On April 22, 1991, a circulation formed in the southern Bay of Bengal from a persistent area of convection, or thunderstorms, near the equator in the eastern Indian Ocean. Within two days, the cloud mass encompassed most of the Bay of Bengal, focused on an area west of the Andaman and Nicobar Islands. On April 24, the India Meteorological Department (IMD) designated the system as a depression, and the Joint Typhoon Warning Center (JTWC) labeled the system as Tropical Cyclone 02B. Ships in the region reported winds of around 55 km/h (35 mph) around this time.