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On the Spatio-Temporal Variations of the Tropopause Height over India and Indian Summer Monsoon Activity


doi: 10.1007/BF02656973

  • The spatio-temporal variation of the tropopause height (TH) over the Indian region (5°N-35°N, 70°E-95°E) has been studied using monthly mean TH data, for 22-year period, 1965 to 1986. The study revealed that the stations south of 20° showed maximum TH in April / May and minimum in September. This variation in TH has been attributed to the corresponding variation of average sea surface temperature (SST) over ± 20° latitudinal belt over Indian Ocean, Arabian Sea and Bay of Bengal. Further the stations north of 20°N showed maximum in June and minimum in October/ November. This maximum in TH has primarily been attributed to the increased insolation and convection. Furthermore it is noticed that the anomaly of TH moved northwards during the period April to July.The interannual variability of the Indian Summer Monsoon Activity (ISMA) has been studied in relation to all India mean TH (at 12 GMT) for six months April through September. The composites of mean TH for good and bad monsoon years showed that all India mean TH is statistically higher in good monsoon years than in bad monsoon years. The relationship between ISMA and all India mean May TH has been studied using the contingency table. The study suggested that the forecast of ISMA could be prepared using mean May TH.
  • [1] Zhao Bolin, Li Wanbiao, Zhu Yuanjing, 1994: Study on Atmospheric Ozone in East Asia with Satellite Observation, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 27-35.  doi: 10.1007/BF02656990
    [2] Ji Zhengang, Chao Jiping, 1987: TELECONNECTIONS OF THE SEA SURFACE TEMPERATURE IN THE INDIAN OCEAN WTTH SEA SURFACE TEMPERATURE IN THE EASTERN EQUATORIAL PACIFIC, AND WITH THE 500 hPa GEOPOTENTIAL HEIGHT FIELD IN THE NORTHERN HEMISPHERE, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 343-348.  doi: 10.1007/BF02663604
    [3] B. KNOPF, K. ZICKFELD, M. FLECHSIG, V. PETOUKHOV, 2008: Sensitivity of the Indian Monsoon to Human Activities, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 932-945.  doi: 10.1007/s00376-008-0932-5
    [4] BIAN Jianchun, CHEN Hongbin, 2008: Statistics of the Tropopause Inversion Layer over Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 381-386.  doi: 10.1007/s00376-008-0381-1
    [5] ZHU Congwen, Chung-Kyu PARK, Woo-Sung LEE, Won-Tae YUN, 2008: Statistical Downscaling for Multi-Model Ensemble Prediction of Summer Monsoon Rainfall in the Asia-Pacific Region Using Geopotential Height Field, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 867-884.  doi: 10.1007/s00376-008-0867-x
    [6] ZHANG Min, TIAN Wenshou, CHEN Lei, LU Daren, 2010: Cross-Tropopause Mass Exchange Associated with a Tropopause Fold Event over the Northeastern Tibetan Plateau, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 1344-1360.  doi: 10.1007/s00376-010-9129-9
    [7] WU Bingyi, 2005: Weakening of Indian Summer Monsoon in Recent Decades, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 21-29.  doi: 10.1007/BF02930866
    [8] S.G. Narkhedkar, 1995: The Variability of the Interannual Oscillations of the Indian Summer Monsoon Rainfall, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 95-102.  doi: 10.1007/BF02661291
    [9] J.M. Pathan, 1994: Diurnal Variation of Southwest Monsoon Rainfall at Indian Stations, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 111-120.  doi: 10.1007/BF02657000
    [10] Lifeng LI, Xin LI, Xiong CHEN, Chongyin LI, Jianqi ZHANG, Yulong SHAN, 2020: Modulation of Madden-Julian Oscillation Activity by the Tropical Pacific-Indian Ocean Associated Mode, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 1375-1388.  doi: 10.1007/s00376-020-0002-1
    [11] Olivia MARTIUS, Cornelia SCHWIERZ, Michael SPRENGER, 2008: Dynamical Tropopause Variability and Potential Vorticity Streamers in the Northern Hemisphere ---A Climatological Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 367-380.  doi: 10.1007/s00376-008-0367-z
    [12] Chen Yingyi, 1993: Predictability of the 500 hPa Height Field, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 497-503.  doi: 10.1007/BF02656975
    [13] S. V. Singh, S. R. Inamdar, R. H. Kripalani, K. D. Prasad, 1986: RELATIONSHIP BETWEEN 500 hPa RIDGE AXIS POSITIONS OVER THE INDIAN AND THE WEST PACIFIC REGIONS AND THE INDIAN SUMMER MONSOON RAINFALL, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 349-359.  doi: 10.1007/BF02678655
    [14] Zhang Minghua, Yu Rucong, Yu Yongqiang, 2001: Comparing Cloud Radiative Properties between the Eastern China and the Indian Monsoon Region, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1090-1102.  doi: 10.1007/s00376-001-0025-1
    [15] D.M. CHATE, RT. . WAGHMARE, C.K. JENA, V. GOPALAKRISHNAN, P. MURUGAVEL, Sachin D. GHUDE, Rachana KULKARNI, P.C. S. DEVARA, 2018: Cloud Condensation Nuclei over the Bay of Bengal during the Indian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 218-223.  doi: 10.1007/s00376-017-6331-z
    [16] Yuli ZHANG, Chuanxi LIU, Yi LIU, Rui YANG, 2019: Intraseasonal Oscillation of Tropospheric Ozone over the Indian Summer Monsoon Region, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 417-430.  doi: 10.1007/s00376-018-8113-7
    [17] P. N. Mahajan, V. R. Mujumdar, S. P. Ghanekar, 1986: THE BURST OF INDIAN SUMMER MONSOON AS REVEALED BY GOES SATELLITE DURING MONEX 1979, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 514-519.  doi: 10.1007/BF02657941
    [18] B.Parthasarathy, Song Yang, 1995: Relationships between Regional Indian Summer Monsoon Rainfall and Eurasian Snow Cover, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 143-150.  doi: 10.1007/BF02656828
    [19] K.D. Prasad, S.V. Singh, 1988: MONSOON RAINFALL AND SOUTHERN OSCILLATION RESPONSES IN THE PRESSURES OVER THE NORTHERN INDIAN OCEAN, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 243-251.  doi: 10.1007/BF02656785
    [20] Tao Zuyu, 1989: Analysis of Indian Monsoon and Associated Low-Level Circulation in 1980 and 1981, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 113-119.  doi: 10.1007/BF02656922

