the western subtropical ridge of high pressure, before it made landfall on southern Odisha during November 3. The system subsequently dissipated over land during November 4. The system caused heavy rainfall over Southern Odisha, which led to flash flooding, dams and reservoirs overflowing and over worth damage to property and crops. 250 deaths were also recorded in conjunction with this system. Severe Cyclonic Storm BOB 09/04B On December 14, the IMD reported that a depression had developed within the Intertropical Convergence Zone over the southern Bay of Bengal. Over the next day the system moved north-westwards and gradually developed into a cyclonic storm, as the JTWC initiated advisories on the depression and assigned it the designation Tropical Cyclone 04B. The system subsequently continued to intensify, as it recurved and moved through a break in the subtropical ridge of high pressure. Late on December 16, the JTWC reported that the cyclone had peaked as a tropical storm, with 1-minute wind speeds of . Early on December 17, the IMD reported that the system had peaked as a Severe Cyclonic Storm with 3-minute wind speeds of . The system subsequently started to weaken later that day, as it encountered increasing upper-level wind shear associated with the mid-latitude westerlies. During the next day the system weakened into a Cyclonic Storm, before it degenerated into a depression. The system subsequently made landfall on Bangladesh near Cox's Bazar, before it was last noted over Myanmar by the JTWC during December 19. The system caused some deaths and damages in both Bangladesh and Myanmar. Other systems On April 17, an area of atmospheric convection developed within the Bay of Bengal to the east of Sri Lanka. During that day the system started to rapidly organise itself as it moved northwards, which prompted the JTWC to issue a Tropical Cyclone Formation Alert on the system. The JTWC subsequently initiated advisories on the system and assigned it the designation Tropical Cyclone 01B. Strong upper-level westerlies inhibited development of the depression and brought about the rapid dissipation of the system while it was located over water during April 18. A land depression was monitored over Bangladesh by the IMD during May 15. During the onset phase of the south-west monsoon on June 13, the IMD reported that a depression had developed had formed over the north-western Bay of Bengal. Over the next day the system moved north-westwards and made