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Environment & Climate25 Oct 2026 · about 6 min

Andhra braces for very severe cyclonic storm; Odisha activates disaster mitigation machinery | LIVE

The brief

A very severe cyclonic storm is a high-strength tropical cyclone category used by the India Meteorological Department. In the North Indian Ocean classification, it generally means sustained winds of about 118 to 166 kmph. Such a system can produce destructive winds, intense rain, coastal flooding and dangerous seas. The article identifies the Bay of Bengal system as likely to strengthen into this category. “Storm” is a broad everyday word. It can describe many weather events, from thunderstorms to powerful cyclones. A very severe cyclonic storm is more specific. Its classification is based mainly on sustained wind speed, while gusts can be even stronger. The article forecasts gusts up to 140 kmph when the system reaches the coast. The distinction matters because stronger storms require faster, wider preparation. Andhra Pradesh officials were told to warn fishermen, alert low-lying communities and prepare emergency assistance. The expected landfall is therefore being treated as a major coastal threat, not simply as a period of ordinary rain.

01

What is a very severe cyclonic storm, and how is it different from an ordinary storm?

A very severe cyclonic storm is a high-strength tropical cyclone category used by the India Meteorological Department. In the North Indian Ocean classification, it generally means sustained winds of about 118 to 166 kmph. Such a system can produce destructive winds, intense rain, coastal flooding and dangerous seas. The article identifies the Bay of Bengal system as likely to strengthen into this category.

“Storm” is a broad everyday word. It can describe many weather events, from thunderstorms to powerful cyclones. A very severe cyclonic storm is more specific. Its classification is based mainly on sustained wind speed, while gusts can be even stronger. The article forecasts gusts up to 140 kmph when the system reaches the coast.

The distinction matters because stronger storms require faster, wider preparation. Andhra Pradesh officials were told to warn fishermen, alert low-lying communities and prepare emergency assistance. The expected landfall is therefore being treated as a major coastal threat, not simply as a period of ordinary rain.

02

When and where is the cyclone expected to cross the coast, and how strong could its winds be?

The India Meteorological Department expects the system to cross the Andhra Pradesh and Yanam coasts between Bapatla and Visakhapatnam. The forecast landfall is during the forenoon of October 28. This gives authorities and residents a defined coastal zone and a limited window for preparations.

The cyclone is likely to strengthen into a very severe cyclonic storm before crossing the coast. The IMD forecasts sustained winds of 115 to 125 kmph, with gusts reaching 140 kmph. These figures describe a powerful system capable of causing dangerous conditions near the shoreline and inland areas along its track.

The forecast has already prompted action. Chief Minister N. Chandrababu Naidu reviewed preparedness and directed officials to stop fishermen from entering the sea. Authorities were also told to alert low-lying residents and establish toll-free emergency numbers. People in the projected zone should follow official updates because the track and intensity can change.

03

Which areas and groups are most at risk, and why are fishermen and people in low-lying areas being warned or evacuated?

Fishermen are at risk because a strengthening cyclone makes the sea hazardous, with powerful winds and rough conditions that can endanger boats and crews. Low-lying communities face a different threat: heavy rain and coastal water can collect quickly, flooding homes, roads and access routes. Evacuation reduces exposure before conditions become too dangerous for movement.

The article says the system may cross between Bapatla and Visakhapatnam on October 28 as a very severe cyclonic storm. Winds are forecast at 115 to 125 kmph, with gusts up to 140 kmph. Andhra Pradesh officials were directed to prevent fishermen from venturing into the sea and alert people in low-lying areas.

People living outside the immediate coast can also be affected if rain bands spread inland or roads become blocked. Officials planned evacuations from low-lying areas between Bapatla and Vizianagaram. Early warnings, transport and toll-free assistance can help people move before flooding, wind damage or isolation worsens.

04

What damage can a cyclone with winds of 115 to 125 kmph, gusting to 140 kmph, and very heavy rain cause?

A cyclone with winds of 115 to 125 kmph and gusts to 140 kmph can damage weak buildings, roofs, signs, trees, power lines and communication systems. Very heavy rain can flood homes and roads, overwhelm drainage and isolate communities. Coastal areas may face especially dangerous water conditions during landfall.

The article records the kinds of disruption already caused by heavy rain in the Nilgiris. Officials reported 62 minor landslips, damage to 15 huts and one hut collapsing completely. Two high-tension poles, nine low-tension poles and a distribution transformer were also damaged, while 28 trees were uprooted.

A cyclone could combine similar rain-related damage with stronger winds and coastal hazards. The article does not give a specific damage forecast for the expected landfall. However, authorities are preparing by reviewing evacuations, warning fishermen, clearing waterlogged areas and opening emergency contact channels. Residents should rely on official instructions and avoid damaged roads or exposed structures.

05

How do the IMD, State governments, local administrations, and emergency helplines work together to reduce casualties during a cyclone?

The IMD monitors the weather system, forecasts its movement and strength, and issues alerts that guide decisions. State governments use that information to coordinate preparedness. In Andhra Pradesh, Chief Minister N. Chandrababu Naidu reviewed preparations and ordered warnings for fishermen and low-lying communities.

Local administrations carry out practical work on the ground. They can restrict access to dangerous areas, arrange evacuations, operate pumping stations and respond to blocked roads or fallen trees. The Greater Chennai Corporation directed teams to speed up drainage and relief work, while its 1913 line was available for tree falls and other rain emergencies.

Emergency numbers give residents a direct route to help and information. The Andhra Pradesh government was told to set up toll-free assistance numbers. Together, forecasts, public warnings, local action and accessible reporting reduce delays. Their success depends on people receiving alerts, following evacuation instructions and reporting hazards quickly.

06

How do red, orange, and yellow rain alerts differ, and what actions should people take under each alert level?

The IMD’s red alert means extremely heavy rain exceeding 20 centimetres in 24 hours. Orange means very heavy rain between 11 and 20 centimetres. Yellow means heavy rain between 6 and 11 centimetres. These alerts describe expected rainfall, not the cyclone’s wind category.

Under a red alert, people should remain in safer places, avoid unnecessary travel, watch official updates and follow any evacuation order. Under orange, households should prepare for flooding, avoid waterlogged roads and keep emergency contacts ready. Under yellow, people should stay alert, check updates and take care near trees, slopes and drainage channels.

The article reports red alerts for Malappuram, Kozhikode and Wayanad, orange alerts for 10 Kerala districts, and a yellow alert for Kasaragod. The best response depends on local instructions and actual conditions. Rain can cause flooding, landslips and transport disruption even before the highest alert level is issued.

07

How does a low-pressure system over the warm Bay of Bengal develop into a cyclone?

A low-pressure system is an area where air pressure is lower than nearby regions. Over warm ocean water, heat adds energy to moist air. That air rises, cools and forms clouds and thunderstorms. As more air rises, pressure can fall further, drawing in additional moist air and strengthening the system.

Earth’s rotation helps the inflowing air curve around the low-pressure centre. When thunderstorms become better organized and winds strengthen, the system can develop into a tropical cyclone. Continued warm water, moisture and favourable upper-air conditions can allow further intensification. Strong wind differences or cooler water can weaken development.

The article says the Bay of Bengal system is expected to intensify into a very severe cyclonic storm and move toward the Andhra coast. It does not describe the system’s physical development in detail. Forecasts therefore remain important, because the IMD tracks changes in pressure, organization, movement and wind strength before landfall.

This brief was written by AI from the original reporting and checked by other models. Names, figures and quotes come from the source; read it for full context.

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