[1] MASON R B, ANDERSON C E. The development and decay of the 100mb summertime anticyclone over southern Asia [J]. Mon Wea Rev, 1958, 91(1): 3-12.
[2] ZHU Fu-kang, LU Long-hua, CHEN Xian-ji, et al. The South Asian High [M]. Beijing: Science Press, 1980 (in Chinese).
[3] ZHU Qian-gen, HE Jin-hai. On features of the upper circulation in the establishment of Asian monsoon in 1979 and its medium-range oscillation [J]. J Trop Meteorol, 1985, 1(1): 9-18 (in Chinese).
[4] LUO Si-wei, QIAN Zheng-an, WANG Qian-qian. The climatic and synoptical study about the relation between the Qinghai-Xizang High Pressure on the 100mb surface and the flood and drought in East China in summer [J]. Plateau Meteorol, 1982, 1(2): 1-10 (in Chinese).
[5] ZHANG Qiong, QIAN Yong-fu, ZHANG Xue-hong. Interannual and interdecadal variations of the South Asia High [J]. Chin J Atmos Sci, 2000, 24(1): 67-78 (in Chinese).
[6] ZHU Fu-kang, FAN Yun. The features of the diabatic heating and the kinetic energy budget over the Qinghai-Xizhang Plateau during the early summer 1979 [J]. Acta Meteorol Sinica, 1987, 45(2): 219-228 (in Chinese).
[7] ZHANG Qiong. Evolution patterns, mechanisms of the South Asian High and its impact on regional climate [D]. Nanjing: Nanjing University, 1999: 149 (in Chinese).
[8] JU Jian-hua. Simulation of the precipitation during Yunnan rainy season with the UGAMP GCM [J]. J Yunnan Univ, 1994, 16 (Suppl): 53-57 (in Chinese).
[9] QIAN Yong-fu, JIANG Jing, ZHANG Yan, et al. The earliest onset area of the tropical Asian summer monsoon and its mechanisms [J]. Acta Meteorol Sinica, 2004, 62(2): 129-139 (in Chinese).
[10] XU Xiang-de, YIN Shu-xin, SHEN Jian-guo, et al. Numerical experiments of the correlation between drought-flood in East China and East Asian zonal stationary waves [J]. J Nanjing Inst Meteorol, 1992, 15(2): 12-20 (in Chinese).
[11] YAO Yong-hong, QIAN Yong-fu. The relationship of the South China Sea monsoon with the South Asia High and its characteristics of seasonal or interannual variations [J]. Adv Atmos Sci, 2003, 17 (Suppl. 1): 57-70.
[12] ZHANG Qing-yun, TAO Shi-yan. The anomalous subtropical anticyclone in western Pacific and their association with circulation over East Asia during summer [J]. Chin J Atmos Sci, 2003, 27(3): 369-380 (in Chinese).
[13] LIU Mei, PEI Hai-ying,YU Jian-wei, et al. On the relationship between 100-hPa South Asia High and Mei-yu in Jiangsu province [J]. J Trop Meteorol, 2011, 17(3): 302-309.
[14] CHI Yan-zhen, HE Jin-hai, WU Zhi-wei. Features analysis of the different precipitation periods in the pre-flood season in South China [J]. J Nanjing Inst Meteorol, 2005, 28(2): 163-171 (in Chinese).
[15] QIAN Yong-fu, ZHANG Qiong, ZHANG Xue-hong. The South Asian High and its effects on China’s mid-summer climate abnormality [J]. J Nanjing Univ (Nat Sci), 2002, 38(3): 295-307 (in Chinese).
[16] TAN Jing, YANG Hui, SUN Shu-qing, et al. Characteristics of the longitudinal oscillation of South Asia High during summer [J]. J Nanjing Inst Meteorol, 2005, 28(4): 452-460 (in Chinese).
[17] HU Jing-gao, TAO Li, ZHOU Bing. Characteristic of South Asia High activity and its relation with the precipitation of East China in summer [J]. Plateau Meteorol, 2010, 29(1): 128-136 (in Chinese).
