’n‹…˜f¯‰ÈŠwêU ’n‹…‰ÈŠwçt‡•”“Á•Êu‰‰‰ï u‰‰‘è–¼F Impact of Typhoon on Ocean in the Pacific (ITOP) 2010: High-Resolution Coupled Modeling u‰‰ÒF Prof. Shuyi S. Chen (RSMAS/University of Miami, Miami, Florida) “úEêŠ: 2010”N5Œ20“ú(–Ø) 16F00`17F30 ‹“s‘åŠw—Šw•”1†ŠÙ5ŠK563†º u‰‰—v|: Rapid intensification and decay in hurricanes and typhoons continue to be a major challenge for storm predictions over the Atlantic and Pacific basins. It highlights the urgent need for a better understanding of factors contributing to rapid intensity change and for development of the corresponding advanced prediction models to improve intensity forecasts. The lack of skill in forecasts of storm structure and intensity may be attributed in part to deficiencies in the current prediction models: insufficient grid resolution, inadequate model physics such as PBL/surface and microphysics, and the lack of full coupling to a dynamic ocean. The extreme high winds, intense rainfall, large ocean waves, and copious sea spray in tropical cyclones push the surface-exchange parameters for temperature, water vapor, and momentum into untested regimes. The main objectives of the Impact of Typhoons on Ocean in the Pacific (ITOP) are to better understand and observe typhoons and their impact on the ocean over the western North Pacific and to improve prediction of tropical cyclone formation and development in the next generation research and operational coupled atmosphere-wave-ocean prediction systems. The recent modeling effort at the University of Miami is to develop and test a fully coupled atmosphere-wave-ocean modeling system that is capable of resolving the eye and eyewall in a tropical cyclone at ~1 km grid resolution. The lack of in situ observation to get accurate initial conditions for high-resolution coupled models presents another major challenge for storm prediction in real time, especially in the early stage of development. This study aims to better identify and quantify both convective and large-scale properties of developing cases prior to tropical cyclogenesis as well as significant non-developing cases using an objective cloud-cluster tracking method. An objective means of identifying and tracking developing and non-developing cases has been a major gap in the literature. Improvements in initial conditions for mature storms rest on the use of airborne and satellite observations in high-resolution data assimilation systems and applications of advanced assimilation technique in tropical cyclones. This talk aims to provide an overview of these new challenges using high-resolution coupled model simulations and forecasts of hurricanes and typhoons in 2003-05 and 2008-09. Several cases were observed extensively by recent field programs, namely, the Coupled Boundary Layer Air-Sea Transfer (CBLAST)-Hurricane in 2003-2004, the Hurricane Rainbands and Intensity Change Experiment (RAINEX) in 2005, and some limited observations from the Tropical Cyclone Structure (TCS-08) over the West Pacific. –â‚¢‡‚킹æ: d ®ˆê