Vol.17, NO.6, 2006
Turn off MathJax
Article Contents
Article Navigation >  Journal of Applied Meteorological Science  > 2006  >  17(6): 711-724
Chen Longxun, Zhang Bo, Zhang Ying. Progress in research on the East Asian monsoon. J Appl Meteor Sci, 2006, 17(6): 711-724.
Citation: Chen Longxun, Zhang Bo, Zhang Ying. Progress in research on the East Asian monsoon. J Appl Meteor Sci, 2006, 17(6): 711-724.
shu

Progress in Research on the East Asian Monsoon

  • Chinese Academy of Meteorological Sciences, Beijing 100081

  • Received Date: 2006-11-13
  • Rev Recd Date: 2006-11-27
  • Publish Date: 2006-12-31
    Abstract
  • Chinese Academy of Meteorological Sciences (CAMS) has organized the investigation on the East Asian Monsoon with its influences on the weather and drought/flood in China for a long term since the foundation of new China. A summary of the achievements of the past researches by CAMS is briefly depicted. A basic review of the East Asian Monsoon researches in China after 1950s; the study on the East Asian Monsoon circulation system (EAMCS): the history of proposals to EAMCS affecting the weather and climate in China, the interactions between East Asian and Indian Monsoon system, the water vapour transportation resulting in the torrential rain in China, and the design of the monsoon index representing the East Asian Monsonn activity are set forth. The seasonal variation of EAMCS is summarized on the onset of the South China Sea Summer Monsoon, Meiyu and the rainy season in China and its propagation. The Madden-Julian oscillation (MJO) of EAMCS and its impacts on the summer precipitation in China are presented by the study on the characteristics of zonal and meridional propagation of the subtropical MJO of EAMCS, the differences between it and that on the Equatorial area, and its possible effects on the formation of El Niño, the onset of East Asian tropical and subtropical monsoon and the weather and climate in China. The calculation and distribution of atmosphere apparent heat source in Asia, and its possible influence on the East Asian Summer Monsoon and the rainfall, and the possible influence of the winter cold source over the Tibetan Plateau on the formation of El Niño are given. The inter-annual and interdecadal variation of the EAMCS are reviewed on the characteristics of the inter-annual variation of the EAMCS and the rainfall, the analysis of the quasi-4-year oscillation, the interaction between it and the formation of El Niño, the impact of the polar region on the summer rainfall in East Asia, and the inter-decadal variation of the EAMCS. The possible mechanism of the formation of the EAMCS is proposed, especially the essential role in the formation of summer and winter monsoon, the EAMCS and the Indian Monsson system of the land-sea thermal difference between the Asian continent and the West Pacific, the African continent, the Indian and IndoChina peninsula, Australian continent, and the ocean and sea around them.
    • FullText(HTML)
    References(126)
  • [1]
    Yeh Tucheng, staff member of Academia Sinica.On the General circulation over the Eastern Asia (Ⅰ).Tellus, 1957, 9:432-446. doi:  10.1111/j.2153-3490.1957.tb01903.x/abstract
    [2]
    Yeh Tucheng, staff member of Academia Sinica.On the general circulation over the Eastern Asia (Ⅱ).Tellus, 1958, 10:58-75.
    [3]
    Dao Shihyen, Chen Lungshun.The structure of general circulation over continent of Asia in Summer.J Meteor Soc Japan, 1957:215-229. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXB195703005.htm
    [4]
    Yeh Tuchang, Dao Shihyen, Li Maicun. The Abrupt Change of Circulation over the Northern Hemisphere During June and October∥The Atmosphere and Sea in Motion. New York:The Rockefelher Institute Press in Association with Oxford University Press, 1959:246-267.
    [5]
    《会议文集》编辑组.全国热带夏季风学术会议文集.昆明:云南人民出版社, 1981.
    [6]
    《会议文集》编辑组.全国热带夏季风学术会议文集.昆明:云南人民出版社, 1982.
    [7]
    陈隆勋, 朱乾根, 罗会邦, 等.东亚季风.北京:气象出版社, 1991.
