[4] During the year a strong south-west monsoon was observed, which produced heavy rain and lead to flooding in India, Bangladesh and Myanmar.
[3] The system subsequently started to weaken and had become a very severe cyclonic storm, by the time it made landfall in southern Andhra Pradesh during May 9.
[2][9] The system continued to move towards the northwest along the western subtropical ridge of high pressure, before it made landfall on southern Odisha during November 3.
[9] The system caused heavy rainfall over Southern Odisha, which led to flash flooding, dams and reservoirs overflowing and over US$110 million worth damage to property and crops.
[9] The system subsequently started to weaken later that day, as it encountered increasing upper-level wind shear associated with the mid-latitude westerlies.
[2] 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.
[8] 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.
[13] The system subsequently intensified into a Deep Depression while located over land near Jamshedpur, before as it moved north-westwards it weakened and dissipated over Madhya Pradesh during June 15.
[13] Over the next day the system moved towards the northwest and made landfall on the coast of northern Andhra Pradesh and southern Odisha during August 15.
[13] Early on August 20, the IMD reported that a Depression had developed over the northern Bay of Bengal and was embedded within a deep easterly flow of an anticyclone.
[13] On September 1, the remnants of Typhoon Becky crossed the coast of Bangladesh, and moved into the Indian state of West Bengal as an area of low pressure.
[9] 370 deaths were recorded in Bangladesh in association with this system, while a storm surge affected Chittagong and caused extensive damage to two offshore islands.
[11][14] On November 14, the IMD reported that a depression had developed out of a pre existing disturbance, that was located over the south-west Bay of Bengal near the Tamil Nadu Coast.
[9] During that day the system moved westwards and made landfall on the Northern Tamil Nadu and Southern Andhra Pradesh coasts before it rapidly weakened into an area of low pressure.