Prelims: Current events of national and international importance
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The cyclonic disturbances over the North Indian Ocean, which include the Arabian Sea, the Bay of Bengal, and the land area in between, have changed drastically over the last century.
- Major trends - There are 4 major trends.
- Shifting of frequency - First, the frequency of cyclonic disturbances has shifted significantly.
- The below plots annual disturbances (left axis) alongside a 10-year rolling average (right axis) from 1900 to 2025.
- The chart reveals a distinct inverted U-shaped trend in the past century.

- Drop-in activity - Second, the overall decline in disturbances in recent years is driven almost entirely by a sharp drop in activity within the Bay of Bengal.
- The below chart breaks down the 10-year rolling average of cyclonic disturbances by origin: the Bay of Bengal, the Arabian Sea, and inland/other areas.

- The Arabian Sea has seen a marked increase in activity, though its frequency remains lower than that of the Bay even in recent years.
- Increase in severity - Third, while the number of disturbances has decreased, their severity has intensified.
- Typically, a disturbance begins as a low-pressure area (winds <31 kmph) and can intensify into a depression (31–49 kmph) or a deep depression (50-61 kmph).
- Beyond this point, they are classified as cyclonic storms (62-88 kmph) or severe cyclonic storms (89-117 kmph).
- The most destructive stages follow: very severe (118-166 kmph), extremely severe (167-221 kmph), and super cyclonic storms (≥222 kmph).
- The below chart illustrates the percentage of disturbances that intensify into severe cyclonic storms or higher.

- Generally, warmer oceans provide more energy to tropical storms, making cyclones stronger and their paths harder to predict.
- Data show that the Arabian Sea is heating up more than average, leading to more intense, tougher-to-predict cyclones.
- Shift in seasonality - Fourth, there has been a significant shift in the seasonality of these storms.
- In the Bay of Bengal, disturbances are increasingly originating in the final quarter of the year (October–December) rather than in the July–September window.
Reference
The Hindu | Trends reshaping Indian ocean