Cyclone Murasu LIVE updates: Eye of cyclone crosses Andhra Pradesh coast

The cyclone’s eye crossed the Andhra Pradesh coast, marking the storm’s passage over land. This mattered because the coastal region then faced intense weather impacts, including very heavy rain, flooding risks, crop damage, and transport disruption. Bapatla was identified as a particularly affected area.

The Hindu reported that very heavy rainfall continued to pound Bapatla. Authorities also issued flash-flood alerts, showing that rainfall was creating dangerous conditions beyond the immediate coastal crossing. NDTV reported damage to crops and interruptions to transport after the cyclone crossed the coast.

The available reports do not give a precise landfall time or a complete damage assessment. They show, however, that the storm’s effects extended from rainfall and flood danger to agriculture and mobility. Conditions in affected areas required continued monitoring as rain and flooding persisted.

The eye is the central region of a tropical cyclone. It is often calmer than the surrounding eyewall, where the strongest winds and heaviest rain occur. When the eye crosses a coast, the cyclone’s central circulation has moved over land. This is an important marker because dangerous conditions usually surround the eye before and after its passage.

For Cyclone Murasu, reports said the eye crossed the Andhra Pradesh coast while very heavy rain continued in Bapatla. Flash-flood alerts were issued, and reports also described crop damage and transport disruption. These effects show why the eye crossing is not the end of the danger.

After the eye passes, winds can change direction sharply as the storm’s opposite side arrives. Rain and flooding may also continue. The reports provide no measurements of Murasu’s eye or wind speed, but they clearly connect its coastal crossing with serious impacts in Andhra Pradesh.

The reports describe very heavy rainfall in Bapatla and nearby areas, but they do not provide a measured total in millimetres. They also report flash-flood alerts, indicating that rainfall was intense enough to create a rapid flooding risk. The available source therefore supports a description of severe rain and flood danger, not a precise rainfall figure.

The Hindu reported that very heavy rainfall continued to pound Bapatla. The same headline noted flash-flood alerts. This combination matters because sustained, intense rain can overwhelm drainage and cause water levels to rise quickly, especially during a coastal cyclone.

The current information gives no confirmed flooded-area size, water depth, casualty figure, or rainfall record. It does show that Bapatla remained under serious weather pressure after Murasu’s eye crossed Andhra Pradesh. Further official measurements would be needed to quantify the rainfall and flooding accurately.

Cyclone Murasu caused reported damage to crops and hit transport after crossing the Andhra Pradesh coast. These impacts matter because they affect both livelihoods and movement. Farmers can lose standing crops, while disrupted roads, rail services, or other transport links can slow evacuations and the delivery of essential supplies.

NDTV’s report specifically identified damaged crops and transport disruption. The supplied text does not explain which crops were affected, how much farmland was damaged, or whether roads, bridges, railways, ports, or power systems suffered losses. It also gives no confirmed account of homes being damaged.

The reports therefore establish agricultural and transport consequences, but not a complete infrastructure assessment. Continued rainfall and flash-flood alerts could complicate inspections and repairs. A fuller picture would require later surveys and official damage figures, which are not included in the supplied article information.

Odisha took large-scale precautions because Cyclone Murasu posed a threat to the state. It evacuated more than 1.65 lakh people and deployed 63 disaster response teams. These steps matter because moving residents from exposed areas can reduce danger, while response teams can support rescue, relief, and emergency operations.

The New Indian Express reported both figures in its coverage of Odisha’s preparations. The supplied information does not identify the exact districts evacuated or describe each team’s assignment. It does establish that the state treated the cyclone threat as serious enough to require mass movement and a substantial emergency deployment.

Evacuation and readiness are especially important when a cyclone can bring heavy rain, flooding, strong winds, and transport disruption. The source does not state the final number of casualties, rescues, or shelters used in Odisha. Those outcomes would depend on the storm’s path and the conditions that followed.

One cyclone can produce different weather across a wide region because its winds and rain are not spread evenly. The heaviest rain is usually concentrated near the storm’s core and rainbands. Areas farther from that core may receive weaker outer bands, even when they remain within the cyclone’s broader weather system.

Murasu’s eye crossed the Andhra Pradesh coast, and Bapatla experienced very heavy rainfall with flash-flood alerts. By contrast, the Telegraph India report said Kolkata and south Bengal were likely to receive light to moderate rain. Their differing conditions fit the storm’s uneven structure and the distance between the regions, although the supplied reports do not give the exact track or rainfall distribution.

This means a cyclone warning cannot be understood as one uniform forecast for every place. Local rainfall depends on the storm’s path, size, intensity, and interaction with land. Kolkata and south Bengal could still see rain, but the available report expected less intense conditions than Bapatla.

Tropical cyclones generally form over warm ocean water when moist air rises and lowers air pressure near the surface. Surrounding air moves inward and begins rotating because of Earth’s rotation. As water vapour condenses into clouds, it releases heat, which can make the rising air stronger and deepen the storm. A well-organised circulation can then intensify.

The ocean acts as the cyclone’s fuel source. Warm water adds moisture to the air, while condensation releases energy inside the storm. If winds higher in the atmosphere do not disrupt the circulation, the cyclone can strengthen. The supplied reports do not explain Murasu’s formation or intensification, so these are established scientific principles rather than details stated in the article.

After landfall, a cyclone usually weakens because it is cut off from warm ocean water and moves over rougher land. Friction slows its circulation, while mountains or dry air can disrupt its structure. It may still produce dangerous rain and flooding while weakening, as Murasu’s impacts in Andhra Pradesh demonstrate.