Meteorological history | |
---|---|
Formed | 8 November 1970 |
Dissipated | 13 November 1970 |
Extremely severe cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 185 km/h (115 mph) |
Lowest pressure | 960 hPa (mbar);28.35 inHg |
Category 4-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 240 km/h (150 mph) |
Overall effects | |
Fatalities | 300,000–500,000 (Deadliest tropical cyclone on record) |
Damage | $86.4 million (1970 USD) |
Areas affected | East Pakistan and India |
Part of the 1970 North Indian Ocean cyclone season |
The 1970 Bhola cyclone (also known as the Great Cyclone of 1970 [1] ) was a devastating tropical cyclone that struck East Pakistan (present-day Bangladesh) and India's West Bengal on 12 November 1970. [2] It remains the deadliest tropical cyclone ever recorded and one of the world's deadliest humanitarian disasters. At least 300,000 people died in the storm, [3] possibly as many as 500,000, [4] [5] [6] primarily as a result of the storm surge that flooded much of the low-lying islands of the Ganges Delta. [7] Bhola was the sixth and strongest cyclonic storm of the 1970 North Indian Ocean cyclone season. [8]
The cyclone formed over the central Bay of Bengal on 8 November and traveled northward,intensifying as it did so. It reached its peak with winds of 185 km/h (115 mph) on 10 November,and made landfall on the coast of East Pakistan on the following afternoon. The storm surge devastated many of the offshore islands,wiping out villages and destroying crops throughout the region. In the most severely affected upazila Tazumuddin,over 45% of the population of 167,000 were killed by the storm.
The Pakistani government,led by junta leader General Yahya Khan,was criticized for its delayed handling of relief operations following the storm,both by local political leaders in East Pakistan and by the international media. The poor and discriminating response from the West Pakistan government led to the increasingly widespread disillusionment from the East Pakistani people,allowing the opposition Awami League to gain a landslide victory in the province during the election that took place a month later as well as the Bangladesh Liberation War 7 months later.
On 1 November, Tropical Storm Nora developed over the South China Sea, in the West Pacific Ocean. The system lasted for four days, before degenerating into a remnant low over the Gulf of Thailand on 4 November, and subsequently moved west over the Malay Peninsula the next day. [9] [10] The remnants of this system contributed to the development of a new depression in the central Bay of Bengal on the morning of 8 November. The depression intensified as it moved slowly northward, and the India Meteorological Department upgraded it to a cyclonic storm the next day. No country in the region had ever named tropical cyclones during this time, so no new identity was given. [11] The storm became nearly stationary that evening near 14.5° N, 87° E, but began to accelerate toward the north on 10 November. [11]
The storm further intensified into a severe cyclonic storm on 11 November and began to turn towards the northeast, as it approached the head of the bay. It developed a clear eye and reached its peak intensity later that day, with three-minute sustained winds of 185 km/h (115 mph), one-minute sustained winds of 240 km/h (150 mph), [12] and a central pressure of 960 hPa. The cyclone made landfall on the East Pakistan coastline during the evening of 12 November, around the same time as the local high tide. Once over land, the system began to weaken; the storm degraded to a cyclonic storm on 13 November, when it was about 100 km (62 mi) south-southeast of Agartala. The storm then rapidly weakened into a remnant low over southern Assam that evening. [11]
There is question as to how much of the information about the cyclone said to have been received by Indian weather authorities was transmitted to East Pakistan authorities. This is because the Indian and East Pakistani weather services may not have shared information given the Indo-Pakistani friction at the time. [13] A large part of the population was reportedly taken by surprise by the storm. [14] There were indications that East Pakistan's storm warning system was not used properly. [15] The Pakistan Meteorological Department issued a report calling for "danger preparedness" in the vulnerable coastal regions during the day on 12 November. As the storm neared the coast, a "great danger signal" was broadcast on Radio Pakistan. Survivors later said that this meant little to them, but that they had recognised a No. 1 warning signal as representing the greatest possible threat. [16]
Following two previously destructive cyclones in October 1960 which killed at least 16,000 people in East Pakistan, [17] the Pakistani central government contacted the American government for assistance in developing a system to avert future disasters. Gordon Dunn, the director of the National Hurricane Center at the time, carried out a detailed study and submitted his report in 1961. However, the central government did not carry out all of the recommendations Dunn had listed. [13]
Although the North Indian Ocean is the least active of the tropical cyclone basins, the coast of the Bay of Bengal is particularly vulnerable to the effects of tropical cyclones. The exact death toll from the Bhola cyclone will never be known, but at least 300,000 fatalities were associated with the storm, [3] [10] possibly as many as 500,000. [4] The cyclone was not, however, the most powerful of these; the 1991 Bangladesh cyclone was significantly stronger when it made landfall in the same general area, as a Category 5-equivalent cyclone with 260 km/h (160 mph) winds.
