The Convective Boundary Layer over the Deccan Plateau, India during the summer monsoon
β Scribed by Surendra S. Parasnis; Savita B. Morwal
- Publisher
- Springer
- Year
- 1991
- Tongue
- English
- Weight
- 575 KB
- Volume
- 54
- Category
- Article
- ISSN
- 0006-8314
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β¦ Synopsis
The thermodynamic structure of the Convective Boundary Layer (CBL) over the Deccan Plateau, India has been investigated using serological data during the summer monsoon seasons of 1980 and 1981. Conserved-variable analysis and the saturation-point approach, which were used in this study. suggest that the top of the CBL varied between 700-600 mb during the monsoon. The air above the top of the CBL during a weak monsoon was estimated to have subsided for 4 days with a subsidence rate of 30 mb day-'.
π SIMILAR VOLUMES
Aerological observations over a tropical inland station collected during different phases of the Indian summer monsoon have been used to study the convective mixing in the monsoon boundary layer. The mixing line (ML) model for the thermodynamic structure of a partially cloudy boundary layer has been
## Abstract In this study, 20 years (1961β1980) of rainfall data for 34 stations over Thailand are used to investigate and understand the intraseasonal and interannual variability of the summer monsoon. Dominant structures of 5βday and seasonal rainfall are determined through empirical orthogonal f