERGES, WITH HWRF AND GALWEM JUMPING CIRCULATION CENTERS AND TRACKING THE NORTHERN, SECONDARY LOW DISCUSSED ABOVE AS THE ALTERNATE SCENARIO. THE REMAINDER OF THE TRACKERS SHOW A TRACK GENERALLY EAST-NORTHEASTWARD THROUGH THE REMAINDER OF THE FORECAST PERIOD. HOWEVER, THE GFS, NAVGEM, EGRR AND ECMWF AND ITS ENSEMBLE MEAN HAVE AL SHOWN SIGNIFICANT CHANGES SINCE THE PREVIOUS RUN, AND NOW ALL AGREE ON A SLOWER TRACK SOUTH OF TOKYO THROUGH 72H. INTERESTINGLY, THE GFS AND UKMET ENSEMBLE MEAN TRACKERS REMAIN CONSISTENT WITH THE PREVIOUS RUNS AND INDICATE A FAST TRACK TO THE NORTHEAST, CONSISTENT WITH THE PREVIOUS FORECAST. WHILE THERE IS HIGH CONFIDENCE IN THE 0-24HR FORECAST TRACK, WITH SUCH A HIGH DEGREE OF UNCERTAINTY IN THE DETERMINISTIC GUIDANCE BEYOND 36H AND THE EXTREMELY LARGE SPREAD IN THE ENSEMBLE GUIDANCE, THERE IS OVERALL LOW CONFIDENCE IN THE JTWC FORECAST TRACK. INTENSITY GUIDANCE IS IN OVERALL GOOD AGREEMENT, THOUGH THE HWRF REMAINS UNREALISTICALLY HIGH AS IT JUMPS CIRCULATIONS. THE REMAINDER OF THE GUIDANCE REMAINS TIGHTLY CLUSTERED ABOUT THE CONSENSUS MEAN. THE JTWC FORECAST LIES SLIGHTLY HIGHER THAN THE MEAN WITH MEDIUM CONFIDENCE DUE TO THE UNCERTAINTIES ASSOCIATED WITH THE EXACT TRACK AND THUS THE AMOUNT OF TERRAIN INTERACTION.
9521091312 100N 118W 20
9521091318 100N 138W 20
9521091400 101N 159W 20
9521091406 102N 181W 25
9521091412 102N 199W 25
9521091418 102N 215W 25
9521091500 103N 231W 25
9521091506 103N 246W 30
9521091512 104N 261W 30
9521091518 105N 276W 30
9521091600 115N 315W 25
9521091606 117N 340W 25
9521091318 100N 138W 20
9521091400 101N 159W 20
9521091406 102N 181W 25
9521091412 102N 199W 25
9521091418 102N 215W 25
9521091500 103N 231W 25
9521091506 103N 246W 30
9521091512 104N 261W 30
9521091518 105N 276W 30
9521091600 115N 315W 25
9521091606 117N 340W 25
9621091400 227N 686W 20
9621091406 235N 694W 20
9621091412 242N 700W 20
9621091418 249N 706W 20
9621091500 255N 711W 25
9621091506 264N 720W 25
9621091512 278N 725W 30
9621091518 287N 731W 30
9621091600 293N 740W 30
9621091606 303N 743W 30
9621091406 235N 694W 20
9621091412 242N 700W 20
9621091418 249N 706W 20
9621091500 255N 711W 25
9621091506 264N 720W 25
9621091512 278N 725W 30
9621091518 287N 731W 30
9621091600 293N 740W 30
9621091606 303N 743W 30