[1] HUANG Shi-song, YU Zhi-hai. Study on the subtropical high activity and its relation with a number of issues of the general circulation [J]. Acta Meteorologica Sinica, 1961, 31: 339-359.
[2] TAO Shi-yan, ZHU Fu-kang. The relationship between the 100-hPa flow pattern variation in southern Asia in summer and relation with the advancement / retreat of the subtropical high [J]. Beijing: Meteorological Press, 1964. 385-395.
[3] YU Shi-hua, WANG Shao-long. Circulation mechanisms for the mid-term advancement / retreat of the subtropical high in West Pacific [J]. Acta Oceanologica Sinica, 1989, 11: 370-377.
[4] ZHANG Ren, SHI Han-sheng, YU Shi-hua. A study on the issue of non-linear stability of the subtropical high in West Pacific [J]. Chinese Journal of Atmospheric Sciences, 1995, 19: 687-700.
[5] ZHANG Qing-yun, TAO Shi-yan. Tropical and subtropical monsoons in East Asia in summer and precipitation in raining seasons in eastern China [J]. Quarterly Journal of Applied Meteorology, 1998, (supp.): 16-23.
[6] PENG Jia-yi. Effect of ENSO on the West Pacific subtropical high and its interactions with the East Asian monsoon [D]. Nanjing: Nanjing Institute of Meteorology. 1999. 100-114.
[7] TAO Shi-yan, ZHANG Qing-yun, ZHANG Shun-li. The activity of North Pacific subtropical high in summer [J]. Acta Meteorologica Sinica, (to be published).
[8] LUO Jian YU Shi-hua. CEOF analyses of atmospheric low-frequency oscillation in lower latitude region and frequency modulation phenomena of low-frequency signals [J]. Acta Meteorologica Sinica, 1995, 9: 199-206.
[9] YU Shi-hua, ZHANG Ren, YANG Wei-wu. Study on the mechanism governing the advancement / retreat of the subtropical high [J]. Beijing: PLA Press, 1999. 123-169.
[10] LI Jian-ping. Wavelet Analysis and Signal Treatment [M]. Chongqing: Chongqing University Press, 1997. 125-137.
[11] ZHAO Song-nian, XIONG Xiao-yun. Wavelet Transform and Wavelet Analysis [M]. Beijing: Electronic Industrial Press, 1996. 51-63.