郭准, 郭品文, 茅懋. 2009. 南亚高压在高原建立的路径类型及其分析[J]. 大气科学学报, 32 (6): 815-823. Guo Zhun, Guo Pinwen, Mao Mao. 2009. Motion tracks of South Asia high and its onset mechanisms[J]. Transactions of Atmospheric Sciences (in Chinese), 32 (6): 815-823.
[2]
Liu Xuanfei, Zhu Qiangen, Guo Pinwen. 2000. Conversion characteristics between barotropic and baroclinic circulations of the SAH in its seasonal evolution[J]. Adv. Atmos. Sci., 17 (1): 129-139.
[3]
Liu Yimin, Wu Guoxiong, Ren Rongcai. 2004. Relationship between the subtropical anticyclone and diabatic heating[J]. J. Climate, 17: 682-698.
[4]
Liu Y M, Hoskins B J, Blackburn M. 2007b. Impact of Tibetan orography and heating on the summer flow over Asia[J]. J. Meteor. Soc. Japan, 85: 1-19.
[5]
刘屹岷, 吴国雄, 刘辉, 等. 1999. 空间非均匀加热对副热带高压形成和变异的影响 Ⅲ: 凝结潜热加热与南亚高压及西太平洋副高[J]. 气象学报, 57 (5): 525-538. Liu Yimin, Wu Guoxiong, Liu Hui, et al. 1999. The effect of spatially non-uniform heating on the formation and variation of subtropical high. Part III: Condensation released latent heating in relation to the South-Asian high and subtropical high[J]. Acta Meteorologica Sinica (in Chinese), 57 (5): 525-538.
[6]
刘屹岷, 吴国雄, 宇如聪, 等. 2001. 热力适应、过流、频散和副高II. 水平非均匀加热与能量频散[J]. 大气科学, 25 (3): 317-328. Liu Yimin, Wu Guoxiong, Yu Rucong, et al. 2001. Thermal adaptation overshooting, dispersion, and subtropical anticyclone. Part II: Horizontal inhomogeneous heating and energy dispersion[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 25 (3): 317-328.
[7]
He Jinhai, Wen Min, Wang Lijuan, et al. 2006. Characteristics of the onset of the Asian summer monsoon and the importance of Asian-Australian "Land Bridge"[J]. Adv. Atmos. Sci., 23 (6): 951-963.
[8]
Huang Gang, Qu Xia, Hu Kaiming. 2011. The impact of the tropical Indian ocean on South Asian high in boreal summer[J]. Adv. Atmos. Sci., 28 (2): 421-432.
[9]
Huang Ronghui, Chen Jilong, Wang Lin, et al. 2012. Characteristics, processes, and causes of the spatio-temporal variabilities of the East Asian monsoon system[J]. Adv. Atmos. Sci., 29 (5): 910-942.
[10]
Kalnay E C, Kanamitsu M, Kistler R, et al. 1996. The NCEP/NCAR 40-year reanalysis project[J]. Bull. Amer. Meteor. Soc., 77 (3): 437-472.
[11]
李崇银, 李琳, 谭言科. 2011. 南亚高压在平流层的特征及ENSO 影响的进一步研究[J]. 热带气象学报, 27 (3): 289-298. Li Chongyin, Li Lin, Tan Yanke. 2011. Further study on structure of South Asia high in the stratosphere and influence of ENSO[J]. Journal of Tropical Meteorology (in Chinese), 27 (3): 289-298.
[12]
刘伯奇, 何金海, 王黎娟. 2009. 4~5月南亚高压在中南半岛上空建立过程特征及其可能机制[J]. 大气科学, 33 (6): 1319-1332. Liu Boqi, He Jinhai, Wang Lijuan. 2009. Characteristics of the South Asia high establishment processes above the Indo-China Peninsula from April to May and their possible mechanism[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 33 (6): 1319-1332.
[13]
刘四臣, 李维亮. 1987. 热力强迫下斜压大气的多平衡态与副热带高压[J]. 中国科学(B辑),9 (4): 441-450. Liu Sichen, Li Weiliang. 1987. Multi-equilibrium and subtropical high pressure of the baroclinic under the heating force[J]. Science in China (Series B) (in Chinese), 9 (4): 441-450.
[14]
Liu Yimin, Bao Qing, Duan Anmin, et al. 2007a. Recent progress in the impact of the Tibetan Plateau on climate in China[J]. Adv. Atmos. Sci., 24 (6): 1060-1076.
[15]
Lu Riyu. 2004. Associations among the components of the East Asian summer monsoon system in the meridional direction[J]. J. Meteor. Soc. Japan, 82 (1): 155-165.
[16]
Mason R B, Anderson C E. 1958. The development and decay of the 100 mb summertime anticyclone over southern Asia[J]. Mon. Wea. Rev., 91 (1): 3-12.
