The 1970 North Indian Ocean cyclone season was an extremely devastating North Indian cyclone season. It saw a total of seven cyclonic storms, of which three developed into severe cyclonic storms. The Bay of Bengal was more active than the Arabian Sea during 1970, with all of the three severe cyclonic storms in the season forming there. Unusually, none of the storms in the Arabian Sea made landfall this year. The most significant storm of the season was the Bhola cyclone, which formed in the Bay of Bengal and hit Bangladesh on November 12. The storm killed at least 500,000, making it the deadliest tropical cyclone in recorded history.The world's worst natural disasters Calamities of the 20th and 21st centuries CBC News. Retrieved 2010-10-29. The season was also the deadliest tropical cyclone season globally, with 500,805 fatalities, mostly due to the aforementioned Bhola cyclone.
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Season summary
Systems Severe Cyclonic Storm One
A low-pressure area that developed over the southern Andaman Sea late in April moved north into the Bay of Bengal, becoming the first depression of the year on May 2. The depression intensified under the influence of a high-level anticyclone and became a cyclonic storm the next day. The storm then turned to the northeast and strengthened into a severe cyclonic storm on May 4. Soon after this, it peaked with winds of and a well-defined eye formed. The storm made its landfall near Cox's Bazar in easternmost East Pakistan (now Bangladesh) early in the morning of May 7 and dissipated over western Burma that evening.
The cyclone brought widespread rain to the Andaman and Nicobar Islands, before it moved clear of them on May 3. Effects in East Pakistan are unknown, but Akyab in western Burma reported winds of as the cyclone approached land.
Depression Two
A depression formed in the northeast of the Bay of Bengal during the morning of May 23, near the East Pakistan coast. It moved towards the coast and made landfall to the south of Cox's Bazar that night, before dissipating over southern Assam on the next day. Any effects on land are unknown.
Cyclonic Storm Three
A low-pressure area developed off the Karnataka–Goa coastline in the Arabian Sea on May 27, and developed into a depression on the next day. The system developed further into a cyclonic storm on May 29 as it moved to the north. The storm reached its peak with ; soon after this, as it turned to the west, but soon degenerated into a deep depression over the northern Arabian Sea on May 31. The depression continued to move westward, weakening to a remnant low shortly afterward, as it made landfall on the Arabian Peninsula, on June 2. The remnant low dissipated over southern Saudi Arabia on the next day. The cyclone itself had minimal effects on land, but the monsoon advanced into western India in late May in association with the system. As the cyclone moved to the west away from the subcontinent, the incursion of moist air from the Arabian Sea persisted over northwestern India for the first three days of June. This brought moderate rainfall to regions of Gujarat, Rajasthan and western Madhya Pradesh.
Cyclonic Storm Four
A low-pressure area developed in the northern Bay of Bengal on June 6 and developed into a depression on the next day, as it drifted to the north, moving over the south of the Ganges Delta. The depression reversed its course overland, reemerging into the Bay of Bengal on June 8. Once over open water, the depression intensified into a cyclonic storm on the morning of June 9. The cyclone's motion shifted to the northwest and it made a second landfall near Balasore in northern Orissa that night. The cyclone quickly weakened to a deep depression overland and tracked to the west over central India, where it degenerated into a broad area of low pressure on June 11. Sustained winds of were recorded at Sandheads on June 9, while the cyclone was at its peak offshore. High levels of rain affected much of Orissa and West Bengal, with over falling over large areas of both states. As the storm dissipated overland, it brought severe rain to Vidarbha and southern Madhya Pradesh. The highest recorded rainfall was at Khandwa were fell on June 13 alone. The rains led to localised flooding in parts of Vidarbha and disrupted road transport in the region.
Deep Depression Five
A low-pressure area that had developed over the northern Bay of Bengal on June 28 organized into a depression early on June 29. The depression intensified as it moved to the northwest, becoming a deep depression shortly before it crossed the Orissa coast. After landfall, the storm continued to move to the northwest, weakening to a depression again on July 2, over northeast Madhya Pradesh. It degenerated into a remnant low over central Uttar Pradesh during the evening of July 3. The depression brought intense monsoon conditions to Orissa, Madhya Pradesh and Vidarbha during its life. Over of rain and winds of were recorded in Paradip as the depression made landfall on June 30. Inland, the heavy rains caused some rivers in Orissa to overflow and flooded rice paddies in Cuttack District. Further west, the Wainganga River overflowed its banks in places. Road transport in Madhya Pradesh was disrupted and there was damage to crops in the Raipur area. Raipur recorded the highest 24-hour rains associated with the depression, with falling there on July 2.
Deep Depression Six
A low-pressure area moved to the west, off the Burmese coast on July 5, and developed into a depression on the next day, in the north-central Bay of Bengal. The depression intensified as it moved to the northwest, becoming a deep depression on July 7. The system made landfall on the Orissa coast during the morning of July 8, and rapidly degenerated into a broad area of low pressure overland. The remnant low moved north over western Bihar and it persisted there until July 12, when it was absorbed by the monsoon trough. Winds of were recorded offshore at Sandheads when the system was at its peak. The depression brought isolated heavy rains to many places throughout East India, with rains in excess of falling each day from the depression's landfall until the absorption of the storm's remnant low.
