Akiyama T. 1989. Large, synoptic and mesoscale variations of the Baiu front during July 1982. Part Ⅰ: Cloud features [J]. J. Meteor. Soc. Japan, 67: 57-81.
[2]
贝耐芳, 赵思雄. 2002. 1998年 “二度梅” 期间突发强暴雨系统的中尺度分析 [J]. 大气科学, 26 (4): 526-540. Bei Naifang, Zhao Sixiong. 2002. Mesoscale analysis of severe local heavy rainfall during the second stage of the 1998 Meiyu season [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 26 (4): 526-540.
[3]
Chen S J, Kuo Y H, Wang W, et al. 1997. A modeling case study of heavy rainstorms along the Meiyu front [J]. Mon. Wea. Rev., 126: 2330-2351.
[4]
Cho H R, Chan D. 1991. Meso-β-scale potential vorticity anomalies and rainbands. Part II: Moist model simulation [J]. J. Atmos. Sci., 48 (2): 331-341.
[5]
Ding Y H. 1992. Summer monsoon rainfall in China [J]. J. Meteor. Soc. Japan, 70: 373-396.
[6]
董佩明, 赵思雄. 2004a. 引发梅雨锋暴雨的频发型中尺度低压(扰动)的诊断研究 [J]. 大气科学, 28 (6): 876-891. Dong Peiming, Zhao Sixiong. 2004a. A diagnostic study of mesoscale lows (disturbances) on Meiyu front and associated heavy rainfall [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 28 (6): 876-891.
[7]
董佩明, 赵思雄. 2004b. 梅雨锋两类中尺度低压(扰动)及其暴雨的数值研究 [J]. 气候与环境研究, 9 (4): 641-657. Dong Peiming, Zhao Sixiong. 2004b. A numerical study of two kinds of mesoscale low (disturbance) on Meiyu front and associated heavy rainfall [J]. Climatic and Environmental Research (in Chinese), 9 (4): 641-657.
[8]
高坤, 徐亚梅. 2001. 1999年6月下旬长江中下游梅雨锋低涡扰动的结构研究 [J]. 大气科学, 25 (6): 740-755. Gao Kun, Xu Yamei. 2001. A simulation study of structure of mesovortexes along Meiyu front during 22-30 June 1999 [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 25 (6): 740-755.
[9]
高守亭, 孙淑清. 1984. 次天气尺度低空急流的形成 [J]. 大气科学, 8 (2): 178-188. Gao Shouting, Sun Shuqing. 1984. The forming of subsynoptic scale low-level jet stream [J]. Chinese Journal of Atmospheric Sciences (Scientia Atmospherica Sinica) (in Chinese), 8 (2): 178-188.
[10]
谷文龙. 2008. 长江下游梅雨锋中尺度涡旋统计分析与模拟研究 [D]. 南京信息工程大学硕士论文. Gu Wenlong. 2008. Statistical and simulative analysis of mesoscale vortexes on Meiyu front over lower reaches of Yangtze River [D]. M.S. thesis (in Chinese), Nanjing University of Information Science and Technology.
[11]
Hoskins B J. 1974. The role of potential vorticity in symmetric stability and instability [J]. Quart. J. Roy. Metor. Soc., 100: 180-182.
[12]
胡伯威,潘鄂芬. 1996.梅雨期长江流域两类气旋性扰动和暴雨 [J].应用气象学报,7(2): 138-144. Hu Bowei,Pan Efen. 1996. Two kinds of cyclonic disturbances and their accompanied heavy rain in the Yangtze River valley during the Mei-yu period [J]. Journal of Applied Meteorological Science (in Chinese),7(2): 138-144.
[13]
李鲲, 徐幼平, 宇如聪, 等. 2005. 梅雨锋上三类暴雨特征的数值模拟比较研究 [J]. 大气科学, 29 (2): 236-248. Li Kun, Xu Youping, Yu Rucong, et al. 2005. Comparative studies of three types of heavy rainstorms associated with the Meiyu front by numerical simulations [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 29 (2): 236-248.
[14]
李毓芳, 黄安丽, 高坤, 等. 1986. 对流加热在梅雨暴雨系统中的作用 [J]. 中国科学 (B辑), (7): 765-775. Li Yufang, Huang Anli, Gao Kun. 1986. The role of convective heating in heavy rain system during Mei-rains season [J]. Scentia Sinica (Series B) (in Chinese), (7): 765-775.
[15]
隆霄, 程麟生. 2004. “99×6” 梅雨锋暴雨低涡切变线的数值模拟和分析 [J]. 大气科学, 28 (3): 342-356. Long Xiao, Chen Linsheng. 2004. Numerical simulation and analysis for “99×6” Meiyu front rainstorm and the low vortex with shear line [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 28 (3): 342-356.
[16]
Moteki Q, Uyeda H, Masesaka T, et al. 2004. Structure and development of two merged rainbands observed over the East China Sea during X-BAIU-99. Parts II: Meso-a-scale structure and build-up processes of convergence in the Baiu frontal region [J]. J. Meteor. Soc. Japan, 82 (1): 45-65.
[17]
倪允琪, 周秀骥. 2004. 中国长江中下游梅雨锋暴雨形成机理以及监测与预测理论和方法研究 [J]. 气象学报, 62 (5): 645-661. Ni Yunqi, Zhou Xiuji. 2004. Study for formation mechanism of heavy rainfall within the Meiyu front along the middle and downstream of Yangtze River and theories and methods of their detection and prediction [J]. Acta Meteorologica Sinica (in Chinese), 62 (5): 645-661.
