On the presence of upper air divergence in relation to pre-monsoon and monsoon weather systems of the MONEX period 1979
A case of formation of a cyclonic storm in the Bay of Bengal and some cases of intensification of equatorial trough during pre-monsoon period were studied with the help of GOES-l satellite wind flow data, It could be inferred that divergence in these cases was mostly generated and the development took place without the movement of any pre-existing divergent system aloft, Onset of the southwest monsoon along the west coast, together with formation of a cyclonic storm in the Arabian Sea and three other cases of formation of depression in the Bay of Bengal were examined in light of the above wind flow data, The development of these systems took place in the presence of upper air divergence systems.
How to Cite
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