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Manuscript History

Manuscript received: 10 October 1993
Manuscript revised: 10 October 1993
通讯作者: 陈斌, bchen63@163.com
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On the Spatio-Temporal Variations of the Tropopause Height over India and Indian Summer Monsoon Activity

  • 1. Indian Institute of Tropical Meteorology, Pashan, Pune-411008, India,Indian Institute of Tropical Meteorology, Pashan, Pune-411008, India

Abstract: The spatio-temporal variation of the tropopause height (TH) over the Indian region (5°N-35°N, 70°E-95°E) has been studied using monthly mean TH data, for 22-year period, 1965 to 1986. The study revealed that the stations south of 20° showed maximum TH in April / May and minimum in September. This variation in TH has been attributed to the corresponding variation of average sea surface temperature (SST) over ± 20° latitudinal belt over Indian Ocean, Arabian Sea and Bay of Bengal. Further the stations north of 20°N showed maximum in June and minimum in October/ November. This maximum in TH has primarily been attributed to the increased insolation and convection. Furthermore it is noticed that the anomaly of TH moved northwards during the period April to July.The interannual variability of the Indian Summer Monsoon Activity (ISMA) has been studied in relation to all India mean TH (at 12 GMT) for six months April through September. The composites of mean TH for good and bad monsoon years showed that all India mean TH is statistically higher in good monsoon years than in bad monsoon years. The relationship between ISMA and all India mean May TH has been studied using the contingency table. The study suggested that the forecast of ISMA could be prepared using mean May TH.

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