The Bhola cyclone is the deadliest tropical cyclone on record and also one of the deadliest natural disasters in modern history. A comparable number of people died as a result of the 1976 Tangshan earthquake, 2004 Indian Ocean earthquake and the 2010 Haiti earthquake, but because of uncertainty in the number of deaths in all four disasters, it may never be known which one was the deadliest. [18]
Rank | Name/Year | Region | Fatalities |
---|---|---|---|
1 | Bhola 1970 | Bangladesh | 300,000 |
2 | Bangladesh 1991 | Bangladesh | 138,866 |
3 | Nargis 2008 | Myanmar | 138,373 |
4 | Unnamed 1911 | Bangladesh | 120,000 |
5 | Unnamed 1917 | Bangladesh | 70,000 |
6 | Harriet 1962 | Thailand, Bangladesh | 50,935 |
7 | Unnamed 1919 | Bangladesh | 40,000 |
8 | Nina 1975 | China | 26,000 |
9 | Unnamed 1958 | Bangladesh | 12,000 |
Unnamed 1965 | Bangladesh |
The meteorological station in Chittagong, 95 km (59 mi) to the east of where the storm made landfall, recorded winds of 144 km/h (89 mph) before its anemometer was blown off at about 2200 UTC on 12 November. A ship anchored in the port in the same area recorded a peak gust of 222 km/h (138 mph) about 45 minutes later. [10] As the storm made landfall, it caused a 10-metre (33 ft) high storm surge at the Ganges Delta. [23] In the port at Chittagong, the storm tide peaked at about 4 m (13 ft) above the average sea level, 1.2 m (3.9 ft) of which was the storm surge. [10]
Radio Pakistan reported that there were no survivors on the thirteen islands near Chittagong. A flight over the area showed the devastation was complete throughout the southern half of Bhola Island, and the rice crops of Bhola Island, Hatia Island and the nearby mainland coastline were destroyed. [24] Several seagoing vessels in the ports of Chittagong and Mongla were reported damaged, and the airports at Chittagong and Cox's Bazar were under 1 m (3.3 ft) of water for several hours. [25]
Over 3.6 million people were directly affected by the cyclone, and the total damage from the storm was estimated at US$86.4 million (US$701 million in 2024). [26] The survivors claimed that approximately 85% of homes in the area were destroyed or severely damaged, with the greatest destruction occurring along the coast. [27] : 9 Ninety percent of marine fishermen in the region suffered heavy losses, including the destruction of 9,000 offshore fishing boats. Of the 77,000 onshore fishermen, 46,000 were killed by the cyclone, and 40% of the survivors were affected severely. In total, approximately 65% of the fishing capacity of the coastal region was destroyed by the storm, in a region where about 80% of the protein consumed comes from fish. Agricultural damage was similarly severe with the loss of US$63 million worth of crops and 280,000 cattle. [10] Three months after the storm, 75% of the population was receiving food from relief workers, and over 150,000 relied upon aid for half of their food. [27] : 11
The Bhola Cyclone would also lead to increased cholera and typhoid cases in the region due to the contamination of the water supply in the storm. Many attempts of sending aid to the region were impeded by the prevalent cholera, and as a result, medical aid was delayed. [28]
The cyclone brought widespread rain to the Andaman and Nicobar Islands, with very heavy rain falling in places on 8–9 November. Port Blair recorded 130 mm (5.1 in) of rain on 8 November, and there were a number of floods on the islands. MV Mahajagmitra, a 5,500-ton freighter en route from Calcutta to Kuwait, was sunk by the storm on 12 November with the loss of all fifty people on board. The ship sent out a distress signal and reported experiencing hurricane-force winds before it sank. [11] [29] There was also widespread rain in West Bengal and southern Assam. The rain caused damage to housing and crops in both Indian states, with the worst damage occurring in the southernmost districts. [11]
Two medical relief surveys were carried out by the Pakistan-SEATO Cholera Research Laboratory: the first in November and the second in February and March. The purpose of the first survey was to establish the immediate medical needs in the affected regions, and the second, more detailed, survey was designed as the basis for long-term relief and recovery planning. In the second survey, approximately 1.4% of the area's population was studied. [27] : 6
