The mean Jet Stream over India and Burma in winter
DOI:
https://doi.org/10.54302/mausam.v4i2.4799Abstract
The mean jet stream over the Indian sub-continent and Burma has been computed from all available radiosonde data and is found to exist at about 27°N at an altitude of 12 km. No secondary' equatorial jet' as postulated by Chaudhury (1950) is found.
A study of the mean distribution of thermal gradients and lapse rates in the troposphere has been made both for the Indian cross section and the Hess' cross section for North America. The thermodynamic properties of the jet stream typified by the cross sections have been compared. It is found that the gradient of the lapse rate concentrates into a maximum in the vicinity of the jet stream. The occurrence of the two types of jet streams is discussed from thermodynamic considerations.
Downloads
Downloads
Published
License
Copyright (c) 2021 MAUSAM
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
All articles published by MAUSAM are licensed under the Creative Commons Attribution 4.0 International License. This permits anyone.
Anyone is free:
- To Share - to copy, distribute and transmit the work
- To Remix - to adapt the work.
Under the following conditions:
- Share - copy and redistribute the material in any medium or format
- Adapt - remix, transform, and build upon the material for any purpose, even
commercially.
