[1] WU Shang-sen, LIANG Jian-yin.. Schematic predictive model for extremely severe cold months in SouthChina winter [J]. Journal of Tropical Meteorology, 2000, 16(3): 193-201.
[2] ZHU Qian-geng, XIE Li-an. 1986 ~ 1987 northern winter Asia/Australia circulation anomalies with theirrelation to the western Pacific SST [J]. Journal of Tropical Meteorology, 1988, 4(3): 254-262.
[3] SHI Neng. Features of the East Asian winter monsoon intensity on multiple time scale in recent 40 years andtheir relation to climate [J]. Quarterly Journal of Applied Meteorology, 1996, 7(2): 175-182.
[4] SHI Neng, ZHU Qian-geng, WU Bin-gui. The East Asian summer monsoon in relation to summer largescale weather-climate anomaly in China for last 40 years [J]. Scientia Atmospherica Sinica, 1996, 20(5):575-583.
[5] HUANG Da-wen. Analysis and forecasting of cold air surges in Guangdong [J]. Journal of Guangdong Meteorology,1995, (4): 2-6.
[6] LI Xiao-quan, LIU Zong-xiu. Area index of 500-hPa polar vortex for Northern Hemisphere and regions dividedwithin it [J]. Meteorological Monthly, (suppl. ), 1986, 69.
[7] PENG Gong-bing, LI Qing, QIAN Bu-dong. Climate and Snow Cover [M]. Beijing: Meteorological Press,1992. 59-65, 84-91.
[8] LI Wei-jing. General Atmospheric circulation anomaly in 1988 and their impact on climate anomaly inChina [J]. Meteorological Monthly, 1999, (4): 20-25.
[9] CHEN Qian-jin, GAO Bo, ZHANG Qiang. Studies on relation of snow cover over the Tibetan Plateau inwinter to the winter-summer monsoon change [J]. Scientia Atmospherica Sinica, 2000, 24(4): 477-492.