1. For meteorologists. 2. 12 hour summary and analysis. A. Tropical Storm (TS) 10w has become much better organized during the past 12 hours, with the development of sustained deep convection and a tightening low level circulation center. The storm has continued to track generally northeastward along the eastern periphery of a broad monsoon circulation and the northwestern periphery of near-equatorial ridging to the south and east. Convec- tive banding has persisted in the convergent low level flow between the storm and the near-equatorial ridge. B. Recent Dvorak intensity estimates of 3.0 from pgtw and 2.5 from knes and a 281925z Quikscat pass indicate that the system has developed into a 35 knot tropical storm over the past 06 hours. Recent microwave satellite imagery, including a 282152z ssmis pass, depict tighten- ing curvature in convective banding near the low level center. High ocean heat content along and near 20 degrees north latitude and favorable poleward and equatorward outflow have contributed to improvements in storm structure. 3. Forecast reasoning. A. The forecast philosophy remains unchanged from the previous warning. B. Ts 10w is expected to continue tracking along the outer periphery of its parent monsoon circulation. In the near term - between tau 00 and tau 24 - the storm will track northeastward to northward in the gradient between the broad monsoon circulation and near-Equator- ial ridging to the southeast. After tau 24, the system is expected to turn westward, continuing along the the outer periphery of the monsoon circulation. A building subtropical ridge to the northeast will provide an additional westward steering influence. The storm is expected to intensify at a climatological rate through tau 36 under the influence of favorable equatorward out- flow and poleward outflow enhanced by the upper tropo- spheric trough (tutt) the north. Thereafter, the storm should continue to intensify over very warm sea surface temperatures, but potential intrusion of more stable, subsident air associated with the TUTT and increasingly suppressed poleward outflow are expected to slow the intensification rate slightly. C. In the extended forecast period, ts 10w is forecast to continue westward along the northern periphery of the broader monsoon circulation and the southern periphery of the subtropical ridge. Slow intensification should continue as the then well-developed typhoon takes advan- tage of high sea surface temperatures and moderate upper level outflow. Forecast team: Delta//