Extended Abstract

Two kind of en ergies will help remnant of LTC revival to reinvigorate the rainfall ofremnant. Those are the potential energy and latent heat energy. Those different kind ofenergy could be acqu ired when TC interact w ith westerly trough or monsoon surgerespectively.Remote h eavy rainfall of TC is also an unus ual pheno menon. W ater vapourtransport fo rm a ty phoon pla y a m ajor role. Plenty of water v apour could betransported b y the TC right sid e stream f low. Both of westerly trou gh and lan dtopography have a positive effect to produce a remote rainfall of a TC.BibliographyAkihiko. M2006: A cloud resolving numerical simulation for characteristic rainfallinduced by typhoon Meari (2004). T eam member report o n t opic 0.3 o f sixthWMO IWTC.Dong Meiying, e t al,2010: Rai nfall Reinforcement A ssociated with Landfal lingTropical Cyclone. Journal of Atmospheric Sciences(waiting list).Duan L et al2005: Diagnostic an alysis and nu merical stud y o f t orrential rainassociated with tropical stor m F itow (01 14). Chinese J. Atmos SCI., Vol 29 ,No.3.Liying et al, 2 010: Study on for mation and dev elopment of a mesoscaleconvergence line in typhoon Rananim. Acta meteorologica Sinica, Vol 24, No.4.Yongqing Wang., Yuqing Wang, H F udeyasu, 2009: Th e role of typhoon songd a(2004) in producing d istantly located heavy rainfall in Japan. Monthly WeatherReview, Vol 137, PP3699-3716.Zeng Z.H et al, 2002: Simulation of influence of “urban heat island ” on torrential rainin Shanghai on 5Aug, 2001 Acta Meteorologica Sinica Vol 60, PP58-64..Zhu H. Y., L.S.Chen., X. D. Xu 2000: A numerical Study of the interaction betweentyphoon and mid-latitude circ ulation and its rainfall Cha racteristics. Chin eseJournal of Atmos. SCI., Vol. 24, No. 5.-30-