Cyclone Murasu begins making landfall on India’s eastern coast

A cyclone making landfall is moving from the sea onto land, with the storm’s center crossing the coastline. This marks a major change because communities, roads, homes, and infrastructure are now directly exposed to the storm’s strongest conditions.

Cyclone Murasu began making landfall at 1:00 a.m. local time on Tuesday. The India Meteorological Department placed the landfall over the coast of Andhra Pradesh, a southeastern Indian state. The storm had formed over the Bay of Bengal before reaching shore.

Landfall does not mean the danger ends immediately. Strong winds and heavy rain can continue inland, while coastal areas may face flooding and dangerous seas. Because Murasu followed Cyclone Arnab, which killed at least six people, authorities evacuated thousands and planned to move about 30,000 people to safety.

Andhra Pradesh is a state on India’s southeastern, or eastern, coast. Its position beside the Bay of Bengal places it close to the route taken by storms forming over that ocean. That geography makes the state especially important when a cyclone approaches from the east.

Cyclone Murasu began making landfall over Andhra Pradesh at 1:00 a.m. local time on Tuesday. The India Meteorological Department identified Andhra Pradesh as one of the states expected to be worst hit. Authorities began evacuating thousands of residents there and planned to move about 30,000 people to safety.

The state’s location matters because coastal communities can face the storm before it weakens over land. Tamil Nadu, immediately to Andhra Pradesh’s south, was also forecast to be badly affected. The storm’s path therefore shaped both evacuation planning and wider warnings across the region.

Authorities planned to evacuate around 30,000 people in Andhra Pradesh. This is a large emergency response because it requires moving many residents before dangerous weather reaches a populated coastal state. The operation also began while another cyclone had struck the region only days earlier.

Officials started evacuating thousands of people on Monday, before Murasu began making landfall early Tuesday. The India Meteorological Department forecast that Andhra Pradesh would be among the worst-hit states. Tamil Nadu, to the south, was also expected to face severe effects.

The figure shows the scale of preparation, not the number of people harmed. Evacuation moves residents away from the storm’s expected path and toward safety. It also reduces pressure on emergency services during the storm. The need for such a response was especially serious because Cyclone Arnab killed at least six people the previous week.

Severe cyclonic storms threaten coastal communities with powerful winds, flooding, dangerous seas, and damage to homes or infrastructure. These hazards can injure or kill people and disrupt roads, communications, and emergency services. The article gives a clear warning: Cyclone Arnab killed at least six people the previous week.

Evacuation reduces risk by taking residents out of areas expected to face the worst conditions. In Andhra Pradesh, authorities began moving thousands of people on Monday, before Murasu started making landfall. They planned to move about 30,000 people to safety. This creates distance between people and the storm’s strongest hazards.

Evacuation cannot stop the cyclone or prevent all damage. It can, however, reduce the number of people exposed during the most dangerous period. The response mattered even more because Murasu was the second cyclone to hit the region in one week, after Arnab’s deadly landfall.

The India Meteorological Department, or IMD, provides official weather information during cyclones. It identifies storm strength, tracks movement, estimates landfall, and forecasts which areas may face the greatest danger. Those details help authorities make timely decisions that protect residents.

For Murasu, IMD reported that the severe cyclonic storm began making landfall at 1:00 a.m. over Andhra Pradesh. Its forecasts said Andhra Pradesh and Tamil Nadu would be worst hit. Authorities then evacuated thousands of people and planned to move about 30,000 residents in Andhra Pradesh to safety.

Forecasts guide action by connecting the storm’s expected path with specific communities. Officials can issue warnings, arrange transport, and prepare safe locations before conditions become dangerous. Forecasts are not the evacuation itself, but they provide the information needed to target the response. The recent death toll from Cyclone Arnab made those warnings especially urgent.

The Bay of Bengal can produce multiple tropical cyclones because it is a broad tropical ocean basin where storms develop. Warm ocean water supplies energy to developing systems, while suitable atmospheric conditions can help them organize and strengthen. The basin’s position also places India’s eastern coast in the path of many storms.

The article describes the Bay of Bengal as a major region for tropical cyclones that has spawned deadly storms on India’s east coast. Murasu formed there and began making landfall over Andhra Pradesh. It was the second storm to hit the region in a week, following Cyclone Arnab.

That short interval leaves communities and authorities with little recovery time. Arnab killed at least six people, while Murasu prompted evacuations of thousands and plans to move about 30,000 residents. The repeated threat shows why forecasting, warnings, and preparedness remain important along the eastern coast.

Tropical cyclones generally begin over warm tropical ocean water. Heat causes seawater to evaporate, adding moist air above the surface. When that air rises and cools, water vapor condenses and releases heat. This added energy makes more air rise and can lower pressure near the ocean surface.

Lower pressure draws in surrounding air, while Earth’s rotation helps the winds curve around the system. If the ocean stays warm and upper-level winds do not tear the storm apart, the circulation can become more organized and intensify. The developing system may eventually be classified as a tropical cyclone.

Murasu formed over the Bay of Bengal, which the article identifies as a major tropical-cyclone region. Its exact intensification process is not detailed in the article, so this explanation uses established meteorological knowledge. Once a cyclone reaches land, it usually loses its main ocean energy source, though dangerous conditions can continue inland.