    [8]
    国家气象局气象科学研究院.气象科学技术集刊 (10) (季风论文专集).北京:气象出版社, 1987:1-235.
    [9]
    国家气象局气象科学研究院.气象科学技术集刊 (11) (东亚夏季风).北京:气象出版社, 1987:1-142.
    [10]
    丁一汇, 陈隆勋, Murakami M.亚洲季风.北京:气象出版社, 1994:1-263.
    [11]
    何金海, 丁一汇, 陈隆勋.亚洲季风研究新进展.北京:气象出版社, 1996:1-231.
    [12]
    陈隆勋, 丁一汇, Murakami M, 等.亚洲季风机制研究新进展.北京:气象出版社, 1998:1-334.
    [13]
    陈隆勋, 金祖辉.夏季东亚季风环流系统内中期变化的南北半球相互作用∥《会议文集》编辑组.全国热带夏季风学术学术会议文集.昆明:云南人民出版社, 1982: 218-232.
    [14]
    金祖辉, 陈隆勋.夏季东亚季风环流系统的中期变化及其与印度季风环流系统的相互关系∥《会议文集》编辑组.全国热带夏季风学术会议文集.昆明:云南人民出版社, 1982: 204-218.
    [15]
    陈隆勋.东亚季风环流系统的结构及其中期变动.海洋学报, 1984, 6(4): 744-758. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198406003.htm
    [16]
    Chen Longxun, Jin Zuhui.The medium-range variations of the summer monsoon circulation system over East Asia.Adv Atmos Sci, 1984, 1: 224-233. doi:  10.1007/BF02678135
    [17]
    Tao Shiyan, Chen Longxun.The East Asian Summer Monsoon ∥Proceedings of International Conference on Monsoon in the Far East, Tokyo, 1985:1-11.
    [18]
    Tao Shiyan, Chen Longxun.A review on the East Asian Summer monsoon∥Krishnamurti, Chang C P.Monsoon Meteorology.Oxford: Oxford University Press, 1987: 60-92.
    [19]
    Chen Longxun, Gao Hui, He Jinhai, et al.Zonal propagation of kinetic energy and convection in the South China Sea and Indian monsoon regions in boreal summer.Science in China (Series D), 2004:47(12):1076-1084. doi:  10.1360/02yd0448
    [20]
    高辉, 陈隆勋, 何金海, 等.亚洲赤道地区大气动能的纬向传播.气象学报, 2005, 63(1):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200501002.htm
    [21]
    Chen Longxun, Song Yi, Masato Murakami. The Characteristics of Large Scale Convective System Variation During the Onset and Prevailing Periods of Summer Monsoon over the South China Sea and its Relation to the Air-sea Interaction, Part Ⅰ: The Characteristics of Convective System Change During the Onset Period of Summer Monson ∥Atmospheric Circulation to Global Change.Celebration of the 80th Birthday of Professor Ye Duzheng.Beijing : China Meteorological Press, 1996, 289-329.
    [22]
    Chen Longxun, Xie An.Westward propagation of low-frequency oscillations in the subtropics of eastern hemisphere and its remote correlation.Acta Meteorologica Sinica, 1988, 2(3):300-312.
    [23]
    田红, 郭品文, 陆维松.夏季水汽输送特征及其与中国降水异常关系.南京气象学院学报, 2002, 25(4): 496-502. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX200204008.htm
    [24]
    Liang Ping, Li Wei, Chen Longxun, et al. Features and sources of the anomalous moisture transport for the severe summer rainfall over the upper reaches of the Yangtze River.Acta Meteorologica Sinica, 2005, 19 (2): 202-215. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXW200502006.htm
    [25]
    祝从文, 何敏, 何金海.热带环流指数与夏季长江中下游旱涝的年际变化.南京气象学院学报, 1998, 21(1):15-224. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX801.002.htm
    [26]
    祝从文, 何金海, 吴国雄.东亚季风指数及其与大尺度热力环流年际变化关系.气象学报, 2000, 58(4):391-402. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200004001.htm
    [27]
    Wang Y F, Wang Bin, Jai-Ho Oh.Impact of preceding El Nino on the East Asian Summer Atmosphere Circulation.J Meteor Soc Japan, 2001, 79:575-588. doi:  10.2151/jmsj.79.575
    [28]
    王亚非, 张雁, 陈菊英.一个能反映梅雨现象的东亚夏季风指数.气候与环境研究, 2001, 6(2):147-152. http://www.cnki.com.cn/Article/CJFDTOTAL-QHYH200102001.htm
    [29]
    Sun Xiurong, Chen Longxun, He Jinhai.Interannal variation of index of East Asian land-sea thermal difference and its relation to monsoon circulation and rainfall over China.Acta Meteorologica Sinica, 2001, 15(1): 71-85.
