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Volume 11 Issue 1

Jan.  1994

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1994 >  11(1): 51-56

A GCM Study on the Mechanism of Seasonal Abrupt Changes

  • 1.

    LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080


doi: 10.1007/BF02656993

  • In this paper the observational studies and some related dynamical and numerical researches on seasonal abrupt changes were reviewed first. Then a speculation that the seasonal variation of insolation and the nonlinear dynamic interaction account for the abrupt changes was put forward and was asserted by a set of GCM sensitivity experiments. The results show that the abrupt changes would exist in case that all the earth surface was grass land and there was no topography. However, many factors may have influences on the abrupt changes. Hence this phenome-non is quite complicated and needs further investigations.
  • [1] 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
    [2] LI Chongyin, HE Jinhai, ZHU Jinhong, 2004: A Review of Decadal/Interdecadal Climate Variation Studies in China, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 425-436.  doi: 10.1007/BF02915569
    [3] WAN Rijin, ZHAO Bingke, WU Guoxiong, 2009: New Evidences on the Climatic Causes of the Formation of the Spring Persistent Rains over Southeastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1081-1087.  doi: 10.1007/s00376-009-7202-z
    [4] GAO Shanhong, LIN Hang, SHEN Biao, FU Gang, 2007: A Heavy Sea Fog Event over the Yellow Sea in March 2005: Analysis and Numerical Modeling, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 65-81.  doi: 10.1007/s00376-007-0065-2
    [5] GAO Shouting, Xiaofan LI, 2008: Impacts of Initial Conditions on Cloud-Resolving Model Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 737-747.  doi: 10.1007/s00376-008-0737-6
    [6] WU Tongwen, WU Guoxiong, 2004: An Empirical Formula to Compute Snow Cover Fraction in GCMs, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 529-535.  doi: 10.1007/BF02915720
    [7] Zeng Qingcun, Yuan Chongguang, Li Xu, Zhang Ronghua, Yang Fanglin, Zhang Banglin, Lu Peisheng, Bi Xunqiang, Wang Huijun, 1997: Seasonal and Extraseasonal Predictions of Summer Monsoon Precipitation by Gcms, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 163-176.  doi: 10.1007/s00376-997-0017-x
    [8] BAI Jie, GE Quansheng, DAI Junhu, 2011: The Response of First Flowering Dates to Abrupt Climate Change in Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 564-572.  doi: 10.1007/s00376-010-9219-8
    [9] WANG Zhi, GAO Kun, 2003: Sensitivity Experiments of an Eastward-Moving Southwest Vortex to Initial Perturbations, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 638-649.  doi: 10.1007/BF02915507
    [10] He Jinhai, Li Jun, Zhu Qiangen, 1989: Sensitivity Experiments on Summer Monsoon Circulation Cell in East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 120-132.  doi: 10.1007/BF02656923
    [11] WANG Shaowu, ZHOU Tianjun, CAI Jingning, ZHU Jinhong, XIE Zhihui, GONG Daoyi, 2004: Abrupt Climate Change around 4 ka BP: Role of the Thermohaline Circulation as Indicated by a GCM Experiment, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 291-295.  doi: 10.1007/BF02915716
    [12] Luo Zhexian, 1987: ABRUPT CHANGE OF FLOW PATTERN IN BAROCLINIC ATMOSPHERE FORCED BY JOINT EFFECTS OF DIABATIC HEATING AND OROGRAPHY, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 137-144.  doi: 10.1007/BF02677060
    [13] Qian Yongfu, 1991: Numerical Experiments of the Effects of Initial Desert Moisture on the Climate Change, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 459-470.  doi: 10.1007/BF02919268
    [14] CHEN Hua, GUO Jing, XIONG Wei, GUO Shenglian, Chong-Yu XU, 2010: Downscaling GCMs Using the Smooth Support Vector Machine Method to Predict Daily Precipitation in the Hanjiang Basin, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 274-284.  doi: 10.1007/s00376-009-8071-1
    [15] 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
    [16] ZHOU Qian, DUAN Wansuo, MU Mu, FENG Rong, 2015: Influence of Positive and Negative Indian Ocean Dipoles on ENSO via the Indonesian Throughflow: Results from Sensitivity Experiments, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 783-793.  doi: 10.1007/s00376-014-4141-0
    [17] WANG Zhi, GAO Kun, 2006: Adjoint Sensitivity Experiments of a Meso- -scale Vortex in the Middle Reaches of the Yangtze River, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 267-281.  doi: 10.1007/s00376-006-0267-z
    [18] Kai Chi WONG, Senfeng LIU, Andrew G. TURNER, Reinhard K. SCHIEMANN, 2018: Different Asian Monsoon Rainfall Responses to Idealized Orography Sensitivity Experiments in the HadGEM3-GA6 and FGOALS-FAMIL Global Climate Models, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1049-1062.  doi: 10.1007/s00376-018-7269-5
    [19] SUN Guodong, MU Mu, 2009: Nonlinear Feature of the Abrupt Transitions between Multiple Equilibria States of an Ecosystem Model, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 293-304.  doi: 10.1007/s00376-009-0293-8
    [20] Fu Congbin, 1993: An Aridity Trend in China and Its Abrupt Feature in Association with the Global Warming, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 11-20.  doi: 10.1007/BF02656950
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    • Manuscript History

    Manuscript received: 10 January 1994
    Manuscript revised: 10 January 1994
    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

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    A GCM Study on the Mechanism of Seasonal Abrupt Changes

    • 1. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080
    • Manuscript received: 1994-01-10
    • Manuscript revised: 1994-01-10

    Abstract: In this paper the observational studies and some related dynamical and numerical researches on seasonal abrupt changes were reviewed first. Then a speculation that the seasonal variation of insolation and the nonlinear dynamic interaction account for the abrupt changes was put forward and was asserted by a set of GCM sensitivity experiments. The results show that the abrupt changes would exist in case that all the earth surface was grass land and there was no topography. However, many factors may have influences on the abrupt changes. Hence this phenome-non is quite complicated and needs further investigations.

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