[1] Anther R A,Chang S W,1978 .Response of the hurricane boundary layer to change of sea surface temperature in a numerical model. J. Atmos. Sci.,35 : 1240-1255.
[2] Anther R A,1987 [Translation]. Ikvelopment,structure and influence of tropical cyclones. Beijing;Meteorological Press. 74. Translated from English by Li Yufang et al.
[3] Holland G J,1983 .Tropical cyclones in the Australian/Southwest Pacific Region .J .Atmos .Sci.Paper No. 363. Colorado State University. 264.
[4] Holland G J,1985 [Translation]. Transportation of angular momentum in tropical cyclones. Meteor. Sci. Tech.,4: 27-36. Translated from English by Liang Ii.
[5] Moss M S,Mercert F J .1976 .A note on several low-layer features of Hurricane Eloise(1975). Mon. Wea. Rev.,104: 967-971.
[6] Moss M S. 1977. Low-layer observations along the periphery of 1975 Hurricane Eloise. AMS. Boston, 550-553.
[7] Liang Li,Wu Zhiwei,Fu Fenhua,1990.On angular momentum budgets for typhoons with sudden intensity change. J. prop. Meteor.,6: 273-282.
[8] Liang Li et al.,1985. Budgets of angular momentum for genesis and development of offshore Typhoon 7909 in East China Sea. In:Collected papers from typhoon conference. 379-387(in Chinese).
[9] Wata,Misuzu,1975 [Translation]. On the mechanisms of decaying typhoons. Beijing: Meteorological Press,116-128. Translated from Japanese by C;hen Lianshou.