    [30]
    赵平, 周自江.东亚副热带夏季风指数及其与降水的关系.气象学报, 2005, 63(6):933-941. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200506009.htm
    [31]
    赵平, 张人禾.东亚给太平洋偶极型气压场及其与东亚季风年际变化的关系.大气科学, 2006, 30(2):307-316. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200602012.htm
    [32]
    何金海, 温敏, 丁一汇, 等.亚澳"大陆桥"对流影响东亚夏季风建立的可能机制.中国科学 (D辑), 2006, 36(10): 959-967. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGQX200610003045.htm
    [33]
    丁一汇, 李崇银, 何金海, 等.南海季风试验与东亚夏季风.气象学报, 2004, 62(5):561-587. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200405005.htm
    [34]
    林之光.我国东部地区夏季风雨带进退规律的进一步研究∥国家气象局气象科学研究院.气象科学技术集刊 (10).北京:气象出版社, 1987:24-31.
    [35]
    林之光.我国西部地区夏季风雨季的进退∥国家气象局气象科学研究院.气象科学技术集刊 (11).北京:气象出版社, 1987:70-76.
    [36]
    Chen Longxun, Li Wei, Zhao Ping, et al.On the process of summer monsoon onset over East Asia.Acta Meteorologica Sinica, 2001, 15(4):436-449. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXW200104004.htm
    [37]
    Chen Longxun, Zhu Congwen. Characteristics and Mechanism Analysis of SCS Summer Monsoon Onset during SCSMEX in 1998∥Ding Yihui. Onset and Evolution of the South China Sea Monsoon and its Interaction with the Ocean. Beijing:China Meteorological Press, 1999:210-215.
    [38]
    陈隆勋, 刘洪庆, 王文, 等.南海及邻近地区夏季风爆发的特征及其机制的初步研究.气象学报, 1999: 57(1):16-29. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB901.001.htm
    [39]
    阎俊岳.南海西南风季风爆发的气候特征.气象学报, 1997, 55(2):174-186. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB702.004.htm
    [40]
    陈隆勋, 王予辉.南海和西太平洋暖池表面海温对东亚季风影响的数值模拟∥何金海, 丁一汇, 陈隆勋.亚洲季风研究新进展.北京:气象出版社, 1996:184-199.
    [41]
    陈隆勋, 刘洪庆, 王文, 等.南海及其邻近地区夏季风爆发的特征及其机制的初步研究.气象学报, 1999, 57(1):16-30. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB901.001.htm
    [42]
    Chen Longxun, Liu Hongqing, Wang Wen.Features of Monsoon onset over South China Sea and its Mechanisms∥Murakami M, Chen Longxun.Recent Progress in Studies of Asian Monsoon Mechanism (English edition).Science and Technology Agency of Japan, 1999:339-352.
