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[1]宋美洋,顾建峰,刘海文,等.重庆夏季低涡无暴雨的气候学分析[J].成都信息工程大学学报,2016,(04):413-418.
 SONG Mei-Yang,GU Jian-feng,LIU Hai-wen,et al.The Summery without Heavy Rainfall Climatic Characteristics Associated with the Mesocale Low Vortex over Chongqing[J].Journal of Chengdu University of Information Technology,2016,(04):413-418.
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重庆夏季低涡无暴雨的气候学分析

参考文献/References:

[1] 刘红武, 李国平. 近三十年西南低涡研究的回顾与展望[J]. 高原山地气象研究, 2008,(2):68-73.
[2] 李国平. 高原涡、西南涡研究的新进展及有关科学问题[J]. 沙漠与绿洲气象, 2013,(3):1-6.
[3] 何光碧. 西南低涡研究综述[J]. 气象, 2012, 38(2):155-163.
[4] Tao, S Y. The Heavy Rainfalls in China[M]. Science Press, 1980:225.
[5] Lu, J H. Introduction to the Southwest Vortices[M]. Meteorological Press,1986:276.
[6] Chen Z M, Xu M, Min W B, et al. Relationship between abnormal activities of southwest vortex and heavy rain the upper reach of Yangtze River during summer of 1998[J]. Plateau Meteorology, 2003, 22(2): 162-167.
[7] Chen T, Zhang F, Duan Y. A study of relationship between a southwest vortex and themesoscale convective system during the severe ‘6.12' rainstorm event in Guangxi Province. Acta Meteorol[J]. 2011, 69(3): 472-485.
[8] Kuo Y, Cheng L, Bao J. Numerical simulation of the 1981 Sichuan flood. Part I: evolution of a mesoscale southwest vortex. Monthly Weather Review[J].1998,116:2481-2504.
[9] Chen S J, Dell'Osso L. Numerical prediction of the heavy rainfall vortex over eastern Asia monsoon region[J]. Journal of the Meteorological Society of Japan, 1984, 62(5):730-747.
[10] Wang B, Orlanski I. Study of a heavy rain vortex formed over the eastern flank of the Tibetan Plateau[J]. Monthly Weather Review, 1987,115(7):1370-1393
[11] Wang W, Kuo Y H, Warner T T. A diabatically driven mesoscale vortex in the lee of the Tibetan Plateau[J]. Monthly weather review, 1993, 121(9): 2542-2561.
[12] Fu S, Sun J, Zhao S, et al. The energy budget of a southwest vortex with heavy rainfall over south China[J]. Advances in Atmospheric Sciences, 2011, 28(3): 709-724.
[13] Li J, Du J, Zhang D L, et al. Ensemble‐based analysis and sensitivity of mesoscale forecasts of a vortex over southwest China[J]. Quarterly Journal of the Royal Meteorological Society, 2014, 140(680): 766-782.
[14] 陶诗言. 中国之暴雨[M]. 北京:科学出版社, 1980, 225.
[15] 卢敬华. 西南低涡概论[M]. 北京:气象出版社, 1986:263.
[16] 乔全明,张雅高. 青藏高原天气学[M].北京:气象出版社,1994:156.
[17] 蒋璐君, 李国平, 母灵,等. 基于TRMM资料的西南涡强降水结构分析[J]. 高原气象, 2014, 33(3).
[18] 赵思雄, 傅慎明. 2004年9月川渝大暴雨期间西南低涡结构及其环境场的分析[J]. 大气科学, 2007, 31(6):1059-1075.
[19] 刘晓冉, 李国平.一次东移型西南低涡的数值模拟及位涡诊断[J]. 高原气象,2014,33(5).
[20] 孙婕, 李国平. 西南低涡东移引发重庆暴雨的综合诊断[J]. 高原山地气象研究, 2013,(2):10-17.
[21] 翟丹华,刘德,李强,等. 引发重庆中西部暴雨的西南低涡特征分析[J]. 高原气象,2014,33(1):140-147
[22] 张飒,程相坤.造成山东不同天气的两个西南低涡异同分析[J].气象,1998,24(1):20-24.
[23] 石鹏祥,刘海文.影响重庆夏季暴雨的中尺度低涡的气候学特征[J].成都信息工程大学学报,2016,(3).
[24] 丁一汇. 天气动力学中的诊断分析方法[M]. 北京:科学出版社, 1989:293.
[25] 伍荣生. 现代天气学原理[M].北京:高等教育出版社,1999:319.
[26] Uccellini L W, Johnson D R.The Coupling of Upper and Lower Tropospheric Jet Streaks and Implications for the Development of Severe Convective Storms[J]. Mon.wea.rev, 1979, 107:682-703.
[27] 丁一汇. 高等天气学[M]. 北京:气象出版社, 2005:139.
[28] 刘海文, 丁一汇. 华北汛期大尺度降水条件的年代际变化[J]. 大气科学学报, 2011, 34(2):146-152.

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备注/Memo

收稿日期:2015-12-21 基金项目:重庆市气象局开放式研究基金资助项目(KFJJ-201102); 重庆市博士后科研资助项目(渝xm201103028)

更新日期/Last Update: 2016-03-30