[18]
Ninomiya K. 1984. Characteristics of Baiu front as a predominant subtropical front in the summer Northern Hemisphere [J]. J. Meteor. Soc. Japan, 62: 880-894.
[19]
Shen H F, Zhai G Q, Zhu Y, et al. 2012. Numerical study of a mesoscale vortex in the planetary boundary layer of the Meiyu front [J]. Acta Meteorologica Sinica, 26 (6): 788-802.
[20]
孙建华, 张小玲, 齐琳琳, 等. 2004. 2002年6月20～24日梅雨锋中尺度对流系统发生发展分析 [J]. 气象学报, 62 (4): 423-438. Sun Jianhua, Zhang Xiaoling, Qi Linlin, et al. 2004. Analysis on MCSs in Meiyu front during 20-24 June 2002 [J]. Acta Meteorologica Sinica (in Chinese), 62 (4): 423-438.
[21]
孙晶. 2011. 梅雨锋暴雨中尺度对流系统研究若干进展 [J]. 气象科技, 39 (3): 257-265. Sun Jin. 2011. Advances in researches on meso-scale convective systems related to Meiyu heavy rainfall [J]. Meteorological Science and Technology (in Chinese), 39 (3): 257-265.
[22]
孙淑清. 1990. 梅雨锋中大振幅重力波的活动及其与环境场的关系 [J]. 大气科学, 14 (2): 163-172. Sun Shuqing. 1990. Activities of inertia-gravitational waves in bai-u front and their interaction with background field [J]. Chinese Journal of Atmospheric Sciences (Scientia Atmospherica Sinica) (in Chinese), 14 (2): 163-172.
[23]
孙淑清, 翟国庆. 1980. 低空急流的不稳定性及其对暴雨的触发作用 [J]. 大气科学, 4 (4): 327-337. Sun Shuqing, Zhai Guoqing. 1980. On the instability of the low level jet and its trigger function for the occurrence of heavy rain-storms [J]. Chinese Journal Atmospheric Sciences (Scientia Atmospherica Sinica) (in Chinese), 4 (4): 327-337.
[24]
陶诗言. 1980. 中国之暴雨 [M]. 北京: 科学出版社, 225pp. Tao Shiyan. 1980. Heavy Rainfalls in China (in Chinese) [M]. Beijing: Science Press, 225pp.
[25]
陶诗言, 倪允琪, 赵思雄, 等. 2001. 1998年夏季中国暴雨的形成机理与预报研究 [M]. 北京: 气象出版社, 184pp. Tao Shiyan, Ni Yunqi, Zhao Sixiong, et al. 2001. The Study on Formation Mechanisms and Forecasting of Heavy Rainfall in the Summer 1998 (in Chinese) [M]. Beijing: China Meteorological Press, 184pp.
[26]
张凤, 赵思雄. 2003. 梅雨锋上引发暴雨的低压动力学研究 [J]. 气候与环境研究, 8(2): 143-156. Zhang Feng, Zhao Sixiong. 2003. A dynamic study of one kind of Meiyu front lows producing heavy rainfall [J]. Climatic and Environmental Research (in Chinese), 8 (2): 143-156.
[27]
张小玲, 陶诗言, 张顺利. 2004. 梅雨锋上的三类暴雨 [J]. 大气科学, 28 (2): 187-205. Zhang Xiaoling, Tao Shiyan, Zhang Shunli. 2004. Three types of heavy rainstorms associated with the Meiyu front [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 28 (2): 187-205.
[28]
Zhao S X, Li Z J. 1990. A case study on the frontogenesis and conditional symmertrical instability in China [C] // The second US-PRC Joint Mesoscale Meteorology Workshop, NCAR, Boulder, Colorado, U. S. A, 38-39.
[29]
赵思雄, 陶祖钰, 孙建华, 等. 2004. 长江流域梅雨锋暴雨机理的分析研究 [M]. 北京: 气象出版社, 281pp. Zhao Sixiong, Tao Zuyu, Sun Jianhua, et al. 2004. Study on the Mechanism of the Formation and Development of Heavy Rainfall on the Meiyu Front in Yangtze River (in Chinese) [M]. Beijing: China Meteorology Press, 281pp. 朱乾根, 林锦瑞, 寿绍文, 等. 2000. 天气学原理与方法(第三版) [M]. 北京: 气象出版社, 1-649. Zhu Qianggen, Lin Jinrui, Shou Shaowen, et al. 2002. Synoptic Meteorological Analysis (3rd ed.) (in Chinese) [M]. Beijing: China Meteorological Press.
[30]
翟国庆, 王智, 何斌. 2003. 长江中下游梅雨期中小尺度涡旋族发生演变分析 [J]. 气象学报, 61 (6): 661-671. Zhai Guo Qing, Wang Zhi, He Bin. 2003. Formation and evolution analysis of the mesoscale vortex group in the middle and lower reaches during Meiyu of the Yangtze River [J]. Acta Meteorologica Sinica (in Chinese), 61 (6): 661-671.
[31]
Zhai G Q, Zhou L L, Wang Z. 2007. Analysis of a group of weak small-scale vortexes in the planetary boundary layer in the Meiyu front [J]. Adv. Atmos. Sci., 24 (3): 399-408.
