Charney J G,Eliassen A.1964.On the growth of the hurricane de-pression[J].J.Atmos.Sci.,21:68-75.
[2]
陈秋士.1986.重力惯性波的不稳定与台风和中纬度次天气尺度系统发生发展的关系[C]//天气学的新进展,北京:气象出版社,189-213.Chen Qiushi.1986.The relationship between the in-stability of inertia-gravitational wave and genesis and development of typhoon and subsynoptic scale systems in the middle latitude region[C]//Recent Progress on Synoptic Meteorology(in Chi-nese),Beijing:China Meteorological Press,189-213.
[3]
陈英仪.1984.涡旋运动中的波作用密度守恒及稳定性[J].中国科学(B辑),5:476-483.Chen Yingyi.1984.Wave-action density conversation and stability of vortex motions[J].Science in China(Series B)(in Chinese),5:476-483.
[4]
端义宏,余晖,伍荣生.2005.热带气旋强度变化研究进展[J].气象学报,63(5):636-645.Duan Yihong,Yu Hui,Wu Rong-sheog.2005.Review of the research in the intensity change of tropical cyclone[J].Acta Meteorologica Sinica(in Chinese),63(5):636-645.
[5]
Gray W M.1982.Tropical cyclone genesis and intensification[M]//Intense Atmospheric Vortices.Springer-Verlag Berlin Heidei-berg,New York.
[6]
刘式适,倪秉健.1986.惯性稳定度、层结稳定度对台风发展的影响[C]//台风会议文集(1983).上海科学技术出版社,13-22.Liu Shikuo,Ni Bingjian.1986.The influences of inertial stability and stratification stability on typhoon development[C]//Proceed-ings of Conference on Typhoon(1983)(in Chinese).Shaoghai:Shanghai Science ＆ Technology Press,13-22.
[7]
刘式适,杨大升.1980.台风的螺旋结构[J].气象学报,38(3):193-204.Liu Shikuo,Yang Dasheng.1980.The spiral stroc-ture of the tropical cyclone[J].Acta Meteorologica Sinica(in Chinese),38(3):193-204.
[8]
钮学新.1991.不稳定状态下惯性重力波对台风发生、发展和移动的作用[J].海洋学报,13(3):325-332.Niu Xuexin.1991.The effects of inertia-gravitational wave on the development and motion of typhoon in the unstable state[J].Acta Oceanologica Sinica(in Chinese),13(3):325-332.
[9]
夏友龙,郑祖光,刘式达.1995.台风内核与外围加热对其强度突变的影响[J].气象学报,53(4):424-430.Xia Youlong,Zheng Zoguang,Liu Shida.1995.The effects of heating in the inner core and the external part of typhoon on their intensity ab-ropt changes[J].Acta Meteorologica Siniea (in Chinese),53(4):424-430.
[10]
杨大升,丁敏芳.1985.台风发生的非线性动力机制[C]//台风会议文集(1985),北京:气象出版社,231-243.Yang Dasheng,Ding Minfang.1985.Nonlinear dynamical mechanism of typhoon formation[C]//Proceedings of Conference on Typhoon(in Chi-nese),Beijing:China Meteorological Press,231-243.
[11]
杨成彬,郑祖光,王雨.1994.用非线性模型研究环境温度场和涡度场对台风发生、发展的影响[J].大气科学,18(增刊):810-819.Yang Chengbin,Zheng Zuguang,Wang Yu.1984.The studies of impact of environment and vorticity on formation and development of typhoon[J].Chinese Journal of Atmospheric Sci-ences(in Chinese),18(Suppl.):810-819.
[12]
于玉斌.2007.我国近海热带气旋强度突变的机理研究[D].中国气象科学研究院/南京信息工程大学博士学位论文.Yu Yubin.2007.The theoretical study on tropical cyclone intensity sudden ehange over the coastal waters of China[D].Pk D.dissertation (in Chinese),Chinese Academy of Meteorological Sciences and Nanjing University of Information Science ＆ Technology.
[13]
Krishnamurti T N,Pattnaik S,Stefanova L,et al.2005.The hur-ricane intensity issue[J].Mon.Wea.Rev.,133:1886-1912.
[14]
李崇银.1983.对流凝结加热与不稳定波[J].大气科学,7(3):260-268.Li Chongyin.1983.Convective condensation heating and unstable mode[J].Chinese Journal of Atmospheric Sciences (in Chinese),7(3):260-268.
于玉斌,陈联寿,杨昌贤.2008a.超强台风"桑美"(2006)近海急剧增强特征及机理分析[J].大气科学,32(2):405-416.Yu Yubin,Chen Lianshou,Yang Changxian 2008a.The fea-tures and mechanism analysis on rapid intensity change of super typhoon Saomai(2006)over the offshore of China[J].Chinese Journal of Atmospheric Sciences(in Chinese),32(2):405-416.
[17]
于玉斌,段海霞,炎利军,等.2008b.超强台风"桑美"(2006)近海急剧增强过程数值模拟试验[J].大气科学,32(6):1365-1378.Yu Yubin,Duan Haixia,Yah Lijan,et al.2008b.Nu-merical simulation of rapid intensification change of super typhoon Saomai(2006)over the coastal water of China[J].Chinese Jour-nal of Atmospheric Sciences(in Chinese),32(6):1365-1378.
[18]
郑祖光,夏友龙.1994.台风内核与外围能量发展的物理因子[J].热带气象学报,10(4):300-308.Zheng Zuguang,Xia You-long.1994.Physical factors contributing to energy development in inner core and external part of typhoon[J].Journal of Tropical Meteorology(in Chinese),10(4):300-308.
[19]
郑祖光,夏友龙,刘式达.1996.台风内核与外围的强度突变[J].气象学报,54(3):294-302.Zheng Zuguang,Xia Youlong,Liu Shida.1996.The intensity abrupt changing in the inner core and external part of typhoon[J].Acta Meteorologica Sinica(in Chinese),54(3):294-302.
