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Volume 6 Issue 1

Jan.  1989

Article Contents

Analysis of Indian Monsoon and Associated Low-Level Circulation in 1980 and 1981


doi: 10.1007/BF02656922

  • In this paper, Indian monsoon of 1980 and 1981 is analysed based on the seasonal and half-month averaged data of 850 hPa of ECMWF analysis. The results show that Indian monsoon is related to Somali jet, the low-latitude easterlies and the mid-latitude westerlies over southern Indian Ocean, which are associated with the stationary wave of Southern Hemisphere. The forces affecting on the low-level flow are diagnosed, which display the relationship between Indian monsoon and the associated low-level flow.
  • [1] Jun LI, Hongbin CHEN, Zhanqing LI, Pucai WANG, Xuehua FAN, Wenying HE, Jinqiang ZHANG, 2019: Analysis of Low-level Temperature Inversions and Their Effects on Aerosols in the Lower Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 1235-1250.  doi: 10.1007/s00376-019-9018-9
    [2] Chunguang CUI, Wen ZHOU, Hao YANG, Xiaokang WANG, Yi DENG, Xiaofang WANG, Guirong XU, Jingyu WANG, 2023: Analysis of the Characteristics of the Low-level Jets in the Middle Reaches of the Yangtze River during the Mei-yu Season, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 711-724.  doi: 10.1007/s00376-022-2107-1
    [3] Marco Y. T. LEUNG, Wen ZHOU, Chi-Ming SHUN, Pak-Wai CHAN, 2018: Large-scale Circulation Control of the Occurrence of Low-level Turbulence at Hong Kong International Airport, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 435-444.  doi: 10.1007/s00376-017-7118-y
    [4] Zhong Zhong, Wang Hanjie, 2000: A Study of the Relationship between Low-level Jet and Inversion Layer over an Agroforest Ecosystem in East China Plain?, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 299-310.  doi: 10.1007/s00376-000-0011-z
    [5] DAI Fushan, YU Rucong, ZHANG Xuehong, YU Yongqiang, LI Jianglong, 2003: The Impact of Low-Level Cloud over the Eastern Subtropical Pacific on the "Double ITCZ" in LASG FGCM-0, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 461-474.  doi: 10.1007/BF02690804
    [6] Yong CHEN, Junling AN, Yele SUN, Xiquan WANG, Yu QU, Jingwei ZHANG, Zifa WANG, Jing DUAN, 2018: Nocturnal Low-level Winds and Their Impacts on Particulate Matter over the Beijing Area, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1455-1468.  doi: 10.1007/s00376-018-8022-9
    [7] Peiling FU, Kefeng ZHU, Kun ZHAO, Bowen ZHOU, Ming XUE, 2019: Role of the Nocturnal Low-level Jet in the Formation of the Morning Precipitation Peak over the Dabie Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 15-28.  doi: 10.1007/s00376-018-8095-5
    [8] Yuhan LUO, Yu DU, 2023: The Roles of Low-level Jets in “21·7” Henan Extremely Persistent Heavy Rainfall Event, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 350-373.  doi: 10.1007/s00376-022-2026-1
    [9] Xuanyu LIU, Guixing CHEN, Sijia ZHANG, Yu DU, 2023: Formation of Low-Level Jets over Southern China in the Mei-yu Season, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1731-1748.  doi: 10.1007/s00376-023-2358-5
    [10] DAI Fushan, YU Rucong, ZHANG Xuehong, YU Yongqiang, LI Jianglong, 2005: Impacts of an Improved Low-Level Cloud Scheme on the Eastern Pacific ITCZ-Cold Tongue Complex, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 559-574.  doi: 10.1007/BF02918488
    [11] P.N. Mahajan, V.R. Mujumdar, S.P. Ghanekar, 1989: Excitation of Low-level Jet as Seen by GOES (I-O) Satellite off the Somali Coast, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 475-482.  doi: 10.1007/BF02659081
    [12] Zhou Jun, Walter K. Henry, 1987: THE INTERFACE EFFECT AND THE FORMATION OF A LOW-LEVEL JET ALONG THE EAST SIDE OF THE ROCKY MOUNTAINS, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 175-184.  doi: 10.1007/BF02677064
    [13] Huijie WANG, Jianhua SUN, Shenming FU, Yuanchun ZHANG, 2021: Typical Circulation Patterns and Associated Mechanisms for Persistent Heavy Rainfall Events over Yangtze–Huaihe River Valley during 1981–2020, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 2167-2182.  doi: 10.1007/s00376-021-1194-8
    [14] LI Jun, CHEN Hongbin, Zhanqing LI, WANG Pucai, Maureen CRIBB, FAN Xuehua, 2015: Low-Level Temperature Inversions and Their Effect on Aerosol Condensation Nuclei Concentrations under Different Large-Scale Synoptic Circulations, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 898-908.  doi: 10.1007/s00376-014-4150-z
    [15] LI Chongyin, PAN Jing, 2006: Atmospheric Circulation Characteristics Associated with the Onset of Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 925-939.  doi: 10.1007/s00376-006-0925-1
    [16] M. Sankar-Rao, V. N. Lykossov, E. M. Volodin, A. E. Nikitin, A. I. Degtiarev, Kusuma G. Rao, 1991: Relationships between the Global General Circulation and the Indian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 137-148.  doi: 10.1007/BF02658090
    [17] 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
    [18] Yu ZHAO, Anmin DUAN, Guoxiong WU, 2018: Interannual Variability of Late-spring Circulation and Diabatic Heating over the Tibetan Plateau Associated with Indian Ocean Forcing, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 927-941.  doi: 10.1007/s00376-018-7217-4
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    [20] Ya GAO, Huijun WANG, Dong CHEN, 2017: Interdecadal Variations of the South Asian Summer Monsoon Circulation Variability and the Associated Sea Surface Temperatures on Interannual Scales, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 816-832.  doi: 10.1007/ s00376-017-6246-8

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Manuscript History

Manuscript received: 10 January 1989
Manuscript revised: 10 January 1989
通讯作者: 陈斌, bchen63@163.com
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Analysis of Indian Monsoon and Associated Low-Level Circulation in 1980 and 1981

  • 1. Department of Geophysics, Peking University, Beijing

Abstract: In this paper, Indian monsoon of 1980 and 1981 is analysed based on the seasonal and half-month averaged data of 850 hPa of ECMWF analysis. The results show that Indian monsoon is related to Somali jet, the low-latitude easterlies and the mid-latitude westerlies over southern Indian Ocean, which are associated with the stationary wave of Southern Hemisphere. The forces affecting on the low-level flow are diagnosed, which display the relationship between Indian monsoon and the associated low-level flow.

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