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Volume 1 Issue 1

Jan.  1984

Article Contents

NUMERICAL EXPERIMENT ON THE SEASONAL TRANSITION OF GENERAL CIRCULATION OVER ASIA - PART Ⅰ


doi: 10.1007/BF03187624

  • The onset of the 1979 summer monsoon is investigated using the ECMWF grid-point model. The role of the Tibetan Plateau in this process is investigated by means of parallel model integrations with different orographies. Similarly, the relative roles of land-sea thermal contrast, latent heat release and Southern Hemisphere influence are studied. The influence of the African Highland on the onset of the Somali jet is also explored. A generally satisfactory performance of the model in representing the onset of the monsoon is documented and various contributions to this from different model components are discussed. In Pan I of this paper the impact from the Southern Hemisphere is presented.
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    [2] Zhao Shengju, 1986: RELATION BETWEEN LONG-DISTANCE MIGRATION OF ORIENTAL ARMYWORMS AND SEASONAL VARIATION OF GENERAL CIRCULATION OVER EAST ASIA, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 215-226.  doi: 10.1007/BF02682555
    [3] Ni Yunqi, Bette L. Otto-Bliesner, David D. Houghton, 1987: THE SENSITIVITY OF NUMERICAL SIMULATION TO OROGRAPHY SPECIFICATION IN THE LOW RESOLUTION SPECTRAL MODEL-PART I: THE EFFECTS OF OROGRAPHY ON THE ATMOSPHERIC GENERAL CIRCULATION, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 1-12.  doi: 10.1007/BF02663607
    [4] Jianhua LU, Tapio SCHNEIDER, 2017: Evolving Perspectives on Abrupt Seasonal Changes of the General Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1185-1194.  doi: 10.1007/s00376-017-7068-4
    [5] Zhang Xuehong, Liang Xinzhong, 1989: A Numerical World Ocean General Circulation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 44-61.  doi: 10.1007/BF02656917
    [6] Jun Matsumoto, 1997: Seasonal Transition of Summer Rainy Season over Indochina and Adjacent Monsoon Region, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 231-245.  doi: 10.1007/s00376-997-0022-0
    [7] Chen Yuejuan, Zhang Hong, Bi Xunqiang, 1998: Numerical Experiment for the Impact of the Ozone Hole over Antarctica on the Global Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 300-311.  doi: 10.1007/s00376-998-0002-z
    [8] Wang Huijun, 1992: The Seasonal Climatic Simulation of 9000 Years before Present by Using the IAP Atmospheric General Circulation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 451-457.  doi: 10.1007/BF02677077
    [9] Lin Chunyu, 1985: STABILIZATION OF SUMMER MONSOON IN MIDDLE AND LOWER REACHES OF THE CHANGJIANG RIVER AND SEASONAL TRANSITION OF EAST-ASIAN CIRCULATION PATTERN IN EARLY SUMMER, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 376-384.  doi: 10.1007/BF02677254
    [10] Gong-Wang Si, Kuranoshin Kato, Takao Takeda, 1995: The Early Summer Seasonal Change of Large-scale Circulation over East Asia and Its Relation to Change of The Frontal Features and Frontal Rainfall Environment During 1991 Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 151-176.  doi: 10.1007/BF02656829
    [11] LI Jiawei, HAN Zhiwei, 2012: A Modeling Study of Seasonal Variation of Atmospheric Aerosols over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 101-117.  doi: 10.1007/s00376-011-0234-1
    [12] Liu Ruizhi, 1986: A NUMERICAL EXPERIMENT OF CYCLOGENESIS AND THE DEVELOPMENT OF DISTURBANCES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 499-504.  doi: 10.1007/BF02657939
    [13] 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
    [14] 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
    [15] WANG Chenghai, YU Lian, HUANG Bo, 2012: The Impact of Warm Pool SST and General Circulation on Increased Temperature over the Tibetan Plateau, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 274-284.  doi: 10.1007/s00376-011-1034-3
    [16] Hu Zengzhen, Tsuyoshi Nitta, 1997: Seasonality of the Interaction between Convection over the Western Pacific and General Circulation in the Northern Hemisphere, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 541-553.  doi: 10.1007/s00376-997-0072-3
    [17] Liu Huizhi, Sang Jianguo, Zhang Boyin, Johnny C.L. Chan, Andrew Y.S.Cheng, Liu Heping, 2002: Influences of Structures on Urban Ventilation:A Numerical Experiment, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 1045-1054.  doi: 10.1007/s00376-002-0063-3
    [18] Xu Yuantai, Li Hongzhou, 1989: A Numerical Experiment of Mesolow on the Eastern Side of the Taihang Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 133-136.  doi: 10.1007/BF02656924
    [19] FU Yunfei, LIN Yihua, Guosheng LIU, WANG Qiang, 2003: Seasonal Characteristics of Precipitation in 1998 over East Asia as Derived from TRMM PR, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 511-529.  doi: 10.1007/BF02915495
    [20] KUANG Xueyuan, ZHANG Yaocun, 2005: Seasonal Variation of the East Asian Subtropical Westerly Jet and Its Association with the Heating Field over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 831-840.  doi: 10.1007/BF02918683

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Manuscript History

Manuscript received: 10 January 1984
Manuscript revised: 10 January 1984
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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NUMERICAL EXPERIMENT ON THE SEASONAL TRANSITION OF GENERAL CIRCULATION OVER ASIA - PART Ⅰ

  • 1. InstituteofAtmosphericPhysics,AcademiaSinica.Beijing,EuropeanCentreforMediumRandgeWeatherForecasts,Reading,England

Abstract: The onset of the 1979 summer monsoon is investigated using the ECMWF grid-point model. The role of the Tibetan Plateau in this process is investigated by means of parallel model integrations with different orographies. Similarly, the relative roles of land-sea thermal contrast, latent heat release and Southern Hemisphere influence are studied. The influence of the African Highland on the onset of the Somali jet is also explored. A generally satisfactory performance of the model in representing the onset of the monsoon is documented and various contributions to this from different model components are discussed. In Pan I of this paper the impact from the Southern Hemisphere is presented.

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