Advanced Search

Volume 8 Issue 1

Jan.  1991

Article Contents

Some Analyses and Numerical Simulations of Meiyu in East Asia in 1983


doi: 10.1007/BF02657365

  • In this paper the differences between Meiyu and Baiu front in 1983 have firstly been analysed, the trajectories of air on and to the north side of Meiyu and Baiu fronts during the Meiyu period have then been traced, and the fore-casting and simulating of 4 sets of Meiyu onset of the year have finally been run utilizing the global model at UK Me-teorological Office. The results show: 1) Meiyu fronts are different from Baiu ones in temperature, humidity and stratification fields in lower atmosphere; and the possibly reasons for it are explained. 2) The Bay of Bengal is the main moisture source for Meiyu front, the South China Sea and the Pacific, for Baiu ones; and some existed argu-ments on it are also discussed. 3) The onset of Meiyu and its rainfall and rain belts are sensitive to the Tibetan Plateau, and the water vapour conditions over the Bay of Bengal and the South China Sea, but not sensitive to the SST over the equatorial area or to the East of Japan.
  • [1] ZHANG Meigen, XU Yongfu, Itsushi UNO, Hajime AKIMOTO, 2004: A Numerical Study of Tropospheric Ozone in the Springtime in East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 163-170.  doi: 10.1007/BF02915702
    [2] Liu Huaqiang, Qian Yongfu, 1999: Numerical Simulations of Intense Meiyu Rainfall in 1991 over the Changjiang and Huaihe River Valleys by a Regional Climate Model with p-б Incorporated Coordinate System, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 395-404.  doi: 10.1007/s00376-999-0018-z
    [3] Gao Xuejie, Zhao Zongci, Filippo Giorgi, 2002: Changes of Extreme Events in Regional Climate Simulations over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 927-942.  doi: 10.1007/s00376-002-0056-2
    [4] LI Qiaoping, DING Yihui, DONG Wenjie, YAN Guanhua, 2007: A Numerical Study on the Winter Monsoon and Cold Surge over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 664-678.  doi: 10.1007/s00376-007-0664-y
    [5] ZHANG Jie, Laurent LI, ZHOU Tianjun, XIN Xiaoge, 2013: Evaluation of Spring Persistent Rainfall over East Asia in CMIP3/CMIP5 AGCM Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1587-1600.  doi: 10.1007/s00376-013-2139-7
    [6] Xiaohan LI, Yi ZHANG, Yanluan LIN, Xindong PENG, Baiquan ZHOU, Panmao ZHAI, Jian LI, 2023: Impact of Revised Trigger and Closure of the Double-Plume Convective Parameterization on Precipitation Simulations over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1225-1243.  doi: 10.1007/s00376-022-2225-9
    [7] ZHOU Ningfang, YU Yongqiang, QIAN Yongfu, 2006: Simulations of the 100-hPa South Asian High and Precipitation over East Asia with IPCC Coupled GCMs, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 375-390.  doi: 10.1007/s00376-006-0375-9
    [8] Huang Ronghui, Wu Bingyi, Sung-Gil Hong, Jai-Ho Oh, 2001: Sensitivity of Numerical Simulations of the East Asian Summer Monsoon Rainfall and Circulation to Different Cumulus Parameterization Schemes, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 23-41.  doi: 10.1007/s00376-001-0002-8
    [9] Yuan Zhuojian, Wang Tongmei, He Haiyan, Luo Huibang, Guo Yufu, 2000: A Comparison between Numerical Simulations of Forced Local Hadley (Anti-Hadley) Circulation in East Asian and Indian Monsoon Regions, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 538-554.  doi: 10.1007/s00376-000-0017-6
    [10] Huang Ronghui, Lu Li, 1989: Numerical Simulation of the Relationship between the Anomaly of Subtropical High over East Asia and the Convective Activities in the Western Tropical Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 202-214.  doi: 10.1007/BF02658016
    [11] Huang Ronghui, Li Xu, Yuan Chongguang, Lu Riyu, Moon Sung-Euii, Kim Ung-Jun, 1998: Seasonal Prediction Experiments of the Summer Droughts and Floods during the Early 1990’s in East Asia with Numerical Models, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 433-446.  doi: 10.1007/s00376-998-0025-5
    [12] Jie WU, Xuejie GAO, Yingmo ZHU, Ying SHI, Filippo GIORGI, 2022: Projection of the Future Changes in Tropical Cyclone Activity Affecting East Asia over the Western North Pacific Based on Multi-RegCM4 Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 284-303.  doi: 10.1007/s00376-021-0286-9
    [13] Zhang Ren, Yu Zhihao, 2000: Numerical and Dynamical Analyses of Heat Source Forcing and Restricting Subtropical High Activity, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 61-71.  doi: 10.1007/s00376-000-0043-4
    [14] Si Gongwang, Donald R. Johnson, 1985: A NUMERICAL EXPERIMENTAL STUDY OF SOME DYNAMICAL EFFECTS ON SOUTHERN ASIATIC HIGH, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 133-146.  doi: 10.1007/BF03179746
    [15] Yang Yan, Li Zhijin, Ji Liren, 1997: Adjoint Sensitivity Analyses on the Anomalous Circulation Features in East Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 111-123.  doi: 10.1007/s00376-997-0050-9
    [16] YANG Shili, FENG Jinming, DONG Wenjie, CHOU Jieming, 2014: Analyses of Extreme Climate Events over China Based on CMIP5 Historical and Future Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1209-1220.  doi: 10.1007/s00376-014-3119-2
    [17] WANG Pengyun, YANG Jing, 2003: Observation and Numerical Simulation of Cloud Physical Processes Associated with Torrential Rain of the Meiyu Front, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 77-96.  doi: 10.1007/BF03342052
    [18] Zhao Li, Zhao Sixiong, 1995: Numerical Experiments of Meiyu(Baiu) Rainfall by Quasi-Lagrangian Limited Area Model with Terrain, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 57-66.  doi: 10.1007/BF02661287
    [19] LOU Xiaofeng, HU Zhijin, SHI Yueqin, WANG Pengyun, ZHOU Xiuji, 2003: Numerical Simulations of a Heavy Rainfall Case in South China, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 128-138.  doi: 10.1007/BF03342057
    [20] Xu Yinlong, Zhou Mingyu, 1999: Numerical Simulations on the Explosive Cyclogenesis over the Kuroshio Current, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 64-76.  doi: 10.1007/s00376-999-0004-5

