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Volume 7 Issue 1

Jan.  1990

Article Contents

A Diagnostic Analysis of Winter Atmospheric Circulation during the 1982-1983 ENSO Event


doi: 10.1007/BF02919168

  • In this paper, the winter atmospheric circulation, the convection along the equator and their variations of 1982 und 1983 are investigated. It is suggested that there was a well organized three dimensional structure of anomalies of the atmospheric circulations during 1982 winter which may be related to the variations of the convection in the equa-torial region.
  • [1] Shou Shaowen, Zhu Aimin, 1993: Diagnostic Study of a Winter Snowstorm Event, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 428-434.  doi: 10.1007/BF02656967
    [2] Qiu Yongyan, 1993: On the Seasonal Transition and the Interannual Variability in Global Kinetic Energy at 500 hPa, Accompanied with Anomalies of Energy during the 1982 / 83 ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 248-256.  doi: 10.1007/BF02919148
    [3] Zhu Weijun, Sun Zhaobo, 1999: Influence of ENSO Event on the Maintenance of Pacific Storm Track in the Northern Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 630-640.  doi: 10.1007/s00376-999-0037-9
    [4] Tae-Won PARK, Jee-Hoon JEONG, Chang-Hoi HO, Seong-Joong KIM, 2008: Characteristics of Atmospheric Circulation Associated with Cold Surge Occurrences in East Asia: A Case Study During 2005/06 Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 791-804.  doi: 10.1007/s00376-008-0791-0
    [5] K. Gambo, Lu Li, Li Weijing, 1987: NUMERICAL SIMULATION OF EURASIAN TELECONNECTION PATTERN IN ATMOSPHERIC CIRCULATION DURING THE NORTHERN HEMISPHERE WINTER, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 385-394.  doi: 10.1007/BF02656739
    [6] Lu LIU, Lingkun RAN, Shouting GAO, 2018: Analysis of the Characteristics of Inertia-Gravity Waves during an Orographic Precipitation Event, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 604-620.  doi: 10.1007/s00376-017-7159-2
    [7] Yuan Zhuojian, Jian Maoqiu, 2001: Diagnostic Equations for the Walker Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 166-178.  doi: 10.1007/s00376-001-0011-7
    [8] ZHOU Putian, SUO Lingling, YUAN Jiacan, TAN Benkui, 2012: The East Pacific Wavetrain: Its Variability and Impact on the Atmospheric Circulation in the Boreal Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 471-483.  doi: 10.1007/s00376-011-0216-3
    [9] ZENG Gang, Wei-Chyung WANG, SUN Zhaobo, LI Zhongxian, 2011: Atmospheric Circulation Cells Associated with Anomalous East Asian Winter Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 913-926.  doi: 10.1007/s00376-010-0100-6
    [10] Jianqi ZHANG, Chongyin LI, Xin LI, Chao ZHANG, Jingjing CHEN, 2021: The Asymmetric Atmospheric Response to the Decadal Variability of Kuroshio Extension during Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 785-799.  doi: 10.1007/s00376-020-0264-7
    [11] ZHAO Sixiong, BEI Naifang, SUN Jianhua, 2007: Mesoscale Analysis of a Heavy Rainfall Event over Hong Kong During a Pre-rainy Season in South China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 555-572.  doi: 10.1007/s00376-007-0555-2
    [12] Xu Jianjun, 1994: Statistical Regression Analysis of Response of Northern Mid and Upper Tropospheric Circulation to Winter Eurasian Snow Cover Effects, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 415-420.  doi: 10.1007/BF02658161
    [13] Manman MA, Xiaogang HUANG, Jianfang FEI, Chi ZHANG, Chao LI, Xiaoping CHENG, 2022: Analysis of the Winter Cloud-to-Ground Lightning Activity and Its Synoptic Background in China during 2010–20, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 985-998.  doi: 10.1007/s00376-021-1260-2
    [14] WANG Lili, WANG Yuesi, SUN Yang, LI Yuanyuan, 2012: Using Synoptic Classification and Trajectory Analysis to Assess Air Quality during the Winter Heating Period in Urumqi, China, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 307-319.  doi: 10.1007/s00376-011-9234-4
    [15] Ja-Yeon MOON, Kyung-Ja HA, 2003: Association between Tropical Convection and Boreal Wintertime Extratropical Circulation in 1982/83 and 1988/89, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 593-603.  doi: 10.1007/BF02915502
    [16] Ting HUA, Xunming WANG, 2018: Temporal and Spatial Variations in the Climate Controls of Vegetation Dynamics on the Tibetan Plateau during 1982-2011, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1337-1346.  doi: 10.1007/s00376-018-7064-3
    [17] Yuting ZHANG, Xiaole PAN, Yu TIAN, Hang LIU, Xueshun CHEN, Baozhu GE, Zhe WANG, Xiao TANG, Shandong LEI, Weijie YAO, Yuanzhe REN, Yongli TIAN, Jie LI, Pingqing FU, Jinyuan XIN, Yele SUN, Junji CAO, Zifa WANG, 2022: Transport Patterns and Potential Sources of Atmospheric Pollution during the XXIV Olympic Winter Games Period, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 1608-1622.  doi: 10.1007/s00376-022-1463-1
    [18] Wenyue HE, Bo SUN, Huijun WANG, 2021: Dominant Modes of Interannual Variability in Atmospheric Water Vapor Content over East Asia during Winter and Their Associated Mechanisms, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1706-1722.  doi: 10.1007/s00376-021-0014-5
    [19] ZHOU Li, XU Xiangde, DING Guoan, ZHOU Mingyu, CHENG Xinghong, 2005: Diurnal Variations of Air Pollution and Atmospheric Boundary Layer Structure in Beijing During Winter 2000/2001, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 126-132.  doi: 10.1007/BF02930876
    [20] LI Lun, ZHANG Renhe, WEN Min, 2011: Diagnostic Analysis of the Evolution Mechanism for a Vortex over the Tibetan Plateau in June 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 797-808.  doi: 10.1007/s00376-010-0027-y

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Manuscript History

Manuscript received: 10 January 1990
Manuscript revised: 10 January 1990
通讯作者: 陈斌, bchen63@163.com
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A Diagnostic Analysis of Winter Atmospheric Circulation during the 1982-1983 ENSO Event

  • 1. Institute of Atmospheric Physics, Academia Sinica, Beijing 100080,Institute of Atmospheric Physics, Academia Sinica, Beijing 100080

Abstract: In this paper, the winter atmospheric circulation, the convection along the equator and their variations of 1982 und 1983 are investigated. It is suggested that there was a well organized three dimensional structure of anomalies of the atmospheric circulations during 1982 winter which may be related to the variations of the convection in the equa-torial region.

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