The first survey concluded that the surface water in most of the affected regions had a comparable salt content to that drawn from wells, except in Sudharam, where the water was almost undrinkable with a salt content of up to 0.5%. The mortality was estimated at 14.2%—equivalent to a death toll of 240,000. [27] : 5 Cyclone-related morbidity was generally restricted to minor injuries, but a phenomenon dubbed "cyclone syndrome" was observed. This consisted of severe abrasions on the limbs and chest caused by survivors clinging to trees to withstand the storm surge. [27] : 5 Initially, there were fears of an outbreak of cholera and typhoid fever in the weeks following the storm, [30] but the survey found no evidence of an epidemic of cholera, smallpox, or any other disease in the region affected by the storm. [27] : 5
The totals from the second survey were likely a considerable underestimate as several groups were not included— 100,000 migrant workers who were collecting the rice harvest, families who were completely wiped out by the storm, and those who had migrated out of the region in the intervening three months. Excluding these groups reduced the risk of hearsay and exaggeration. [27] : 6 The survey concluded that the overall death toll was, at minimum, 224,000. The worst effects were felt in Tazumuddin, where the mortality was 46.3%, corresponding to approximately 77,000 deaths in the thana alone. The mean mortality throughout the affected region was 16.5%. [27] : 7
The results showed that the highest survival rate was for adult males aged 15–49, while more than half the deaths were children under age 10, who only formed a third of the pre-cyclone population. This suggests that the young, old, and sick were at the highest risk of perishing in the cyclone and its storm surge. In the months after the storm, the mortality of the middle-aged was lower in the cyclone area than in the control region, near Dhaka. This reflected the storm's toll on the less healthy individuals. [27] : 7-8
There have been mistakes, there have been delays, but by and large I'm very satisfied that everything is being done and will be done.
The day after the storm struck the coast, three Pakistani gunboats and a hospital ship carrying medical personnel and supplies left Chittagong for the islands of Hatia, Sandwip and Kutubdia. [25] Teams from the Pakistani Army reached many of the stricken areas in the two days following the landfall of the cyclone. [32] President Khan visited East Pakistan on the way back from a trip to China. In a press conference in Dhaka, Khan accepted the government had made "slips" and "mistakes" in their relief effort for the cyclone victims of then East Pakistan (now Bangladesh) but he insisted that "everything was done within the limits of the Government." He then returned to Rawalpindi. [31] No West Pakistani political leaders visited the East. [33]
In the ten days following the cyclone, one military transport aircraft and three crop-dusting aircraft were assigned to relief work by the Pakistani central government. [34] The central government said it was unable to transfer military helicopters from West Pakistan as the Indian government did not grant clearance to cross the intervening Indian territory, a charge the Indian government denied. [30] By 24 November, the central government had allocated a further US$116 million to finance relief operations in the disaster area. [35] Khan arrived in Dhaka to take charge of the relief operations on 24 November. The governor of East Pakistan, Vice Admiral S. M. Ahsan, denied charges that the armed forces had not acted quickly enough and said supplies were reaching all parts of the disaster area except for some small pockets. [36]
Khan said there was a lack of understanding of the magnitude of the disaster. He also said that the 1970 general election slated for 7 December would take place on time, although eight or nine of the worst affected districts might experience delays, denying rumours that the election would be postponed. [31]
As the conflict between East and West Pakistan developed in March 1971, the Dhaka offices of the two government organisations directly involved in relief efforts were closed for at least two weeks, first by a general strike and then by a ban on government work in East Pakistan by the Awami League. Relief work continued in the field, but the long-term planning was curtailed. [37]
We have a large army, but it is left to the British Marines to bury our dead.