    [43]
    Wang Yafei, Takahashi.A case study on the relationship between a preceding La Nina event and East Asian summer atmospheric circulation.Acta Meteor Sinica, 2004, 18(4):387-396. http://www.cqvip.com/QK/88418X/200404/3000621104.html
    [44]
    祝从文, 何金海, 谭言科.春夏季节转换中亚洲季风区副热带高压断裂特征及其可能机制分析.热带气象学报, 2004, 20(3):237-248. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200403001.htm
    [45]
    祝从文, 陈隆勋, 何金海.西太平洋副热带高压季节性东移与大尺度环流和温度场变化关系.热带气象学报, 2004, 20 (5) :334-345. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200405004.htm
    [46]
    Madden R A, Julian P R.Detection of a 40—50 day oscillation in the zonal wind in the tropical Pacific.J A S, 1971, 28: 702-708. doi:  10.1175/1520-0469%281971%29028<0702%3ADOADOI>2.0.CO%3B2
    [47]
    Madden R A, Julian P R.Description of global-scale circulation cells in the tropics with a 40—50 day period.J A S, 1972, 29: 1109-1123. http://adsabs.harvard.edu/abs/1972JAtS...29.1109M
    [48]
    陈隆勋, 谢安, Murakami Takio.OLR资料所揭示的El Nino和30—60天振荡之间关系∥国家气象局气象科学研究院.气象科学技术集刊 (11).北京:气象出版社, 1987:26-35.
    [49]
    Chen Longxun, Shao Yongning.Variation of 30—60 day oscillation in atmosphere before and during 1982 El Nino.Acta Meteorologica Sinica, 1991, (4):397-410.
    [50]
    Zhu Congwen, Nakazawa T, Li Jianping.Modulation of twin tropical cyclogenesis by the MJO westerly wind burst during the onset period of 1997/98 ENSO.Adv AtmosSci, 2003, 20(6): 882-898. doi:  10.1007/BF02915512
    [51]
    Murakami T, Nakazawa T, He Jinhai.On the 40—50 day oscillation during the 1979 Northern Hemisphere summer Part Ⅰ: phase propagation.J Meteor Soc Japan, 1984, 62:440-468. https://www.jstage.jst.go.jp/article/jmsj1965/62/3/62_3_440/_article
    [52]
    Chen Longxun, Zhu Congwen, Wang Wen, et al.Analysis of the characteristics of 30—60 day low frequency oscillation over Asia during 1998 SCSMEX.Adv Atmos Sci, 2001, 18:623-638. doi:  10.1007/s00376-001-0050-0
    [53]
    陈丽臻, 张先恭, 陈隆勋.长江流域两个典型旱涝年大气30—60天低频波差异的初步分析.应用气象学报, 1994, 5 (4):483-488. http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFQ&dbname=CJFD9495&filename=YYQX404.012&v=MjE0ODNhZHJlNEdzL01ybzBxRjU0T2ZnZzV6aEFVNGpoNE9YNlRySDAzZWJPVFJibWRidWRzRkNIaFVBPT1QRFQ=
    [54]
    Zhu C W, Nakazawa T, Li J P, et al. The 30—60 day intraseasonal oscillation over the western North Pacific Ocean and its impacts on summer flooding in China during 1998. Geophys Res Lett, 30(18), 1952, doi:  10.1029/2003GL017817, 2003.
    [55]
    祝从文, Nakazawa T, 李建平.低频振荡对印度-西太平洋地区热带低压/气旋生成的影响.气象学报, 2004, 62(1): 42-50. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200401004.htm
    [56]
    宋玉宽, 陈隆勋.夏季低频振荡的数值模拟∥何金海, 丁一汇, 陈隆勋.亚洲季风研究的新进展.北京:气象出版社, 1996:200-210.
    [57]
    朱福康.南亚高压的研究及其在天气预报中的应用∥国家气象局气象科学研究院.气象科学技术集刊 (6).北京:气象出版社, 1983:1-8.
    [58]
    陈隆勋, 李维亮.亚洲季风区各月的大气热源结构∥《会议文集》编辑组.全国热带夏季风学术会议文集.北京:云南人民出版社, 1982:246-258.
    [59]
    李维亮, 陈隆勋.亚洲上空夏季平均环流的结构及其大气热源分析.气象学报, 1983, 41(1):43-55. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB198301005.htm
    [60]
    Chen Longxun, Li Weiliang, He Jiahua. On the Atmospheric Heat Source over Asia and Its Relation to the Formation of the Summer Circulation∥Proceedings of the First Sino-American Workshop on Mountain Meteorology. Boston: American Meteorological society, 1983: 265-290.
