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Volume 11 Issue 4

Oct.  1994

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1994 >  11(4): 459-462

The Fractal Dimension Distribution of the Short-Term Climate System in China and It’s Connection with the Monsoon Climate

  • 1.

    Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008


doi: 10.1007/BF02658166

  • By analyzing the Fractal Dimension (FD) distribution of the Short-range Climate system (SCS) in China, it is found that the FD varies in different region and this just agrees with the regionality of the monsoon climate in China. The FD of the SCS Lays between 2.0 and 5.0. In the vast eastern area of China, the FD almost grows gradually with the latitude. Line 4.0 is along the mountain chains from the Nanlin Mountain to the Wuyi Mountain. North of the line the FD varies only slightly and all are above 4.0. Only in coastal islands the FD is smaller than 3.0.
  • [1] Yang Fanglin, Yuan Chongguang, 1993: Numerical Simulation of Regional Short-Range Climate Anomalies, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 335-344.  doi: 10.1007/BF02658139
    [2] Liu Jianwen, Dong Peiming, 2001: Short-range Climate Prediction Experiment of the Southern Oscillation Index Based on the Singular Spectrum Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 873-881.
    [3] Ni Yunqi, Zhang Qin, Li Yuedong, 1991: A Numerical Study of the Mechanism for the Effect of Northern Winter Arctic Ice Cover on the Global Short-Range Climate Evolution, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 489-498.  doi: 10.1007/BF02919271
    [4] CAO Jian, Bin WANG, Baoqiang XIANG, Juan LI, WU Tianjie, Xiouhua FU, WU Liguang, MIN Jinzhong, 2015: Major Modes of Short-Term Climate Variability in the Newly Developed NUIST Earth System Model (NESM), ADVANCES IN ATMOSPHERIC SCIENCES, 32, 585-600.  doi: 10.1007/s00376-014-4200-6
    [5] HUANG Ping, WANG Pengfei, HU Kaiming, HUANG Gang, ZHANG Zhihua, LIU Yong, YAN Bangliang, 2014: An Introduction to the Integrated Climate Model of the Center for Monsoon System Research and Its Simulated Influence of El Nio on East Asian-Western North Pacific Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1136-1146.  doi: 10.1007/s00376-014-3233-1
    [6] Wen CHEN, Lin WANG, Juan FENG, Zhiping WEN, Tiaojiao MA, Xiuqun YANG, Chenghai WANG, 2019: Recent Progress in Studies of the Variabilities and Mechanisms of the East Asian Monsoon in a Changing Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 887-901.  doi: 10.1007/s00376-019-8230-y
    [7] Wei-Chyung WANG, Guoxing CHEN, Yangyang SONG, 2017: Modeling Aerosol Climate Effects over Monsoon Asia: A Collaborative Research Program, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1195-1203.  doi: 10.1007/s00376-017-6319-8
    [8] Wen CHEN, Renhe ZHANG, Renguang WU, Zhiping WEN, Liantong ZHOU, Lin WANG, Peng HU, Tianjiao MA, Jinling PIAO, Lei SONG, Zhibiao WANG, Juncong LI, Hainan GONG, Jingliang HUANGFU, Yong LIU, 2023: Recent Advances in Understanding Multi-scale Climate Variability of the Asian Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1429-1456.  doi: 10.1007/s00376-023-2266-8
    [9] Weiwei WANG, Song YANG, Tuantuan ZHANG, Qingquan LI, Wei WEI, 2022: Sub-seasonal Prediction of the South China Sea Summer Monsoon Onset in the NCEP Climate Forecast System Version 2, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 1969-1981.  doi: 10.1007/s00376-022-1403-0
    [10] Song YANG, WEN Min, Rongqian YANG, Wayne HIGGINS, ZHANG Renhe, 2011: Impacts of Land Process on the Onset and Evolution of Asian Summer Monsoon in the NCEP Climate Forecast System, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1301-1317.  doi: 10.1007/s00376-011-0167-8
    [11] HUANG Ronghui, CHEN Jilong, HUANG Gang, 2007: Characteristics and Variations of the East Asian Monsoon System and Its Impacts on Climate Disasters in China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 993-1023.  doi: 10.1007/s00376-007-0993-x
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    [13] QIAN Weihong, DING Ting, HU Haoran, LIN Xiang, QIN Aimin, 2009: An Overview of Dry-wet Climate Variability among Monsoon-Westerly Regions and the Monsoon Northernmost Marginal Active Zone in China, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 630-641.  doi: 10.1007/s00376-009-8213-5
    [14] WEI Jiangfeng, WANG Huijun, 2004: A Possible Role of Solar Radiation and Ocean in the Mid-Holocene East Asian Monsoon Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 1-12.  doi: 10.1007/BF02915675
    [15] Wang Huijun, 2000: The Interannual Variability of East Asian Monsoon and Its Relationship with SST in a Coupled Atmosphere-Ocean-Land Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 31-47.  doi: 10.1007/s00376-000-0041-6
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    [19] WANG Zaizhi, WU Guoxiong, WU Tongwen, YU Rucong, 2004: Simulation of Asian Monsoon Seasonal Variations with Climate Model R42L9/LASG, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 879-889.  doi: 10.1007/BF02915590
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    • Manuscript History

    Manuscript received: 10 October 1994
    Manuscript revised: 10 October 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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    The Fractal Dimension Distribution of the Short-Term Climate System in China and It’s Connection with the Monsoon Climate

    • 1. Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008
    • Manuscript received: 1994-10-10
    • Manuscript revised: 1994-10-10

    Abstract: By analyzing the Fractal Dimension (FD) distribution of the Short-range Climate system (SCS) in China, it is found that the FD varies in different region and this just agrees with the regionality of the monsoon climate in China. The FD of the SCS Lays between 2.0 and 5.0. In the vast eastern area of China, the FD almost grows gradually with the latitude. Line 4.0 is along the mountain chains from the Nanlin Mountain to the Wuyi Mountain. North of the line the FD varies only slightly and all are above 4.0. Only in coastal islands the FD is smaller than 3.0.

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