Convective Boundary Layer in the Region of the Monsoon Trough-A Case Study

Surendra S. Parasnis; Savita B. Morwal; K. G. Vernekar

doi:10.1007/BF02919273

Impact Factor: 5.8

Volume 8 Issue 4

Oct. 1991

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1991 > 8(4): 505-509

Convective Boundary Layer in the Region of the Monsoon Trough-A Case Study

1.
Indian Institute of Tropical Meteorology, Pune 411 005, India,Indian Institute of Tropical Meteorology, Pune 411 005, India,Indian Institute of Tropical Meteorology, Pune 411 005, India

doi: 10.1007/BF02919273

Abstract
References
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Abstract:
A case study of the convectively driven monsoon boundary layer has been carried out using the aerological ob-servations at four stations in the region of monsoon trough during Monsoon Trough Boundary Layer Experiment (MONTBLEX) 1988. The Convective Boundary Layer (CBL) in the region of monsoon trough did not show double mixing line structure. A single mixing line representing the CBL with different stabilities with respect to the convective activities was observed.
References

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Manuscript History

Manuscript received: 10 October 1991

Manuscript revised: 10 October 1991

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

Convective Boundary Layer in the Region of the Monsoon Trough-A Case Study

1. Indian Institute of Tropical Meteorology, Pune 411 005, India,Indian Institute of Tropical Meteorology, Pune 411 005, India,Indian Institute of Tropical Meteorology, Pune 411 005, India

Manuscript received: 1991-10-10
Manuscript revised: 1991-10-10

Abstract: A case study of the convectively driven monsoon boundary layer has been carried out using the aerological ob-servations at four stations in the region of monsoon trough during Monsoon Trough Boundary Layer Experiment (MONTBLEX) 1988. The Convective Boundary Layer (CBL) in the region of monsoon trough did not show double mixing line structure. A single mixing line representing the CBL with different stabilities with respect to the convective activities was observed.