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The Possible Influence of Stratospheric Sudden Warming on East Asian Weather


doi: 10.1007/s00376-008-0841-7

  • By analyzing the linkage of the Northern Annular Mode (NAM) anomaly to the East Asian jet and the East Asian trough during Stratospheric Sudden Warming (SSW), the influence of SSW on East Asian weather is studied. The results show that the East Asian jet is strengthened and the East Asian trough is deepened during SSW. With the downward propagation of SSW, the strengthened East Asian jet and the East Asian trough would move southward, expand westward and gradually influence the area of north and northeastern China. This implies that the winter monsoon tends to be enhanced over East Asia during SSW.
  • [1] Yingxian ZHANG, Dong SI, Yihui DING, Dabang JIANG, Qingquan LI, Guofu WANG, 2022: Influence of Major Stratospheric Sudden Warming on the Unprecedented Cold Wave in East Asia in January 2021, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 576-590.  doi: 10.1007/s00376-022-1318-9
    [2] ZUO Qunjie, GAO Shouting, LU Daren, 2012: Kinetic and Available Potential Energy Transport during the Stratospheric Sudden Warming in January 2009, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1343-1359.  doi: 10.1007/s00376-012-1198-5
    [3] Jian RAO, Rongcai REN, Haishan CHEN, Xiangwen LIU, Yueyue YU, Yang YANG, 2019: Sub-seasonal to Seasonal Hindcasts of Stratospheric Sudden Warming by BCC_CSM1.1(m): A Comparison with ECMWF, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 479-494.  doi: 10.1007/s00376-018-8165-8
    [4] DENG Shumei, CHEN Yuejuan, HUANG Yong, LUO Tao, BI Yun, 2011: Transient Characteristics of Residual Meridional Circulation during Stratospheric Sudden Warming, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 551-563.  doi: 10.1007/s00376-010-0010-7
    [5] LIU Yi, LIU Chuanxi, Xuexi TIE, GAO Shouting, 2011: Middle Stratospheric Polar Vortex Ozone Budget during the Warming Arctic Winter, 2002--2003, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 985-996.  doi: 10.1007/s00376-010-0045-9
    [6] WANG Huijun, SUN Jianqi, 2009: Variability of Northeast China River Break-up Date, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 701-706.  doi: 10.1007/s00376-009-9035-1
    [7] Yueyue YU, Yafei LI, Rongcai REN, Ming CAI, Zhaoyong GUAN, Wei HUANG, 2022: An Isentropic Mass Circulation View on the Extreme Cold Events in the 2020/21 Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 643-657.  doi: 10.1007/s00376-021-1289-2
    [8] Shui YU, Jianqi SUN, 2024: Persistent Variations in the East Asian Trough from March to April and the Possible Mechanism, ADVANCES IN ATMOSPHERIC SCIENCES, 41, 737-753.  doi: 10.1007/s00376-023-3024-7
    [9] Jian RAO, Siming LIU, Yuanhao CHEN, 2021: Northern Hemisphere Sudden Stratospheric Warming and Its Downward Impact in Four Chinese CMIP6 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 187-202.  doi: 10.1007/s00376-020-0250-0
    [10] ZHOU Baiquan, NIU Ruoyun, ZHAI Panmao, 2015: An Assessment of the Predictability of the East Asian Subtropical Westerly Jet Based on TIGGE Data, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 401-412.  doi: 10.1007/s00376-014-4026-2
    [11] Leying ZHANG, Haiming XU, Ning SHI, Jiechun DENG, 2017: Responses of the East Asian Jet Stream to the North Pacific Subtropical Front in Spring, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 144-156.  doi: 10.1007/s00376-016-6026-x
    [12] GUO Lanli, ZHANG Yaocun, WANG Bin, LI Lijuan, ZHOU Tianjun, BAO Qing, 2008: Simulations of the East Asian Subtropical Westerly Jet by LASG/IAP AGCMs, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 447-457.  doi: 10.1007/s00376-008-0447-0
    [13] ZHANG Yaocun, HUANG Danqing, 2011: Has the East Asian Westerly Jet Experienced a Poleward Displacement in Recent Decades?, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1259-1265.  doi: 10.1007/s00376-011-9185-9
    [14] 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
    [15] Yuhan YAN, Chaofan LI, Riyu LU, 2019: Meridional Displacement of the East Asian Upper-tropospheric Westerly Jet and Its Relationship with the East Asian Summer Rainfall in CMIP5 Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 1203-1216.  doi: 10.1007/s00376-019-9066-1
    [16] LIN Zhongda, 2013: Impacts of two types of northward jumps of the East Asian upper-tropospheric jet stream in midsummer on rainfall in eastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1224-1234.  doi: 10.1007/s00376-012-2105-9
    [17] XIANG Yang, YANG Xiuqun, 2012: The Effect of Transient Eddy on Interannual Meridional Displacement of Summer East Asian Subtropical Jet, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 484-492.  doi: 10.1007/s00376-011-1113-5
    [18] LI Chaofan, LIN Zhongda, 2015: Predictability of the Summer East Asian Upper-Tropospheric Westerly Jet in ENSEMBLES Multi-Model Forecasts, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1669-1682.  doi: 10.1007/s00376-015-5057-z
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Manuscript History

Manuscript received: 10 September 2008
Manuscript revised: 10 September 2008
通讯作者: 陈斌, bchen63@163.com
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The Possible Influence of Stratospheric Sudden Warming on East Asian Weather

  • 1. Anhui Institute of Meteorological Sciences, Hefei 230031; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026;School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026;School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026;School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026;Anhui Institute of Meteorological Sciences, Hefei 230031

Abstract: By analyzing the linkage of the Northern Annular Mode (NAM) anomaly to the East Asian jet and the East Asian trough during Stratospheric Sudden Warming (SSW), the influence of SSW on East Asian weather is studied. The results show that the East Asian jet is strengthened and the East Asian trough is deepened during SSW. With the downward propagation of SSW, the strengthened East Asian jet and the East Asian trough would move southward, expand westward and gradually influence the area of north and northeastern China. This implies that the winter monsoon tends to be enhanced over East Asia during SSW.

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