Depression Seven
A low-pressure area that lay over Burma on August 15, moved to the west across the Bay of Bengal and developed into a depression on the evening of August 17, when it was southeast of Gopalpur-on-Sea. The depression moved to the northwest and made landfall near Gopalpur-on-Sea, and turned to the west overland. The depression had weakened into a remnant low by August 20, when it was over western Madhya Pradesh. The depression and associated weather brought widespread rain to much of south and central India, with heavy rain falling in some locations. The heavy rain in Maharashtra disrupted road transport in many areas, especially in the east of the state. The Godavari River inundated parts of Bhadrachalam and many villages in regions of Andhra Pradesh. The rains also damaged rice paddies and disrupted transport in Telangana. Rains associated with the depression reached as far west as Bombay with falling there on August 19.
Cyclonic Storm Eight
A low-pressure area that was centred over West Bengal on August 31 organized into a depression on September 2, when it was to the east of Midnapore. It intensified as it moved to the west, becoming a deep depression on the next day, about east of Ranchi. The system continued to move west across India, before weakening into a depression on September 7, near Ahmedabad, Gujarat. The depression then turned northward and entered southwest Rajasthan. On September 8, the system turned to the southwest and emerged into the Arabian Sea on the following evening. Over open water, it intensified again, becoming a cyclonic storm by the evening of September 10. The cyclone developed a short-lived eye on September 11, as it drifted slowly to the west, before degenerating into a broad area of low pressure as it neared the Oman coast, on September 14. This system brought widespread rains to a wide swathe of India during its existence. Some heavy rains in West Bengal flooded vast areas of many districts and resulted in some fatalities, whilst in parts of neighbouring Orissa the floodwaters damaged fields. of rain fell on Bardhaman over two days as the depression passed overhead. Several thousand people were made homeless in West Bengal. Both the Narmada and Tapti Rivers inundated parts of Madhya Pradesh and Gujarat. The floods in Gujarat took many lives and caused severe damage to crops and other properties. Between 300 and 400 people were washed away in two villages in Bharuch district. of rain fell on Surat on July 7 and a further on Kutch District as the cyclone moved out to sea.
Deep Depression Nine
A low-pressure area moved from Burma to the Bay of Bengal on September 8, where it developed into a depression. The depression strengthened as it moved to the northwest and became a deep depression on the next day, when it was southeast of Calcutta. The system crossed the West Bengal coast later and moved to the northwest across the Chota Nagpur Plateau. The depression stalled over Uttar Pradesh on September 12, and remained near Lucknow until September 14. The depression then turned to the east and weakened into a remnant low over northern Bihar, on September 18. The depression brought widespread rain to West Bengal, Orissa, Bihar, Uttar Pradesh, and Madhya Pradesh during its lifespan, with rains of as far west as Lucknow. The rains in Uttar Pradesh caused severe property damage and flooding, with some 150 people losing their lives in the state. The Ganges flooded in northern Bihar, inundating parts of Munger District, whilst the Gandaki River flooded parts of Motihari. The rains worsened floods in south Bengal, increasing the death toll from the floods there to 80 and affecting 8 million people, with considerable damage done to crops and housing. Jaleswar in Orissa was entirely flooded.
Depression Ten
A well-defined low-pressure area formed over the west central Bay of Bengal on September 20, and developed into a depression on the next morning about south-east of Visakhapatnam. The depression then moved overland, and after crossing Vidarbha, weakened into a remnant low over Gujarat on September 23. The depression brought widespread rain to northern South India as it passed over the country, and its remnants brought scattered rain to Gujarat over the following week. Over a period of four hours, heavy rain fell on Hyderabad and Secunderabad, destroying many houses in the two cities. About of rain fell on Bombay as the system dissipated. The heavy rains claimed about 75 lives.
Depression Eleven
A low-pressure area that developed in the Bay of Bengal passed over the southern Indian subcontinent and developed into a depression in the Arabian Sea, off the southern Maharashtra coast on October 11. The depression did not develop further as it drifted westward, and it degenerated into an area of low pressure on October 13, as it was approaching the Arabian Peninsula. The depression brought widespread rains to southern Maharashtra and Karnataka states, with of rain recorded in Karwar. Scattered heavy rain was also reported in the Laccadives.
Severe Cyclonic Storm Twelve
A depression formed on October 18 in the central Bay of Bengal, and moved to the north. It gradually intensified and turned to the northeast, becoming a cyclonic storm on October 20. The storm became the second severe cyclonic storm of the season on the following day, and turned onto a more northerly track towards the Ganges Delta. The storm peaked with winds of before it made landfall near the West Bengal–East Pakistan border, during the morning of October 23. The storm then crossed over East Pakistan, before dissipating over southern Assam on October 24.