[1] MASON R B, ANADERSON C E. The development and decay of the 100 mb summer time anticyclone over south Asia [J]. Mon. Wea. Rev., 1963, 91: 3-12.
[2] TAO Shi-yan, ZHU Fu-kang. The 100mb flow patterns in southern Asia in summer and its relation to the advance and retreat of the West-Pacific subtropical anticyclone over the Far East [J]. Acta Meteor. Sinica, 1964, 34(4): 385-395.
[3] TAO Shi-yan, LI Yu-fang, WEN Yu-pu. A preliminary study on the general circulation of east Asia in the upper troposphere and stratosphere [J]. Acta Meteor. Sinica, 1965, 35: 155-165.
[4] ZHU Fu-kang, LU Long-yi, CHEN Xian-ji. South Asia High [M]. Beijing: Science Press, 1980, 1-91.
[5] ZHANG Qiong, QIAN Zheng-an, CHEN Min-lian. The further study about south Asia high in summer I. Statistic analyses of relationship between it and precipitation distribution over northwest China [J]. Plateau Meteor., 1997, 16(1): 21-30.
[6] HUANG Ying, QIAN Yong-fu. Relationships between south Asian high and summer rainfall in North China [J]. Plateau Meteor., 2003, 22(6): 602-607.
[7] ZHANG Qiong. Evolution and mechanism of the SAH and its impact on regional climate [D]. Nanjing: Department of Atmospheric Sciences, Nanjing University, 1999, 1-148.
[8] ZHANG Qiong, WU Guo-xiong, The bimodality of the 100 hPa South Asian High and its relationship to the impacts on the climate anomaly over East Asia in summer [J]. J. Meteor .Soc. Japan, 2002, 80(4): 733-744.
[9] YANG Wei-yu, YE Du-zheng, WU Guo-xiong. The influence of the Tibetan Plateau on the summer thermal and circulation fields over East Asia III. Physical mechanisms of maintaining the stable circulation fields [J]. Chin. J. Atmos. Sci., 1992, 16(4): 409-426.
[10] YE Du-zheng, WU Guo-xiong. The role of the heat source of the Tibetan Plateau in the general circulation [J]. Meteor. Atmos. Phys., 1998, 67: 181-198.
[11] WU Guo-xiong, LI Wei-pin, GUO Hua. Air pump of sensible heat on Tibet Plateau and Asian summer monsoon, Collection for ZHAO Jiu-zhang 90th birthday anniversary [M]. Beijing: Science Press, 1997. 116-126.
[12] LIU Yi-min, WU Guo-xiong, LIU Hui, et al. The effect of spatially nonuniform heating on the formation and variation of subtropical high part III: Condensation heating and South Asia High and western Pacific subtropical high [J]. Acta Meteor. Sinica, 1999, 57(5): 525-538.
[13] LI Xiao-yan, ZHAI Pan-mao. On indices and indicators of ENSO episodes [J]. Acta Meteor. Sinica, 2000, 58(1): 102-109.
[14] LOON H V, ZEREFOS C S, REPAPIS C C. The southern oscillation in the stratosphere [J]. Mon. Wea. Rev., 1982, 110: 225-229.
[15] LI Chong-yin, LONG Zhen-xia, The evolution of QBO and the impact of El Ni?o/South Oscillation [J]. Chin. Sci. Bull., 1990, 35(17): 1313-1316.
[16] LI Chong-yin, LONG Zhen-xia. QBO and its influence on the general atmospheric circulation and the climate in East Asia [J]. Chin. J. Atmos. Sci., 1992, 16(2):167-176.
[17] YANG Hui, LI Chong-yin. Effect of the tropical Pacific-Indian Ocean temperature anomaly mode on the South Asia High [J]. Chin. J. Atmos. Sci., 2005, 29(1): 99-110.