THE BURST OF INDIAN SUMMER MONSOON AS REVEALED BY GOES SATELLITE DURING MONEX 1979

P. N. Mahajan; V. R. Mujumdar; S. P. Ghanekar

doi:10.1007/BF02657941

Impact Factor: 5.8

Volume 3 Issue 4

Oct. 1986

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1986 > 3(4): 514-519

THE BURST OF INDIAN SUMMER MONSOON AS REVEALED BY GOES SATELLITE DURING MONEX 1979

1.
Indian Institute of Tropical Meteorology, Pune-411005, India,Indian Institute of Tropical Meteorology, Pune-411005, India,Indian Institute of Tropical Meteorology, Pune-411005, India

doi: 10.1007/BF02657941

Abstract
References
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Abstract:
During FGGE year 1979, low-level air flow over the western Indian Ocean was determined from the analysis of GOES images (5－20 June). The wind pattern shows sudden change in low-level air circulation over western Indian Ocean during the initial burst of summer monsoon. The burst of monsoon is characte-rized by sudden establishment of low-level jet and strong cross-equatorial flow. This abrupt change signals the beginning of southwest monsoon over India and it is associated with the first monsoon rainfall over the southern part of western coast of India. Sudden change in low-level air flow is followed by the burst of monsoon within 3－5 days.
References

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Manuscript History

Manuscript received: 10 October 1986

Manuscript revised: 10 October 1986

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

THE BURST OF INDIAN SUMMER MONSOON AS REVEALED BY GOES SATELLITE DURING MONEX 1979

1. Indian Institute of Tropical Meteorology, Pune-411005, India,Indian Institute of Tropical Meteorology, Pune-411005, India,Indian Institute of Tropical Meteorology, Pune-411005, India

Manuscript received: 1986-10-10
Manuscript revised: 1986-10-10

Abstract: During FGGE year 1979, low-level air flow over the western Indian Ocean was determined from the analysis of GOES images (5－20 June). The wind pattern shows sudden change in low-level air circulation over western Indian Ocean during the initial burst of summer monsoon. The burst of monsoon is characte-rized by sudden establishment of low-level jet and strong cross-equatorial flow. This abrupt change signals the beginning of southwest monsoon over India and it is associated with the first monsoon rainfall over the southern part of western coast of India. Sudden change in low-level air flow is followed by the burst of monsoon within 3－5 days.