On the evening of October 28, 2026, the Andhra Pradesh coastline was bathed in a sudden, ominous glow. Cyclone Arnab, a low‑pressure system that had been gathering strength over the Bay of Bengal, began its descent toward the Indian mainland. The first reports came from Visakhapatnam, where the sky had turned a deep, unsettling red and the sea roiled with waves that seemed to rise on their own accord. Residents were already bracing for the worst, as the storm’s eye was expected to make landfall within the next two to three hours.
The cyclone’s power was measured in a way that few storms in the region have matched. Wind speeds at the point of landfall reached a staggering 150 km/h, a figure that marked the upper limit of what the Indian Meteorological Department (IMD) had recorded for the event. Even as the storm moved inland, the IMD logged sustained winds between 125 km/h and 135 km/h, a range that is enough to uproot trees, topple power lines, and turn even the most sturdy structures into a flurry of debris. The sheer velocity of the wind was a stark reminder of the raw power that nature can unleash when atmospheric conditions align.
While the immediate focus was on Andhra Pradesh, the reach of Arnab’s fury stretched far beyond the state’s borders. Coastal areas in Odisha felt the sting of high winds and heavy rain, and the storm’s influence was also felt in Digha, West Bengal, and even as far inland as Jharkhand. The fact that a single cyclone could impact four states underscored how interconnected the eastern Indian coastline is when it comes to weather events.
In the days that followed, the IMD and local officials urged coastal residents to stay away from the sea.
In response, the IMD issued flood warnings for fifteen districts, a move that signaled the seriousness of the situation. The warnings were not merely advisory; they were a call to action for communities that had already been grappling with the storm’s immediate threats.
The human cost of Arnab’s passage was felt almost immediately. Authorities organized a mass evacuation that displaced 1,80,000 people—an unprecedented number for the region in recent memory. The scale of the operation required coordination across multiple agencies, and it was a testament to the preparedness of local governments that the evacuation proceeded with relative calm. Flights were suspended in the major hubs of Vijayawada and Visakhapatnam, further complicating travel plans for residents and tourists alike.
In the days that followed, the IMD and local officials urged coastal residents to stay away from the sea. The advisory was not a casual suggestion; it was a directive borne out of the knowledge that even a brief encounter with the storm’s eye could prove deadly. The public’s compliance with these warnings played a crucial role in preventing a larger loss of life. Meanwhile, emergency teams worked tirelessly to set up shelters, distribute supplies, and provide medical care to those who had been displaced.
As the storm’s most violent phase subsided, the focus shifted to the aftermath. The landfall process, which had been expected to last two to three hours, had concluded, but the damage remained. Flooded streets, downed power lines, and damaged infrastructure stretched across the fifteen districts that had received warnings. The government’s response involved clearing debris, restoring electricity, and rebuilding homes—tasks that would take weeks, if not months.
Today, the region is in a state of cautious recovery. Authorities continue to monitor weather patterns and are prepared to issue additional advisories if conditions worsen. For the people who were evacuated, the return to normalcy will be a gradual process, one that will test the resilience of both the communities and the infrastructure that supports them.