 Early on October 14, a low pressure area formed off the eastern coast of India. While moving generally westward, the system quickly organized into a depression that day. On October 15, the IMD estimated peak winds of 65 km / h (40 mph), based on satellite imagery appearance warranting a Dvorak rating of 2.5; this made it a cyclonic storm. However, the circulation remained removed from the deep convection. Early on November 16, the storm made landfall near Nellore, Andhra Pradesh. It quickly weakened over land, degenerating into a remnant low pressure area over Rayalaseema on October 17.
