India news: Cyclone Arnab turns deadly after landfall

Cyclone Arnab made a prolonged landfall along the Andhra Pradesh coast before moving farther inland. Landfall brought strong winds and rainfall to several districts. The storm then weakened, but its effects remained deadly. At least three people were killed in Andhra Pradesh.

The storm caused visible damage across the state. Trees were uprooted, and 31 houses of different types were damaged, according to National Disaster Response Force Inspector General Narendra Singh Bundela. Northern Andhra Pradesh and southern Odisha experienced the strongest reported effects, while Odisha’s impact was initially described as less serious.

Nearly 40 NDRF teams were deployed along India’s east coast to manage the cyclone’s effects. Arnab was downgraded from a very severe cyclonic storm to a severe cyclonic storm after landfall. Officials expected it to weaken further into a cyclonic storm and then a deep depression by evening.

A cyclone’s landfall occurs when the storm’s center crosses from the ocean onto the coast. It marks a major change in the storm’s environment. The cyclone loses its direct access to warm ocean water, but landfall does not instantly end the danger. Strong winds, torrential rain, flooding, and falling trees can continue for hours.

Arnab shows why the transition matters. After a prolonged landfall along Andhra Pradesh, it moved inland and was downgraded from a very severe cyclonic storm to a severe cyclonic storm. Even while weakening, it uprooted trees, damaged 31 houses, and killed three people.

The storm was expected to weaken further into a cyclonic storm and then a deep depression. However, officials still deployed nearly 40 NDRF teams along the east coast. This response reflects a basic risk: a weaker inland storm can still threaten lives through wind, rain, flooding, and damaged buildings.

Cyclone Arnab’s reported impact included at least three deaths in Andhra Pradesh and damage to 31 houses of various types. Trees were also uprooted. Northern Andhra Pradesh and southern Odisha were identified as the most affected areas. Preliminary reports described the impact in Odisha as less serious than in Andhra Pradesh.

The storm’s prolonged landfall produced strong winds and rainfall across several districts. These conditions damaged homes and infrastructure and created risks for people in affected communities. The figures came from National Disaster Response Force Inspector General Narendra Singh Bundela, who briefed reporters in New Delhi.

Nearly 40 NDRF teams were deployed to regions along India’s east coast. Officials expected Arnab to weaken from a severe cyclonic storm into a cyclonic storm, then a deep depression. The reported death toll and damage figures were preliminary, so the full effects could change as assessments continued.

Cyclones generally lose strength after moving over land. Their main energy source is warm, moist ocean water, which supplies heat and water vapor. Land removes that fuel, while rough terrain creates friction that slows the rotating winds. Dry air and mountains can weaken a system further, although dangerous rain and winds may continue.

Arnab lost speed after making a prolonged landfall along Andhra Pradesh. That led officials to downgrade it from a very severe cyclonic storm to a severe cyclonic storm. The storm still produced strong winds and rainfall across districts in Andhra Pradesh and southern Odisha.

National Disaster Response Force Inspector General Narendra Singh Bundela said Arnab was expected to weaken further into a cyclonic storm and then a deep depression by evening. The downgrade therefore described falling wind strength, not an immediate end to danger. Three people had already been killed, and 31 houses had been damaged.

Strong winds can kill by collapsing weak buildings, breaking windows, uprooting trees, and turning loose objects into dangerous debris. Heavy rain can overwhelm drainage, flood homes and roads, and trigger landslides. Storm surge is a rise of seawater pushed toward shore by a cyclone’s winds and low pressure. It can rapidly inundate coastal areas.

Arnab’s reported effects included uprooted trees, 31 damaged houses, and at least three deaths in Andhra Pradesh. Strong winds and rainfall were observed in districts of Andhra Pradesh and southern Odisha. These details show how different hazards can strike together during a coastal storm.

The danger can continue after the center moves inland. Floodwater may remain, roads can become impassable, and damaged structures may collapse later. Arnab weakened after landfall, yet nearly 40 NDRF teams were deployed along the east coast. The response reflected the continuing risks from wind, rain, flooding, and debris.

Andhra Pradesh and southern Odisha face cyclone exposure because they lie along India’s eastern coastline beside the Bay of Bengal. Tropical systems forming over that basin can move toward the coast. Low-lying coastal settlements are especially vulnerable because strong winds, heavy rain, flooding, and storm surge can arrive together.

Arnab illustrates this exposure. Officials identified northern Andhra Pradesh and southern Odisha as the most affected areas. Strong winds and rainfall were reported in districts of both states. Andhra Pradesh suffered the clearest reported damage, including uprooted trees, 31 damaged houses, and three deaths.

The storm’s inland path did not remove the need for a major response. Nearly 40 NDRF teams were deployed along India’s east coast. The article does not explain the region’s geography in detail; the coastal exposure described here uses established meteorological knowledge. Arnab’s effects show why communities in this corridor need warnings, evacuation planning, and emergency teams.

A tropical cyclone begins over warm ocean water when moist air rises and creates lower pressure near the surface. Air then flows inward, while Earth’s rotation helps organize the system’s circulation. As moist air rises and condenses, it releases heat. That heat powers more rising air and can strengthen the circulation.

Intensification is most likely when the ocean is warm enough to provide abundant moisture, the atmosphere is unstable, and winds at different heights do not tear the storm apart. A well-organized center allows thunderstorms to cluster around it. Falling pressure and faster winds can then reinforce one another.

The article does not explain how Arnab formed. It reports that Arnab weakened after landfall, when it lost access to warm ocean water and encountered land friction. Established cyclone science explains that process. Officials expected the storm to decline from a severe cyclonic storm to a cyclonic storm and then a deep depression.