[1] CHEN Lian-shou, XU Xiang-de, LUO Zhe-xian, et al.Introduction to Tropical Cyclone Dynamics [M]. Beijing:China Meteorological Press, 2002, 11.
[2] CHEN Lian-shou, DING Yi-hui. Introduction to theWestern Pacific typhoon [M]. Beijing: Science Press, 1979.
[3] LI Jiang-nan, WANG An-yu, YANG Zhao-li, et al.Advancement in the study of typhoon rainstorm [J]. J. Trop.Meteor., 2003, 19(Suppl.): 152-159.
[4] CHEN Jian, KONG Yu-shou. The application of satellitenephogram on analog forecast for typhoon track [J]. MarineForecasts, 2004, 21(3): 22-28.
[5] FAN Ai-fen, LI Xiu-li, DONG Jia-bin. Analysis of threetropical cyclones with similar tracks but different precipitationfeature [J]. Meteor. Mon., 2004, 30(5): 33-37.
[6] SUN Jian-hua, QI Lin-lin, ZHAO Si-xiong. A study onmesoscale convective systems of the severe heavy rainfall inNorth China by “9608” typhoon [J]. Acta Meteor. Sinica, 2006,64(1): 57-71.
[7] LIANG Jun, CHEN Lian-shou, LI Yin, et al. The analysisof tropical cyclone precipitation affecting the Liaodongpeninsula [J]. J. Trop. Meteor., 2006, 22(1): 41-49.
[8] YU Zhen-shou, GAO Shou-ting, REN Hong-xiang. Anumerical study of the severe heavy rainfall associated withthe typhoon HAITANG(0505)[J]. Acta Meteor. Sinica, 2007,65(6): 864-876.
[9] ZHANG Jian-hai, ZHU Xiao-ming, WANG Li-hua.Comparative analysis of the intensity and distribution ofrainstorm in Zhejiang Province caused by typhoon Haitang andMatsa [J]. J. Trop. Meteor., 2007, 23(2): 126-134.
[10] ZHANG Heng-de, KONG Qi. Diagnostic analysis ofsevere tropical storm BILIS heavy rain event [J]. Meteor. Mon.,2007, 33(5): 42-47.
[11] YAO Rong, LI Zu-xian, YE Cheng-zhi, et al. Causalityanalysis of super rainstorm and mountain torrents by strongtropical storm “Bilis” [J]. Meteor. Mon., 2007, 33(8): 40-46.
[12] YU Zhen-shou, LIAO Shen-shi, HUANG Ke-hui, et al. Anumerical simulation study of typhoon Rananim (0414) [J].Acta Meteor. Sinica, 2005, 63(6): 903-913.
[13] ZHENG Qing-lin, WU Jun. Numerical study oforographic effect on amplification of typhoon precipitation [J].J. Nanjing Inst. Meteor., 1996, 19(1):8-17.
[14] DENG Guo, ZHOU Yu-shu, YU Zhan-jiang. Analysis ofwater vapor transportation in typhoon DAN (9914) [J]. J. Trop.Meteor., 2005, 21(5): 533-541.
[15] MARKS F D, HOUZE R A Jr, GAMACHE J F.Dual-aircraft investigation of the inner core of HurricaneNorbert. Part I: Kinematic structure [J]. J. Atmos. Sci., 1992,49: 919-942.
[16] FRANKLIN J L, LORD S J, FEUER S E, et al. Thekinematic structure of Hurricane Gloria (1985) determinedfrom nested analyses of dropwind-sonde and Doppler radardata [J]. Mon. Wea. Rev., 1993, 121: 2433-2451.
[17] GAMACHE J F, WILLOUGHBY H E, BLACK M L, etal. Wind shear, sea surface temperature, and convection inhurricanes observed by airborne Doppler radar [C]. Preprints,1997, 22d Conf. Hurricanes and Tropical Meteorology, FortCollins, CO, Am. Meteor. Soc., 121-122.
[18] REASOR P D, MONTGOMERY M T, MARKS F D Jr,et al. Low-wavenumber structure and evolution of thehurricane inner core observed by airborne dual-Doppler radar[J]. Mon. Wea. Rev., 2000, 128: 1653-1680.
[19] BLACK M L, GAMACHE J F, MARKS F D, et al.Eastern Pacific Hurricanes Jimena of 1991 and Olivia of 1994:The effect of vertical shear on structure and intensity [J]. Mon.Wea. Rev., 2002, 130: 2291-2312.
[20] CORBOSIERO K L, MOLINARI J. The effects of verticalwind shear on the distribution of convection in tropicalcyclones [J]. Mon. Wea. Rev., 2002, 130: 2110-2123.
[21] FRANK W M, RITCHIE E A. Effects of vertical windshear on the intensity and structure of numerically simulatedhurricanes [J]. Mon. Wea. Rev., 2001, 129: 2249-2269.
[22] ROGERS R, CHEN S, TENERELLI J, et al. A numericalstudy of the impact of vertical shear on the distribution ofrainfall in hurricane Bonnie (1998) [J]. Mon. Wea. Rev., 2003,131: 1577-1599.
[23] ZHANG D L, KIEU Chanh Q. Shear-forced verticalcirculations in tropical cyclones [J]. Geophys. Res. Lett., 2005,32, L13822, doi: 10.1029/2005GL023146.