Advanced Search
Impact Factor: 5.8

Volume 13 Issue 4

Oct.  1996

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1996 >  13(4): 411-424

Numerical Simulation of the Effect of the SST Anomalies in the Tropical Western Pacific on the Blocking Highs over the Northeastern Asia

  • 1.

    Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080


doi: 10.1007/BF03342034

  • The effects of the sea surface temperature (SST) anomalies in the tropical western Pacific on the atmospheric cir-culation anomalies over East Asia are simulated by the IAP-GCM with an observed and idealized distributions of the SST anomalies in the tropical western Pacific, respectively Firstly, the atmospheric circulation anomalies during July and August, 1980 are simulated by three anomalous experiments including the global SST anomaly experiment, the tropical SST anomaly experiment and the extratropical SST anomaly experiment, using the observed SST anomalies in 1980. It is shown that the SST anomalies in the tropical ocean greatly influence the formation and maintenance of the blocking high over the northeastern Asia, and may play a more important role than the SST anomalies in the extratropical ocean in the influence on the atmospheric circulation anomalies Secondly, the effects of the SST anomalies in the tropical western Pacific on the atmospheric circulation anoma?lies over East Asia are also simulated with an idealized distribution of the SST anomalies in the tropical western Paci?fic. The simulated results show that the negative anomalies of SST in the tropical western Pacific have a significant ef?fect on the formation and maintenance of the blocking high over the northeastern Asia.
  • [1] Sun Shuqing, Ying Ming, 1999: Subtropical High Anomalies over the Western Pacific and Its Relations to the Asian Monsoon and SST Anomaly, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 559-568.  doi: 10.1007/s00376-999-0031-2
    [2] Huang Fei, Zhou Faxiu, Qian Xiaodan, 2002: Interannual and Decadal Variability of the North Pacific Blocking and Its Relationship to SST,Teleconnection and Storm Tracks, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 807-820.  doi: 10.1007/s00376-002-0046-4
    [3] Yihui DING, Yunyun LIU, Zeng-Zhen HU, 2021: The Record-breaking Mei-yu in 2020 and Associated Atmospheric Circulation and Tropical SST Anomalies, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1980-1993.  doi: 10.1007/s00376-021-0361-2
    [4] LUO Xia, FEI Jianfang, HUANG Xiaogang, CHENG Xiaoping, YU Kun, 2015: Remote Impact of Blocking Highs on the Sudden Track Reversal of Tropical Cyclones, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1517-1532.  doi: 10.1007/s00376-015-4284-7
    [5] Huanlian LI, Huijun WANG, Dabang JIANG, 2017: Influence of October Eurasian Snow on Winter Temperature over Northeast China, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 116-126.  doi: 10.1007/s00376-016-5274-0
    [6] LIU Qinyu, WEN Na, YU Yongqiang, 2006: The Role of the Kuroshio in the Winter North Pacific Ocean-Atmosphere Interaction: Comparison of a Coupled Model and Observations, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 181-189.  doi: 10.1007/s00376-006-0181-4
    [7] Ji Liren, Sun Shuqing, Klaus Arpe, Lennart Benglsson, 1997: Model Study on the Interannual Variability of Asian Winter Monsoon and Its Influence, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 1-22.  doi: 10.1007/s00376-997-0039-4
    [8] Luo Dehai, Li Jianping, 2001: Interaction between a Slowly Moving Planetary-Scale Dipole Envelope Rossby Soliton and a Wavenumber-Two Topography in a Forced Higher Order Nonlinear Schr dinger Equation, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 239-256.  doi: 10.1007/s00376-001-0017-1
    [9] CAO Jie, LU Riyu, HU Jinming, WANG Hai, 2013: Spring Indian Ocean-Western Pacific SST Contrast and the East Asian Summer Rainfall Anomaly, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1560-1568.  doi: 10.1007/s00376-013-2298-6
    [10] Yujie WU, Wansuo DUAN, 2018: Impact of SST Anomaly Events over the Kuroshio-Oyashio Extension on the "Summer Prediction Barrier", ADVANCES IN ATMOSPHERIC SCIENCES, 35, 397-409.  doi: 10.1007/s00376-017-6322-0
    [11] Wu Renguang, Chen Lieting, 1995: Interannual Fluctuations of Surface Air Temperature over North America and Its Relationship to the North Pacific SST Anomaly, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 20-28.  doi: 10.1007/BF02661284
    [12] WANG Hai, and LIU Qinyu, 2014: Boreal Winter Rainfall Anomaly over the Tropical Indo-Pacific and Its Effect on Northern Hemisphere Atmospheric Circulation in CMIP5 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 916-925.  doi: 10.1007/s00376-013-3174-0
    [13] Wang Huijun, 1997: The Effect of Heating Anomaly on the Asian Circulation-A GCM Experiment, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 81-86.  doi: 10.1007/s00376-997-0046-5
    [14] Huang Ronghui, Lu Li, 1989: Numerical Simulation of the Relationship between the Anomaly of Subtropical High over East Asia and the Convective Activities in the Western Tropical Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 202-214.  doi: 10.1007/BF02658016
    [15] Ji Jinjun, 1986: A SIMPLIFIED MODEL STUDY ON THE SHORT-TERM CLIMATIC EFFECT OF SNOWFALL ANOMALY IN MID-HIGH LATITUDES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 443-453.  doi: 10.1007/BF02657934
    [16] 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
    [17] HUANG Ping, HUANG Ronghui, 2009: Delayed Atmospheric Temperature Response to ENSO SST: Role of High SST and the Western Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 343-351.  doi: 10.1007/s00376-009-0343-2
    [18] Kevin HAMILTON, 2006: High Resolution Global Modeling of the Atmospheric Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 842-856.  doi: 10.1007/s00376-006-0842-3
    [19] Fei ZHENG, Jianping LI, Fred KUCHARSKI, Ruiqiang DING, Ting LIU, 2018: Dominant SST Mode in the Southern Hemisphere Extratropics and Its Influence on Atmospheric Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 881-895.  doi: 10.1007/s00376-017-7162-7
    [20] Guo Yufu, Chao Jiping, 1984: SIMPLIFIED DYNAMICAL ANOMALY MODEL FOR LONG-RANGE NUMERICAL FORECASTS, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 30-52.  doi: 10.1007/BF03187614
PDF