Political leaders in East Pakistan were deeply critical of the central government's initial response to the disaster. A statement released by eleven East Pakistan politicians ten days after the storm charged the government with "gross neglect, callous indifference and utter indifference". They also accused President Khan of playing down the news coverage. [35] On November 19, students held a march in Dhaka in protest of the speed of the government response, [39] and Maulana Abdul Hamid Khan Bhashani addressed a rally of 50,000 people on 24 November, when he accused the president of inefficiency and demanded his resignation. Khan's political opponents in West Pakistan accused him of bungling the efforts and some demanded his resignation. [36] Awami League leader Bangabandhu Sheikh Mujibur Rahman described the destruction caused by the cyclone akin to a "Holocaust" and condemned the military junta's response as "criminal negligence". [40]
The Pakistan Red Crescent began to operate independently of the central government as the result of a dispute that arose after the Red Crescent took possession of twenty rafts donated by the British Red Cross. [41] A pesticide company had to wait two days before it received permission for two of its crop dusters, which were already in the country, to carry out supply drops in the affected regions. The central government only deployed a single helicopter to relief operations, with Khan later stating that there was no point deploying any helicopters from West Pakistan as they were unable to carry supplies. [16]
A reporter for the Pakistan Observer spent a week in the worst hit areas in early January 1971 and saw none of the tents supplied by relief agencies being used to house survivors and commented that the grants for building new houses were insufficient. The Observer regularly carried front-page stories with headlines like, "No Relief Coordination", while publishing government statements saying, "Relief operations are going smoothly." In January, the coldest period of the year in East Pakistan, the National Relief and Rehabilitation Committee, headed by the editor of Ittefaq , said thousands of survivors from the storm were "passing their days under [the] open sky". A spokesman said families who were made homeless by the cyclone were receiving up to 250 rupees (US$55 in 1971; equivalent to $341in 2018) to rebuild, but that resources were scarce and he feared the survivors would "eat the cash". [42]
Due to the poor handling and the destructive aftermath of the Bhola Cyclone, leftist parties in both East and West Pakistan boycotted the 1970 Pakistani general election. [43] This allowed the Awami League, headed by Sheikh Mujibur Rahman, to win in a landslide victory. The elections for nine national assembly and eighteen provincial assembly seats had to be postponed until January 18 as a result of the storm. [44]
The central government's handling of the relief efforts helped exacerbate the bitterness felt in East Pakistan, swelling the resistance movement there. Funds only slowly got through, and transport was slow in bringing supplies to the devastated regions. As tensions increased in March 1971, foreign personnel evacuated because of fears of violence. [37] The situation deteriorated further and evolved into the subsequent genocide. [45]
India became one of the first nations to offer aid to Pakistan, despite the generally poor relations between the two countries, and by the end of November had pledged US$1.3 million (US$8.7 million in 2020 dollars) of assistance for the relief efforts. [46] The Pakistani central government refused to allow the Indians to send supplies into East Pakistan by air, forcing them to be transported slowly by road instead. [47] The Indian government also said that the Pakistanis refused an offer of military aircraft, helicopters and boats from West Bengal to assist in the relief operation. [48]
U.S. President Richard Nixon allocated a $10 million ($78 million in 2023) grant to provide food and other essential relief to the survivors of the storm, and the U.S. ambassador to Pakistan pledged that he would "assist the East Pakistan government in every way feasible." [49] The U.S. sent a number of blankets, tents and other supplies to East Pakistan. Six helicopters – two helicopters at an aid mission in Nepal and four from the U.S. – were also sent. [50] Some 200,000 tons of wheat were shipped from the U.S. to the stricken region. [42] By the end of November, there were 38 helicopters operating in the disaster area, ten of which were British and ten American. The Americans had provided about fifty small boats and the British seventy for supply distribution. [46]
