subj/prognostic reasoning for tropical storm 20w warning nr 4// rmks/ 1. For meteorologists. 2. 12 hour summary and analysis. A. The system was upgraded to Tropical Storm (TS) status at 29/06z based on animated metsat imagery indicating a much tighter, well-consolidated low-level circulation center (LLCC), and significantly improved convective banding wrapping into the southern semi-Circle of the storm. This improved banding is best seen in the 290610z amsre image which depicts strong deep con- vection wrapping into the center. Recent storm motion indicates that the steering ridge has strengthened over the past 12 hours as ts 19w moves further north. Thus, ts 20w has deviated significantly from the 29/00z forecast track which guided the storm over Hainan Island, and has moved west-northwestward towards north-central Vietnam over the past 12 hours. The dynamic models are in good agreement and in- dicate a northwestward track into Vietnam. B. Ts 20w is currently tracking northwestward under the steering influence of the low- to mid-level subtropical ridge (str) positioned north of the system. The current position is based on a well-defined LLCC evident in animated infrared satellite imagery. Outflow remains primarily limited to the equatorward periphery of the system due to the continued effects of the northeasterly flow originating from ts 19w which continues to impinge on the northeastern quadrant. The current intensity is based on Dvorak estimates of 45 knots from pgtw and rjtd along with a 291109z qscat pass depicting unflagged 40 knots winds near the center. 3. Forecast reasoning. A. Due to the previously mentioned deviation in track resulting from the strengthening of the str to the north, this forecast rep- resents a more westward track than was depicted in the previous prognostic reasoning. B. Ts 20w is forecast to continue tracking west-northwestward towards north-central Vietnam under the steering influence of the str north of the system. Ts 20w will maintain intensity under gen- erally favorable conditions, and ultimately make landfall approxi- mately 160 nm south of hanoi, Vietnam near tau 24. As the system tracks inland it is expected to weaken significantly, dissipating over land by tau 48. The available dynamic models are in good agree- ment with this forecast. This forecast favors the consensus of avail- able model aids which are in fair agreement throughout the forecast period. Forecast team: Charlie//