乔全明,张雅高.青藏高原天气学.北京:气象出版社,1994.120~155Qiao Quanming,Zhang Yagao.Synoptic Meteorology of Qinghai-Xizang Plateau (in Chinese).Beijing:China Meteorological Press,1994.120~155
[3]
杨克明,毕宝贵,李月安,等.1998年长江上游致洪暴雨的分析研究.气象,2001,27(8):9~14Yang Keming,Bi Baogui,Li Yue\'an,et al.On flood-causing torrential rainfall in the upstream district of Changjiang River in 1998.Meteorological Monthly (in Chinese),2001,27(8):9~14
[4]
Kevin W,Watterson I G.Tropical cyclone-like vortices (TCLV) in a limited area mode-comparison with observed climatology.J.Climate,1997,10:2240~2259
[5]
高守亭.流场配置及地形对西南低涡形成的动力作用.大气科学,1987,11(3):263~271Gao Shouting.The dynamic action of the disposition of the fluid fields and the topography on the formation of the south-west vortex.Chinese Journal of Atmospheric Sciences (Scientia Atmospherica Sinica) (in Chinese),1987,11(3):263~271
[6]
盛华,陶诗言.青藏高原和落基山对气旋的动力影响,气象学报,1988,46(2):130~141Sheng Hua,Tao Shiyan.Dynamic effect of Qnghai-Xizang and Rocky Mountains onthelee cyclones.Acta Meteorologica Sinica(in Chinese),1988,46(2):130~141
[7]
李国平.青藏高原动力气象学.北京:气象出版社,2002.135~193Li Guoping.Dynamic Meteorology of the Tibetan Plateau(in Chinese).Beijing:China Meteorological Press,2002.135~193
[8]
高守亭.行星边界层内低涡的环流结构.气象学报,1983,41(3):285~295Gao Shouting.The circulation structure of the vortex within the planet boundary layer.Acta Meteorologica Sinica(in Chinese),1983,41(3):285~295
[9]
周明煜,徐祥德,卞林根,等.青藏高原大气边界层观测分析与动力学研究.北京:气象出版社,2000.57~78Zhou Mingyu,Xu Xiangde,Bian Lingen,et al.Observational Analysis and Dynamic Study of Atmospheric Boundary Layer on Tibetan Plateau (in Chinese).Beijing:China Meteorological Press,2000.57~78
[10]
陈陟,周明煜,钱粉兰,等.我国西部高原大气边界层中的对流活动.应用气象学报,2002,13(2):142~155Chen Zhi,Zhou Mingyu,Qian Fenlan,et al.Convective activities in the atmospheric boundary layer over the plateau in western China.Journal of Applied Meteorological Science (in Chinese),2002,13(2):142~155
[11]
江吉喜,范梅珠.夏季青藏高原上的对流云和中尺度对流系统.大气科学,2002,26(20):263~270Jiang Jixi,Fan Meizhu.Convective clouds and mesoscale convective systems over the Tibetan Plateau in summer.Chinese Journal of Atmospheric Sciences (in Chinese),2002,26(20):263~270
[12]
过仲阳,林珲,江吉喜,等.青藏高原上中尺度对流系统东移传播成因.地球信息科学,2003,5(1):5~10Guo Zhongyang,Lin Hui,Jiang Jixi,et al.Mining eastwardmoving MCSs features over the Tibetan Plateau.Geo-Information Sciences (in Chinese),2003,5(1):5~10
[13]
Gray S L,Craig G C.A simple theoretical model for the intensification of tropical cyclones and polar lows.Quart.J.Roy.Meteor.Soc.,1998,124:919~947
[14]
李国平,赵邦杰,卢敬华.青藏高原地面总体输送系数的研究.气象学报,2002,60(1):60~67Li Guoping,Zhao Bangjie,Lu Jinghua.Characteristics of bulk transfer coefficients over the Tibetan Plateau.Acta Meteorologica Sinica (in Chinese),2002,60(1):60~67
[15]
李国平,赵邦杰,杨锦青.地面感热对青藏高原低涡流场结构及发展的作用.大气科学,2002,26(4):519~525Li Guoping,Zhao Bangjie,Yang Jinqing.A dynamical study of the role of surface sensible heating in the structure and intensification of the Tibetan Plateau vortices.Chinese Journal of Atmospheric Sciences (in Chinese),2002,26(4):519~525