Get Citation+

shu
Export:  

Share Article

Article Metrics

Article Views: 1365 Times

PDF downloads: 1178 Times

Cited by: Times
  • 加载中

    • Manuscript History

    Manuscript received: 10 October 1996
    Manuscript revised: 10 October 1996
    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

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Numerical Simulation of the Effect of the SST Anomalies in the Tropical Western Pacific on the Blocking Highs over the Northeastern Asia

    • 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080
    • Manuscript received: 1996-10-10
    • Manuscript revised: 1996-10-10

    Abstract: The effects of the sea surface temperature (SST) anomalies in the tropical western Pacific on the atmospheric cir-culation anomalies over East Asia are simulated by the IAP-GCM with an observed and idealized distributions of the SST anomalies in the tropical western Pacific, respectively Firstly, the atmospheric circulation anomalies during July and August, 1980 are simulated by three anomalous experiments including the global SST anomaly experiment, the tropical SST anomaly experiment and the extratropical SST anomaly experiment, using the observed SST anomalies in 1980. It is shown that the SST anomalies in the tropical ocean greatly influence the formation and maintenance of the blocking high over the northeastern Asia, and may play a more important role than the SST anomalies in the extratropical ocean in the influence on the atmospheric circulation anomalies Secondly, the effects of the SST anomalies in the tropical western Pacific on the atmospheric circulation anoma?lies over East Asia are also simulated with an idealized distribution of the SST anomalies in the tropical western Paci?fic. The simulated results show that the negative anomalies of SST in the tropical western Pacific have a significant ef?fect on the formation and maintenance of the blocking high over the northeastern Asia.

      HTML

    Catalog

      Publish with AAS

      Contact us

      Links

      Copyright © 2018-2028 ADVANCES IN ATMOSPHERIC SCIENCES 京ICP备14024088号-7

      Supported by: Beijing Renhe Information Technology Co. Ltd  support: info@rhhz.net  

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return