Get Citation+

Export:  

Share Article

Manuscript History

Manuscript received: 10 January 1991
Manuscript revised: 10 January 1991
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Some Analyses and Numerical Simulations of Meiyu in East Asia in 1983

  • 1. Lanzhou Institute of Plateau Atmospheric Physics,Meteorological Office, Bracknell, Berkshire, UK,Meteorological Office, Bracknell, Berkshire, UK

Abstract: In this paper the differences between Meiyu and Baiu front in 1983 have firstly been analysed, the trajectories of air on and to the north side of Meiyu and Baiu fronts during the Meiyu period have then been traced, and the fore-casting and simulating of 4 sets of Meiyu onset of the year have finally been run utilizing the global model at UK Me-teorological Office. The results show: 1) Meiyu fronts are different from Baiu ones in temperature, humidity and stratification fields in lower atmosphere; and the possibly reasons for it are explained. 2) The Bay of Bengal is the main moisture source for Meiyu front, the South China Sea and the Pacific, for Baiu ones; and some existed argu-ments on it are also discussed. 3) The onset of Meiyu and its rainfall and rain belts are sensitive to the Tibetan Plateau, and the water vapour conditions over the Bay of Bengal and the South China Sea, but not sensitive to the SST over the equatorial area or to the East of Japan.

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return