Moving west-northwest, it further strengthened to a deep depression on the next day, with ships in the area reporting below gale-force winds and a cyclonic storm on May 16.

[3] Heavy rains and gusty winds were reported on the northern parts of Andhra Pradesh, causing widespread destruction and unprecedented floods.

This time, it tracked east-northeastwards before crossing land near Diu on June 6, where Veraval recorded its peak winds from the northwest of 35 km/h (25 mph), while its barometric pressure toppled at 998.9 hPa (29.50 inHg) on Mahuva.

Ship ATAF reported winds of 55 km/h (35 mph), a minimum pressure of 1001.8 hPa (29.58 inHg) and intermittent rains on that day.

On July 20 in the night, it made landfall on the country near Chittagong before rapidly weakening to a low-pressure area and merging with the seasonal trough over Assam.

Bhubaneshwar recorded the heaviest rainfall from the system on July 30 at 28 cm (280 mm), while its remnants produced light downpour at Narmadapuram and Pachmarhi on August 2.

Moving northwest, the system crossed the coast over Sundarbans before rapidly weakening back to a low-pressure area that day.

[3] An upper air cyclonic circulation formed over East Pakistan and the adjoining Bay of Bengal on August 12 in the morning.

Sandheads reported winds of 95 km/h (60 mph) that day, well equivalent to a severe cyclonic storm in the modern-day NIO scale, while its pressure bottomed at 990 hPa (29.23 inHg) at 17:30 IST.

Continuing its course, it crossed north Orissa near Balasore that night before weakening to a deep depression, about 100 kilometres to the south of Jamshedpur.

[3] The influence of the cyclone caused active monsoon conditions on Gangetic West Bengal, Bihar, eastern Madhya Pradesh, Orissa and east Rajasthan from August 13-17.

Later moving in a north-northeast movement after tracking west-northwestwards and northwards, it weakened further to an area of low-pressure on September 11 before merging into the seasonal trough on the evening of the next day.