they dissipated near Delhi. The depression brought heavy rainfall over Odisha and Bihar. Cyclonic Storm BOB 05 Later in September, another depression formed on September 26 in the northwestern Bay of Bengal. Moving northwestward, it quickly moved ashore near Balasore, Odisha, failing to intensify beyond winds of . A ridge turned the system to the northeast, and the depression dissipated on September 28 over West Bengal. The depression brought heavy rainfall to Odisha, Bihar, and West Bengal, peaking at in Malda district in West Bengal. Cyclonic Storm ARB 01 (02A) A low-pressure area accompanied by a well-defined circulation persisted over central India on October 11. By the following day, the system emerged into the Arabian Sea, whereupon its convection organized west of a sheared circulation. On October 12, the system organized into a depression, classified Tropical Cyclone 02A by the JTWC. Steered by a ridge, it moved to the west-northwest and gradually intensified. The IMD upgraded it to a cyclonic storm on October 14, estimating peak 3 minute winds of . The JTWC assessed slightly higher 1 minute winds of . Increased wind shear stripped away the convection, causing the storm to weaken. By October 17, the system deteriorated into a depression and began drifting to the southwest, having moved between two ridges. Later that day, the system degenerated into a remnant low, which the JTWC tracked for an additional day until dissipation east of the Somalia coastline. Very Severe Cyclonic Storm BOB 06 (03B) The storm originated from the monsoon trough on November 7 in the Bay of Bengal, east of India. Moving northwestward, the system gradually intensified while moving toward land, eventually developing an eye in the middle of the convection. Reaching peak 3 minute winds of , the IMD classified the system as a very severe cyclonic storm, in line with the wind estimate from the JTWC. On November 9, the cyclone made landfall near the border of Andhra Pradesh and Orissa. Atypical for most November storms, the system continued to the north and dissipated over Nepal on November 11. In India, the cyclone's strong winds were accompanied by heavy rainfall and a storm surge of that inundated the coastline several hundred feet inland. Power lines, crops, and houses were damaged, and many boats were damaged, causing several nautical fatalities. The cyclone killed 128 people and caused US$46.3 million in damage. In neighboring Bangladesh, high waves killed