    [61]
    Zhao Ping, Chen Longxun.The climate characteristics of surface turbulent exchange coefficient and surface heat source over the Qinghai-Tibetan Plateau. Acta Meteorologica Sinica, 2000, 14 (1):13-29.
    [62]
    Zhao Ping, Chen Longxun.The calculation of solar albedo and radiation balance and the analysis of their climate characteristics over the Qinghai-Tibetan Plateau.Adv Atmos Sci, 2000, 17 (1):140-156. doi:  10.1007/s00376-000-0050-5
    [63]
    Zhao Ping, Chen Longxun.Role of atmospheric heat source/sink over the Qinghai-Xizang Plateau in quasi-4 year oscillation of atmosphere-land-ocean interaction. Chinese Science Bulletin, 2001, 46(3) :241-245. doi:  10.1007/BF03187178
    [64]
    赵平, 陈隆勋.青藏高原大气热量源汇在海-地-气相互作用准4年振荡中的作用.科学通报, 2000, 45(15): 1666-1671. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200015017.htm
    [65]
    Zhao Ping, Chen Longxun.Interannal variability of atmospheric heat source/sink over the Qinghai-Xizang (Tibetan) Plateau and its relation to circulation.Adv Atmos Sci, 2001, 18(1):106-112. doi:  10.1007/s00376-001-0007-3
    [66]
    Zhao Ping, Chen Longxun.Climatic features of atmospheric heat source/sink over the Qinghai-Xizang Plateau in 35 years and its relation to rainfall in China.Science in China (Series D), 2001, 44 (Supp) :858-864. http://earth.scichina.com:8080/sciDe/CN/abstract/abstract306457.shtml
    [67]
    Chen Longxun, Li Wei, Zhao Ping.Impact of winter thermal condition of the Tibetan Plateau on the zonal wind anomaly over equatorial Pacific.Science in China (Series D), 2001, 44 (Supp): 400-409. http://earth.scichina.com:8080/sciDe/CN/abstract/abstract306484.shtml
    [68]
    Li Wei, Chen Longxun.Characteristics of seasonal variation of rainfall over the Tibetan Plateau during summer 1998 and its impact on East Asian weather.Acta Meteorological Sinica, 2001, 15(3):293-309. http://www.cqvip.com/QK/88418X/200103/1001466116.html
    [69]
    Li Wei, Chen Longxun.Characteristics of the Seasonal Variation of Rainy Season over the Tibetan Plateau in 1998 with Its Impact on East Asian Weather∥The Second Plateau Experiment of Atmospheric Sciences (TIPEX-GAME/Tibet).Beijing: China Meteorological Press, 2002:187-190.
    [70]
    Chen Longxun, Li Wei.Characteristics of the Seasonal variation of the Atmospheric Heat Sources and the Moisture Sinks over the Tibetan Plateau and its impact in 1998∥The Second Plateau Experiment of Atmospheric Sciences (TIPEX-GAME/Tibet), Beijing: China Meteorological Press, 2002: 183-186.
    [71]
    Chen L X, Schmidt F, Li W.Characteristics of the atmospheric heat sources and moisture sinks over the Qinghai-Tibetan Plateau during the second TIPEX of summer 1998 and its impact on sur-rounding monsoon.Meteorology and Atmospheric Physics, 2003, 83(1-2): 1-18. doi:  10.1007/s00703-002-0546-x
    [72]
    陶诗言, 朱福康.夏季亚洲南部100 hPa流型的变化及其与太平洋副热带高压进退的关系.气象学报, 1964, 34(4): 385-395. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB196404000.htm
    [73]
    朱福康, 陆龙骅, 陈咸吉, 等.南亚高压.北京:科学出版社, 1981:1-94.
    [74]
    陆龙骅, 陈咸吉, 朱福康, 等.南亚高压与我国夏季降水的天气学相关分析∥国家气象局气象科学研究院.气象科学技术集刊 (6).北京:气象出版社, 1983: 18-25.
