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Volume 6 Issue 1

Jan.  1989

Article Contents

Sensitivity Experiments on Summer Monsoon Circulation Cell in East Asia


doi: 10.1007/BF02656923

  • The East-Asian summer monsoon meridional circulation (SMMC) cell is simulated together with two vigorous rainbands in terms of a primitive-equation model including in itself a variety of diabatic heating, frictional dissipation and moist processes under the condition of mountains available. Results are comparable to observations. Also, performed are experiments with the reduction of water content, and exclusion of the cumulus convective process and mountain effect. Contrast analyses indicate that the cell is strongly sensitive to the condition of the humidity field in the atmosphere, more intensely at 120o than at 100oE, and the presence (absence) of the cumulus convection has considerable effect on the intensification (weakening) of the cell, with the mountain ranges exhibiting more influence upon the cell at 100o than 120oE. This may suggest that a great difference lies in the cause of the cell for the two meridions.
  • [1] 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
    [2] 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
    [3] Chen Longxun, Jin Zuhui, 1984: THE MEDIUM-RANGE VARIATIONS OF THE SUMMER MONSOON CIRCULATION SYSTEM OVER EAST ASIA, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 224-245.  doi: 10.1007/BF02678135
    [4] 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
    [5] ZHU Jiang, LIN Caiyan, WANG Zifa, 2009: Dust Storm Ensemble Forecast Experiments in East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1053-1070.  doi: 10.1007/s00376-009-8218-0
    [6] Ding Yihui, Hu Jian, 1988: THE VARIATION OF THE HEAT SOURCES IN EAST CHINA IN THE EARLY SUMMER OF 1984 AND THEIR EFFECTS ON THE LARGE-SCALE CIRCULATION IN EAST ASIA, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 171-180.  doi: 10.1007/BF02656779
    [7] Wang Qianqian, Wang Anyu, Li Xuefeng, Li Shuren, 1986: THE EFFECTS OF THE QINGHAI-XIZANG PLATEAU ON THE MEAN SUMMER CIRCULATION OVER EAST ASIA, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 72-85.  doi: 10.1007/BF02680046
    [8] Ji Liren, S.Tibaldi, 1984: NUMERICAL EXPERIMENTS ON THE SEASONAL TRANSITION OF GENERAL CIRCULATION OVER ASIA--PART Ⅱ, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 188-205.  doi: 10.1007/BF02678131
    [9] XUE Feng, JIANG Dabang, LANG Xianmei, WANG Huijun, 2003: Influence of the Mascarene High and Australian High on the Summer Monsoon in East Asia: Ensemble Simulation, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 799-809.  doi: 10.1007/BF02915405
    [10] Zhang Renhe, 2001: Relations of Water Vapor Transport from Indian Monsoon with That over East Asia and the Summer Rainfall in China, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1005-1017.
    [11] JU Jianhua, Lü Junmei, CAO Jie, REN Juzhang, 2005: Possible Impacts of the Arctic Oscillation on the Interdecadal Variation of Summer Monsoon Rainfall in East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 39-48.  doi: 10.1007/BF02930868
    [12] Xue Feng, 2001: Interannual to Interdecadal Variation of East Asian Summer Monsoon and its Association with the Global Atmospheric Circulation and Sea Surface Temperature, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 567-575.  doi: 10.1007/s00376-001-0045-x
    [13] He Jinhai, Zhou Xueming, Ye Rongsheng, 1995: Numerical Study of Ural Blocking High’s Effect Upon Asian Summer Monsoon Circulation and East China Flood and Drought, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 361-370.  doi: 10.1007/BF02656985
    [14] Wu Renguang, Chen Lieting, 1998: Decadal Variation of Summer Rainfall in the Yangtze-Huaihe River Valley and Its Relationship to Atmospheric Circulation Anomalies over East Asia and Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 510-522.  doi: 10.1007/s00376-998-0028-2
    [15] 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
    [16] Wei Helin, Wang Wei-Chyung, 1998: A Regional Climate Model Simulation of Summer Monsoon over East Asia: A Case Study of 1991 Flood in Yangtze-Huai River Valley, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 489-509.  doi: 10.1007/s00376-998-0027-3
    [17] Cheng Anning, Chen Wen, Huang Ronghui, 1998: The Sensitivity of Numerical Simulation of the East Asian Monsoon to Different Cumulus Parameterization Schemes, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 204-220.  doi: 10.1007/s00376-998-0040-6
    [18] 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
    [19] SHANG Lin, LIU Yi, TIAN Wenshou, ZHANG Yuli, 2015: Effect of Methane Emission Increases in East Asia on Atmospheric Circulation and Ozone, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1617-1627.  doi: 10.1007/s00376-015-5028-4
    [20] ZHOU Botao, WANG Huijun, 2008: Interdecadal Change in the Connection Between Hadley Circulation and Winter Temperature in East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 24-30.  doi: 10.1007/s00376-008-0024-6

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Manuscript History

Manuscript received: 10 January 1989
Manuscript revised: 10 January 1989
通讯作者: 陈斌, bchen63@163.com
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Sensitivity Experiments on Summer Monsoon Circulation Cell in East Asia

  • 1. Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing

Abstract: The East-Asian summer monsoon meridional circulation (SMMC) cell is simulated together with two vigorous rainbands in terms of a primitive-equation model including in itself a variety of diabatic heating, frictional dissipation and moist processes under the condition of mountains available. Results are comparable to observations. Also, performed are experiments with the reduction of water content, and exclusion of the cumulus convective process and mountain effect. Contrast analyses indicate that the cell is strongly sensitive to the condition of the humidity field in the atmosphere, more intensely at 120o than at 100oE, and the presence (absence) of the cumulus convection has considerable effect on the intensification (weakening) of the cell, with the mountain ranges exhibiting more influence upon the cell at 100o than 120oE. This may suggest that a great difference lies in the cause of the cell for the two meridions.

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