FORMATION OF TROPICAL CYCLONES IN THE BAY OF BENGAL
DOI:
https://doi.org/10.54302/mausam.v45i3.2128Keywords:
poisson distribution, Formation probabilites, Cyclonic systems, Non-severe cyclonic storms, severe cyclonic stormsAbstract
of Rengal. For th is purpose, the Ilay of Bengel is divided into number of one degree lat itud eIOlljlilUJc
squa re- crib and the Ic rmetion prob abilities WMe found in each of these cells in different months of bestmon
soon an ti pre-monsoon 30 th et il will help in formul ation of long term plan for the natura l d isa ster redu crion.In
o rde r 10 lind OUI the la titud inal variation offhe formation o rcyclonic stonns. the Bay o( Btnaal is aaain d ivided into
(our sectors with a wi dth o f S-d ("~rte lo ngitude sectors. namely. 80-85. 85-90, 90-9S and 9SoI00. In (hue sectors the
meanloca tion s of'fonnation in terms of'Iatitude was ca lcula ted and discussed . Furt her, the Bay is sub-divided into 14
division s 10 lin.t out the possible spa tial va ria lions using sta tisl ical lech niques.Th e cause c f these spa tial vari ation is
als o discu ssed .
Downloads
Published
How to Cite
Issue
Section
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.