    [75]
    朱文妹, 楼光平, 赵卫, 等.南亚高压季节性位移及其对我国东部地区雨带的影响∥国家气象局气象科学研究院.气象科学技术集刊 (10).北京:气象出版社, 1987: 131-137.
    [76]
    郑庆林, 燕启民, 宋青丽.初夏过渡季节南亚高压北跳加强中期天气过程的数值研究∥国家气象局气象科学研究院.气象科学技术集刊 (10).北京:气象出版社, 1987: 1-221.
    [77]
    Chen Longxun, Chen Duo, Shen Rugui.The interannual oscillation of rainfall over China and its relation to the interannual oscillation of the air-sea system.Acta Meteorologica Sinica, 1990, 4 (5):598-612. http://www.cqvip.com/QK/88418X/199005/4001664309.html
    [78]
    Chen Longxun, Yang Jinhua, Wang Gao.Evolutional features of interannual low-frequency oscillations and their ralation to the occurrence of El Nino.Acta Meteorologica Sinica, 1989, 3 (3):352-365. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXW198903007.htm
    [79]
    Chen Longxun, Dong Min, Shao Yongning.The characteristics of interannual variations on the East Asian Monsoon.J Meteor Soc Japan (special issue), 1992: 397-421. http://cat.inist.fr/?aModele=afficheN&cpsidt=5475185
    [80]
    Dong Min, Chen Longxun.Interannual Variation of the East Asian Monsoon∥Studies of Asian Monsoon in Japan and China.Japan:Meteorological Research Institute, 1992:268-285.
    [81]
    Xie An, Chen Longxun, Murakami T.Annual and interannual variations of large-scale circulation over the tropics as revealed from OLR data.Acta Oceanologica Sinica, 1988, 7(2): 195-202. http://mall.cnki.net/magazine/article/SEAE198802003.htm
    [82]
    Yang Jinhua, Chen Longxun, Wang Gao.The propagating features of the interannual low-frequency oscillation.Adv Atmos Sci, 1988, 5(4):405-420. doi:  10.1007/BF02656787
    [83]
    Zhu Yanfeng, Chen Longxun.Study on the quasi-four year oscillation of air-sea interaction.Acta Meteorologica Sinica, 2000, 14(3):293-306. http://www.cqvip.com/QK/88418X/200003/4000725300.html
    [84]
    陈隆勋, 赵平, 祝从文, 等.海陆气相互作用的准四年振荡机制.气象科学, 2000, 20(3):240-249. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKX200003002.htm
    [85]
    朱艳峰, 陈隆勋, 宇如聪.中国气候异常变化与ENSO准四年循环的联系分析.热带气象学报, 2003, 19(4): 345-356. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200304001.htm
    [86]
    Zhu Yanfeng, Chen Longxun.Relationship between the Asian/Austrilian monsoon and ENSO on a quasi-four year Scale.Adv Atmos Sci, 2002, 19(4):727-740. doi:  10.1007/s00376-002-0012-1
    [87]
    Zhu Congwen, Chen Longxun, Yamazaki N.The interdecadal variation characteristics of artic sea ice cover-ENSO-East Asian monsoon and their relationship at quasi-four years time Scale.Adv Atmos Sci, 1999, 16(4): 641-652. doi:  10.1007/s00376-999-0038-8
    [88]
    Wu Bingyi, Zhang R, D'Arrigo R.Distinct modes of the East Asian Winter Monsoon.Mon Wea Rev, 2006, 134:2165-2179. doi:  10.1175/MWR3150.1
    [89]
    Wu Bingyi, Wang Jia.Possible impacts of winter Arctic Oscillation on Siberian High, the East Asian winter monsoon and seaice.Adv Atmos Sci, 2002, 19(2):297-320. doi:  10.1007/s00376-002-0024-x
    [90]
    Wu Bingyi, Wang Jia.Winter Arctic Oscillation, Siberian High and East Asian winter monsoon.Geophys Res Lett, 29(19), 1897, doi:  10.1029/2002GL015373, 2002.
