[1] Zhou T J, Yu R C. Atmospheric water vapor transport associated with typical anomalous summer rainfall patterns in China[J]. Journal of Geophysical Research,2005,110: D08104, doi:10.1029/2004JD005413.
[2] Ding yihui. Water Vapor Budget in Monsoon Area: Asia Monsoon[M]. Beijing: Meteorological Press, 1994:105-133.[丁一汇.季风区的水汽收支:亚洲季风[M].北京:气象出版社,1994:105-113.]
[3] Li W P. Moisture flux and water balance over the South China Sea during late boreal spring and summer[J]. Theoretical and Applied Climatology,1999,64:179-187.
[4] Peixoto J P, Oort A H. Physics of Climate[M]. New York: American Institute of Physics Press, 1992.[吴国雄等译.气候物理学[M].北京:气象出版社,1995.]
[5] Ganachaud A, Wunsch C. Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data[J]. Nature, 2000, 408(23):453-457.
[6] Wu Guoxiong, Chou Jifan, Liu Yimin, et al. Dynamics of the Formation and Variation of Subtropical Anticyclone[M].Beijing: Science Press,2002:314.[吴国雄,丑纪范,刘屹岷,等.副热带高压形成和变异的动力学问题[M].北京:科学出版社,2002:314.]
[7] Zhang Qiong, Liu Ping, Wu Guoxiong. SST in Indian Ocean and the Southern China Ocean and the drought/flood in Yangtz regions[J]. Chinese Journal of Atmospheric Sciences,2003,27(6):992-1 005.[张琼,刘平,吴国雄.印度洋和南海海温与长江流域旱涝[J].大气科学,2003,27(6):992-1 005.]
[8] Chen Guanghua, Huang Ronghui. The effect of warm pool thermal states on tropical cyclone in West Northwest Pacific[J]. Journal of Tropical Meteorology,2006,22(6):in press.[陈光华, 黄荣辉.西北太平洋暖池热状态对热带气旋活动的影响[J].热带气象学报,2006,22(6):待刊.]
[9] Yu W, Xiang B, Liu L,et al. Understanding the origins of interannual thermocline variations in the tropical Indian Ocean[J]. Geophysical Research Letters,2005,32:L24706, doi:10.1029/2005GL024327.
[10] Wang B, Ding Q, Fu X, et al. Fundamental channenge in simulation and prediction of summer monsoon rainfall[J]. Geophysical Research Letters,2005,32:L15711, doi: 10.1029/2005GL022734.
[11] Flohn H. Large-scale aspects of the "summer monsoon" in South and East Asia[J]. Journal of Meteorological Society of Japan,1957,35:180-186.
[12] Wu Guoxiong, Zhang Yongshen. Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea[J]. Monthly Weather Review,1998,126:913-927.
[13] Liu Y M, Chan J C L, Mao J Y, et al. The role of Bay of Bengal Convection in the onset of the 1998 South China Sea summer monsoon[J]. Monthly Weather Review,2002,130: 2 731-2 744.
[14] Wu GuoXiong, Meng Wen. The gear-like coupling of air-sea systems between equatorial Indian and Pacific Ocean[J]. Chinese Journal of Atmospheric Sciences,1998,22(4):470-480.[吴国雄,孟文.赤道印度洋—太平洋地区海气系统的齿轮式耦合和ENSO事件[J].大气科学,1998,22(4):470-480.]
[15] Li T, Wang B, Chang C P. Theories on the Tropospheric Biennial Oscillation: A Review[C]∥IAP/Academia Sinica,ed. Dynamics of Atmospheric General Circulation and Climate. Beijing: China Meteorological Press, 2001:252-276.
[16] Wang B, Wu R, Lau K M. Interannual variability of Asian summer monsoon: Contrast between the Indian and Western North Pacific-East Asian monsoons[J]. Journal of Climate,2001,14:4 073-4 090.
[17] Committee on Strategic Guidance for NSF's Support of the Atmospheric Sciences National Research Council. Strategic Guidance for the National Science Foundation's Support of the Atmospheric Sciences: An Interim Report[M/OL].http://www.nap.edu/catalog/11454.html
[18] World Meteorology Organization. The World Climate Research Programme Strategic Framework 2005-2015: Coordinated Observation and Prediction of the Earth System (COPES), 2005. [R/OL]. http://www.wmo.ch/web/wcrp/pdf/WCRP-strateg Imple_Low Res.pdf,2005.[李建平,刘屹岷,等.世界气候研究计划2005—2015年战略框架[M].北京:气象出版社,2006.]
[19] Huang Ronghui, Li Chongyin, Wang Shaowu, et al. On the Major Climate Disasters and Their Formation[M]. Beijing:Meteoralogy Press, 2003.[黄荣辉,李崇银,王绍武,等.我国旱涝重大的气候灾害及其形成机理研究[M].北京:气象出版社,2003.]
[20] Li Weiping, Wu Guoxiong, Liu Yimin, et al. How the surface processes over the Tibetan Plateau affect the summertime Tibetan Anticyclone: Numerical experiments [J]. Chinese Journal of Atmospheric Sciences, 2001, 25(6):809-816.[李伟平,吴国雄,刘屹岷,等.青藏高原表面过程对
夏季青藏高压的影响:数值试验[J].大气科学,2001,25(6): 809-816.]
[21] Liu Xin, Wu Guoxiong, Li Weiping, et al. Thermal adaptation of the large-scale circulation to the summer heating over the Tibetan plateau[J]. Progress in Natural Science,2001,11(3): 33-39.[ 刘新,吴国雄,李伟平,等.夏季青藏高原加热和大尺度流场的热力适应[J].自然科学进展,2000,11(3):33-39.]
[22] Zhang Xuehong, Shi Guangyu, Liu Hui, et al. IAP Global Ocean-Atmosphere-Land System Model[M].Beijing, New York:Science Press, 2000:252.
[23] Duan A M, Wu G X. Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia[J]. Climate Dynamics, 2005, 24:793-807.
[24] Qiao F, Yuan Y, Yang Y, et al. Wave-induced mixing in the upper ocean: Distribution and application in a global ocean circulation model[J]. Geophysical Research Letter,2004,31:L11303,doi:10.1029/2004GL019824.
[25] Wu Guoxiong, Li Jianping, et al. Air-sea-land Interactions in Asia Monsoon Region and their Impacts on the Climate Variation in China[M].Beijing: Meteorology Press,2005.[吴国雄,李建平,等.亚洲季风区海—陆—气相互作用对我国气候变化的影响[M].北京:气象出版社,2005.]
[26] Hu D, Pang Chongguang. Reexamination of the role of vertical circulation in sedimentation in the Yellow and East China seas[J]. Journal of Hydrodynamics, 2001,13:115-121.
|