[17]
Qian Yongfu, Zhang Qiong, Yao Yonghong, et al. 2002. Seasonal variation and heat preference of the South Asia high[J]. Adv. Atmos. Sci., 19 (5): 821-836.
[18]
谭晶, 杨辉, 孙淑清, 等. 2005. 夏季南亚高压东西振荡特征研究[J]. 南京气象学院学报, 28 (4): 452-460. Tan Jing, Yang Hui, Sun Shuqing, et al. 2005. Characteristics of the longitudinal oscillation of South Asia high during summer[J]. Journal of Nanjing Institute of Meteorology (in Chinese), 28 (4): 452-460.
[19]
王黎娟, 郭帅宏. 2012. 4~5月南亚高压在中南半岛上空建立的年际变化特征及其与亚洲南部夏季风的关系[J]. 大气科学学报, 35 (1): 10-23. Wang Lijuan, Guo Shuaihong. 2012. 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]. Transactions of Atmospheric Sciences (in Chinese), 35 (1): 10-23.
[20]
魏维, 张人禾, 温敏. 2012. 南亚高压的南北偏移与我国夏季降水的关系[J]. 应用气象学报, 23 (6): 650-659. Wei Wei, Zhang Renhe, Wen Min. 2012. Meridional variation of South-Asian high and its relationship with the summer precipitation over China[J]. Journal of Applied Meteorological Science (in Chinese), 23 (6): 650-659.
[21]
吴国雄, 刘还珠. 1999. 全型垂直涡度倾向方程和倾斜涡度发展[J]. 气象学报, 57 (1): 1-15. Wu Guoxiong, Liu Huanzhu. 1999. Complete form of vertical vorticity tendency equation and slantwise vorticity development[J]. Acta Meteorologica Sinica (in Chinese), 57 (1): 1-15.
[22]
吴国雄,刘屹岷. 2000.热力适应、过流、频散和副高 I.热力适应和过流[J].大气科学,24(4): 433-446. Wu Guoxiong,Liu Yimin. 2000. Thermal adaptation,overshooting,dispersion and subtropical high. Part I: Thermal adaptation and overshooting[J]. Chinese Journal of Atmospheric Sciences (in Chinese),24(4): 433-446.
[23]
Wu Guoxiong, Liu Yimin. 2003. Summertime quadruplet heating pattern in the subtropics and the associated atmospheric circulation[J]. Geophys. Res. Lett., 30 (5): 1201-1204. doi:10.1029/2002GL016209.
[24]
吴国雄, 刘屹岷, 刘平. 1999. 空间非均匀加热对副热带高压带形成和变异的影响 I: 尺度分析[J]. 气象学报, 57 (3): 257-263. Wu Guoxiong, Liu Yimin, Liu Ping. 1999. The effect of spatially nonuniform heating on the formation and variation of subtropical high. Part I: Scale analysis[J]. Acta Meteorologica Sinica (in Chinese), 57 (3): 257-263.
[25]
吴国雄,刘屹岷,宇婧婧,等. 2008.海陆分布对海气相互作用的调控和副热带高压的形成[J].大气科学,32(4): 720-740. Wu Guoxiong,Liu Yimin,Yu Jingjing,et al. 2008. Modulation of land-sea distribution on air-sea interaction and the formation of subtropical anticyclones[J]. Chinese Journal of Atmospheric Sciences (in Chinese),32(4): 720-740.
[26]
吴国雄, 段安民, 刘屹岷, 等. 2013. 关于亚洲夏季风爆发的动力学研究的若干近期进展[J]. 大气科学, 37 (2): 211-228. Wu Guoxiong, Duan Anmin, Liu Yimin, et al. 2013. Recent advances in the study on the dynamics of the Asian summer monsoon onset[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 37 (2): 211-228.
[27]
Yanai M, Esbensen S, Chu J H. 1973. Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets[J]. J. Atmos. Sci., 30 (4): 611-627.
[28]
Zhao Ping, Zhang Xiangdong, Li Yuefeng, et al. 2009. Remotely modulated tropical-North Pacific ocean-atmosphere interactions by the South Asian high[J]. Atmos. Res., 94 (1): 45-60.
[29]
Zhu Congwen, Zhou Xiuji, Zhao Ping, et al. 2011. Onset of East Asian sub-tropical summer monsoon and rainy season in China[J]. Sci. China Earth Sci., 54 (12): 1845-1853. doi:10.1007/s11430-011-4284-0.
[30]
朱福康, 陆龙骅, 陈咸吉, 等. 1980. 南亚高压[M]. 北京: 科学出版社, 78pp. Zhu Fukang, Lu Longhua, Chen Xianji, et al. 1980. The South Asian high (in Chinese)[M]. Beijing: Science Press, 78pp.