    [91]
    Wu B, Huang R H.Relationship between sea level pressure of the tropical western Pacific and subsequent Asian Summer Monsoon.Adv Atmos Sci, 2003, 20(4): 496-510. doi:  10.1007/BF02915494
    [92]
    Wu B, Huang R H, Gao D Y.Numerical simulations on influences of variation of sea ice thickness and extents on atmospheric circulation.Acta Meteorologica Sinica, 2002, 16(2):150-164.
    [93]
    柏晶瑜, 徐祥德, 苗秋菊.北极海冰"强信号"影响域.气象学报, 2000, 58(4):486-491. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200004011.htm
    [94]
    陈隆勋, 王予辉, 缪群.南极冰雪覆盖变异对南、北半球大气环流影响的数值试验∥地磁大气空间研究及应用———庆贺朱岗昆教授八十寿辰.北京:地震出版社, 1996:322-332.
    [95]
    Chen Longxun, Miao Qun.The numerical experiments for climate variability of monsoon under the united effects of Antarctic ice cover and SST.Acta Meteorologica Sinica, 1996, 10(3): 387-397.
    [96]
    Miao Qun, Chen Longxun.Numerical experiments for the impact of Antarctic ice cover and sea surface temperature on climate variability.Acta Meteorologica Sinica, 1997, 11(1):23-34. http://www.cqvip.com/QK/88418X/199701/1004725639.html
    [97]
    王亚非, 高桥清利.长江中下游降水以及东亚夏季风环流的年代际变化.热带气象学报, 2005, 21(4):351-358. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200504001.htm
    [98]
    陶诗言, 朱文妹, 赵卫.论梅雨的年际变异.大气科学, 1988, 12(特刊):13-21.
    [99]
    朱文妹, 赵卫, 陶诗言.1987和1980年夏季江淮流域典型旱涝异常年份东亚季风环流的特征∥国家气象局气象科学研究院.气象科学技术集刊 (11).北京:气象出版社, 1987: 36-44.
    [100]
    张家诚.关于中国季风性质的几个问题.气象学报, 1959, 30(4): 350-361. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB195904005.htm
    [101]
    张家诚.经向海陆分布对大气环流的热力作用.气象学报, 1980, 38(3):219-226. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB198003002.htm
    [102]
    张家诚.极冰的冷源作用和季风.气象, 1981, (7) :6-8. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX198107001.htm
    [103]
    张家诚.季风环流系统及其相互关系的探讨∥国家气象局气象科学研究院.气象科学技术集刊 (11).北京:气象出版社, 1987:1-8.
    [104]
    张家诚.中国及邻近地区冬到夏的季节变化.气象, 1995, 21(7): 3-8. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX507.000.htm
    [105]
    赵汉光, 张家诚.东亚季风和我国夏季雨带的关系.气象, 1996, 22(4):8-12. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX604.001.htm
    [106]
    赵溱, 张家诚.高纬度冰雪覆盖对行星季风影响的数值试验∥国家气象局气象科学研究院.气象科学技术集刊 (10).北京:气象出版社, 1987: 8-16.
    [107]
    朱福康, 陆龙骅.南半球对北半球初夏季节转换的一种可能机理.气象学报, 1984, 42(4): 448-457. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB198404008.htm
    [108]
    章基嘉, 朱福康, 彭永清, 等.1979年初夏大气环流季节转化的若干事实.气象, 1984, (6): 2-4. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX198406000.htm
    [109]
    章基嘉, 朱福康.夏季东亚大气环流的研究.气象科学研究院院刊, 1986, 1(1):83-93. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX198601010.htm
    [110]
    陈晶华, 陈隆勋.亚洲南部的海陆分布对亚洲夏季风形成的作用.应用气象学报, 1991, 2(4) :355-361. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19910449&flag=1
    [111]
    金华, 何金海, 陈隆勋, 等.亚洲南部地区海陆分布和南半球陆地对亚洲夏季风影响的数值试验.大气科学, 2006, 30(5):1043-1053. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200605029.htm
    [112]
    Jin Qihua, He Jinhai, Chen Longxun, et al.Impact of oceancontinent distribution over Southern Asia on the formation of summer mosoon.Acta Meteorologica Sinica, 2006, 20(1): 95-108. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_qxxb-e200601009
    [113]
    李维亮, 钟名森.1979年夏季南海北部地区大气加热和各分量的中期振荡特征∥国家气象局气象科学研究院.气象科学技术集刊 (10).北京:气象出版社, 1987:137-149.