[18] HUANG Ying, QIAN Yong-fu. Relationships between South Asian High and summer rainfall in North China [J]. Plateau Meteorol, 2003, 22(6): 602-607 (in Chinese).
[19] SHA Wen-yu. Circulation feature of 100mb in Northern Hemisphere and its spectral analysis during a transitional period of anomalous Meiyu season [J]. J Nanjing Univ (Nat Sci Edit), 1985, 21(2): 394-404 (in Chinese).
[20] WANG An-yu, YOU Li-yu. A study of the effects of the anomalies of the subtropical high in the western Pacific region on the floods in the middle and lower reaches of the Yangtze River [J]. Acta Sci Nat Univ Sunyatseni, 1993, 32(2): 68-74 (in Chinese).
[21] ZHANG Qiong, WU Guo-xiong, QIAN Yong-fu. The bimodality of the 100hPa South Asia High and its relationship to the climate anomaly over East Asia in summer [J]. J Meteorol Soc Japan, 2002, 80(4): 733-744.
[22] WANG Li-juan, GUO Shuai-hong. Interannual variability of the South-Asian high establishment over the Indo-china Peninsula from April to May and its relation to southern Asian summer monsoon [J]. Trans Atmos Sci, 2012, 35(1): 10-23 (in Chinese).
[23] KALNAY E, KANAMITSU M, KISTLER R, et al. The NCEP/NCAR 40-year reanalysis project [J]. Bull Amer Meteorol Soc, 1996, 77(3): 437-470.
[24] HE Jin-hai, XU Hai-ming, ZHOU Bing, et al. Large scale features of SCS summer monsoon onset and its possible mechanism [J]. Clim Environ Res, 2000, 5(4): 333-344 (in Chinese).
[25] WANG Qi, DING Yi-hui. Climatological aspects of evolution of summer monsoon over the northern South China Sea [J]. Acta Meteorol Sinica, 1997, 55(4): 466-483 (in Chinese).
[26] LI Chong-yin, QU Xin. Large scale atmospheric circulation evolutions associated with summer monsoon onset in the South China Sea [J]. Chin J Atmos Sci, 2000, 24(1): 1-14 (in Chinese).
[27] DING Yi-hui, LI Chong-yin, HE Jin-hai, et al. South China Sea monsoon experiment (SCSMEX) and the East-Asian monsoon [J]. Acta Meteorol Sinica, 2004, 62(5): 561-586 (in Chinese).
[28] WEN Min, HE Jin-hai, XIAO Zi-niu. Impact of the convection over the Indo-china Peninsula on the onset of SCS summer monsoon [J]. Chin J Atmos Sci, 2004, 28(6): 864-875 (in Chinese).
[29] LI Yan, WANG Ya-fei, WEI Dong. Effects of anomalous SST in tropical Indian Ocean and Pacific Ocean on next June rainfall over the Yangtze River basin and area south of the basin [J]. Acta Meteorol Sinica, 2007, 65(3): 393-405 (in Chinese).
[30] REN Rong-cai, LIU Yi-min, WU Guo-xiong. Impact of South Asia High on the short-term variation of the subtropical anticyclone over western Pacific in July 1998 [J]. Acta Meteorol Sinica, 2007, 65(2): 183-197 (in Chinese).
[31] CHEN Yong-ren, LI Yue-qing. The variations of polar vortex and South Asia High and characters of northern atmosphere circulations at 100 hPa [J]. J Trop Meteorol, 2008, 24(5): 519-526 (in Chinese).
[32] HAN Jie,GUAN Zhao-yong, LI Ming-gang. Comparisons of circulation anomalies between the daily precipitation extreme and non-extreme events in the middle and lower reaches of Yangtze River in boreal summer [J]. J Trop Meteorol, 2015, 21(2): 131-142.
[33] GUO Shuai-hong. Interannual variability of the South-Asian High establishment over the Indo-China Peninsula from April to May: Data analysis and numerical simulation [D]. Nanjing: Nanjing University of Information of Science and Technology, 2012 (in Chinese).