CARE halted aid shipments to East Pakistan the week after the cyclone hit because of unwillingness to let the Pakistani central government handle distribution. [41] However, by January 1971, they had reached an agreement to construct 24,000 cement brick houses at a cost of about $1.2 million ($9 million in 2023). [42] American concerns about delays by the central government in determining how the relief should be used meant that US$7.5 million ($59 million in 2023) of relief granted by the United States Congress had not been handed over in March. Much of the money was earmarked to be spent on constructing cyclone shelters and rebuilding housing. [37] The American Peace Corps offered to send volunteers but were rebuffed by the central government. [46]
A Royal Navy task force, centred on HMS Intrepid and HMS Triumph, left Singapore for the Bay of Bengal to assist with the relief efforts. They carried eight helicopters and eight landing craft, as well as rescue teams and supplies. [49] Fifty soldiers and two helicopters were flown in ahead of the ships to survey the disaster area and bring relief work. [51] The task force arrived off the East Pakistan coast on 24 November, and the 650 troops aboard the ships immediately began using landing craft to deliver supplies to offshore islands. [36] An appeal by the British Disasters Emergency Committee raised about £1.5 million (£29 million in 2023) for disaster relief in East Pakistan. [46] [52]
The Canadian government pledged C$2 million of assistance. France and West Germany both sent helicopters and various supplies worth US$1.3 million. [46] [51] Pope Paul VI announced that he would visit Dhaka during a visit to the Far East and urged people to pray for the victims of the disaster. [53] The Vatican later contributed US$100,000 to the relief efforts. [46] By the start of 1971, four Soviet helicopters were still operating in the region transporting essential supplies to hard-hit areas. The Soviet aircraft, which had drawn criticism from Bengalis, replaced the British and American helicopters that had operated immediately after the cyclone. [42]
The government of Singapore sent a military medical mission to East Pakistan which arrived at Chittagong on 1 December. They were then deployed to Sandwip where they treated nearly 27,000 people and carried out a smallpox vaccination effort. The mission returned to Singapore on 22 December, after bringing about $50,000 worth of medical supplies and fifteen tons of food for the victims of the storm. [54] The Japanese cabinet approved a total of US$1.65 million of relief funds in December. The Japanese government had previously drawn criticism for only donating a small amount to relief work. [55] The first shipment of Chinese supplies was a planeload of 500,000 doses of cholera vaccine, which was not necessary as the country had adequate stocks. [47] The Chinese government sent US$1.2 million in cash to Pakistan. [46] Mohammad Reza Pahlavi declared that the disaster was also an Iranian one and responded by sending two planeloads of supplies within a few days of the cyclone striking. [39] Many smaller, poorer Asian nations sent nominal amounts of aid. [46]
The United Nations donated US$2.1 million in food and cash, while UNICEF began a drive to raise a further million. [46] UNICEF helped to re-establish water supplies in the wake of the storm, repairing over 11,000 wells in the months following the storm. [56] UN Secretary-General U Thant made appeals for aid for the victims of the cyclone and the civil war in August, in two separate relief programs. He said only about $4 million had been contributed towards immediate needs, well short of the target of US$29.2 million. [57] By the end of November, the League of Red Cross Societies had collected US$3.5 million to supply aid to the victims of the disaster. [46]
The World Bank estimated that it would cost US$185 million to reconstruct the area devastated by the storm. The bank drew up a comprehensive recovery plan for the Pakistani government. The plan included restoring housing, water supplies and infrastructure to their pre-storm state. It was designed to combine with a much larger ongoing flood-control and development program. [58] The bank provided US$25 million of credit to help rebuild the East Pakistan economy and to construct protective shelters in the region. This was the first time that the IDA had provided credit for reconstruction. [59] By the start of December, nearly US$40 million had been raised for the relief efforts by the governments of 41 countries, organizations and private groups. [58]
In 1971, ex-Beatle George Harrison and musician Ravi Shankar were inspired to organize The Concert for Bangladesh, in part from the Bhola cyclone, and from the civil war and genocide. [60] Although it was the first benefit concert of its type, it was extremely successful in raising money, aid and awareness for the region's plight.