    [114]
    陈明萱, 李维亮.非绝热加热对赤道地区平均纬向环流的作用———线性响应∥国家气象局气象科学研究院.气象科学技术集刊 (11).北京:气象出版社, 1987:100-108.
    [115]
    徐祥德.热带大气周期性振荡相图结构与南北半球中纬度热力强迫效应的相关关系.大气科学, 1992, 16(2):147-157. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199202002.htm
    [116]
    徐祥德, 赵天良, 何金海, 等.澳洲大陆热力强迫对南北半球流型域的影响效应.大气科学, 1993, 17(6):641-650. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199306000.htm
    [117]
    徐祥德, 苗峻峰.江淮流域旱涝与大气遥相关经向波列路径特征的相关关系.气象科学, 1993, 13(1): 9-16. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKX199301001.htm
    [118]
    徐祥德, 赵天良.偶极子型系统及其阻塞结构成因的数值试验.气象学报, 1994, 52(1):107-110. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB401.012.htm
    [119]
    徐祥德, 苗秋菊, 彭世球, 等.长江中下游洪涝与强信号源大圆路径波列的特征∥中国科学院大气物理研究所.东亚季风和中国暴雨———庆贺陶诗言院士八十华诞文集.北京:气象出版社, 1998: 220-229.
    [120]
    徐祥德, 张雪金, 姚文清, 等.1998年梅雨期区域边界"水汽流"特征及其对长江流域持续特大暴雨影响∥赵柏林,丁一汇.淮河流域能量与水分循环研究.北京:气象出版社, 1999: 12-19.
    [121]
    徐祥德, 陶诗言, 王继志, 等.青藏高原—季风水汽输送"大三角形"影响域特征与中国区域旱涝异常的关系.气象学报, 2002, 60(3): 257-266. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200203000.htm
    [122]
    徐祥德.关于大气环流型季节特征形成的物理因子的数值试验.气象科学, 1990, 10(3):226-236. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKX199003002.htm
    [123]
    徐祥德.波射线变形及其影响因子的探讨.气象学报, 1991, 49(3):288-299. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB199103003.htm
    [124]
    苗秋菊, 徐祥德.区域性旱涝与海温特征分布的相关链模型.应用气象学报, 1998, 9(增刊):47-55. http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFQ&dbname=CJFD9899&filename=YYQX8S1.006&v=MTc2NzgwM2ViT1RSYm1kYnVkc0ZTN21VQT09UERUYWRydmJIOC9NcjRrcUY1NE9mZ2c1emhBVTRqaDRPWDZUckg=
    [125]
    苗秋菊, 徐祥德, 张雪金.长江中下游旱涝的环流型与赤道东太平洋海温遥相关波列特征.气象学报, 2002, 60(6): 688-697. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200206005.htm
    [126]
    章基嘉, 徐祥德, 苗峻峰.青藏高原地面热力异常对夏季江淮流域持续暴雨形成作用的数值试验.大气科学, 1995, 19 (3): 270-276. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK503.001.htm
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中
  • -->

Catalog

    Get Citation
    PDF
    XML
    Article views (9216) PDF downloads(2269) Cited by()
    • Received : 2006-11-13
    • Accepted : 2006-11-27
    • Published : 2006-12-31
    Journal Online
    Contact

    © 2020 Journal of Applied Meteorological Science   京ICP备15006967号-1

    Supported by Beijing Renhe Information Technology Co. Ltd

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return