In December 1970, the League of Red Cross Societies drafted a plan for immediate use should a comparable event to the cyclone hit other "disaster prone countries". A Red Cross official stated some of the relief workers sent to East Pakistan were poorly trained, and the organisation would compile a list of specialists. The UN General Assembly adopted a proposal to improve its ability to provide aid to disaster-stricken countries.
In 1966, the Red Crescent had begun to support the development of a cyclone warning system, which developed into a Cyclone Preparedness Programme in 1972, today run by the government of Bangladesh and the Bangladesh Red Crescent Society. The programme's objectives are to raise public awareness of the risks of cyclones and to provide training to emergency personnel in the coastal regions of Bangladesh. [61]
In the thirty years after the 1970 cyclone, over 200 cyclone shelters were constructed in the coastal regions of Bangladesh. When the next destructive cyclone approached the country in 1991, volunteers from the Cyclone Preparedness Programme warned people of the cyclone two to three days before it struck land. Over 350,000 people fled their homes to shelters and other brick structures, while others sought high ground. While the 1991 cyclone killed over 138,000 people, this was significantly less than the 1970 storm, partly because of the warnings sent out by the Cyclone Preparedness Programme. However, the 1991 storm was significantly more destructive, causing US$1.5 billion (equivalent to $3 billion in 2023) compared to the 1970 storm's $0.086 billion (equivalent to $0.52 billion in 2023). [62] [63]
Footage of the incident appeared in the film Days of Fury (1979), directed by Fred Warshofsky and hosted by Vincent Price. [64]
The Vortex by Scott Carney and Jason Miklian focused on how Yayhia Khan's failure to respond to the aftermath of Bhola cyclone which sparked the 1971 Bangladesh war. [65] [66]
Other extremely deadly tropical cyclones outside the North Indian Ocean basin:
HMS Intrepid (L11) was one of two Fearless-class amphibious warfare ships of the Royal Navy. A landing platform dock (LPD), she served from 1967 until 1999. Based in HM Naval Base, Devonport, Plymouth, Devon and HM Naval Base Portsmouth, she saw service around the world over her 32-year life.
Hurricane Fifi, later known as Hurricane Orlene, was a catastrophic tropical cyclone that killed over 8,000 people in Honduras in September 1974, ranking it as the third deadliest Atlantic hurricane on record, only behind Hurricane Mitch in 1998, and the 1780 hurricane. Fifi is also the first billion-dollar hurricane not to make landfall in the United States. Originating from a strong tropical wave on September 14, the system steadily tracked west-northwestward through the eastern Caribbean. On September 16, the depression intensified into Tropical Storm Fifi just off the coast of Jamaica. The storm quickly intensified into a hurricane the following afternoon and attained its peak intensity on September 18 as a strong Category 2 hurricane. Maintaining hurricane intensity, Fifi brushed the northern coast of Honduras before making landfall in Belize the following day. The storm quickly weakened after landfall, becoming a depression late on September 20. Continuing westward, the former hurricane began to interact with another system in the eastern Pacific.
The 1991 Bangladesh cyclone was among the deadliest tropical cyclones in recorded history. It was also one of the most powerful cyclones in the Indian Ocean. Forming out of a large area of convection over the Bay of Bengal on April 24, the tropical cyclone initially developed gradually while meandering over the southern Bay of Bengal. On April 28, the storm began to accelerate northeastwards under the influence of the southwesterlies, and rapidly intensified to super cyclonic storm strength near the coast of Bangladesh on April 29. After making landfall in the Chittagong district of southeastern Bangladesh with winds of around 250 km/h (155 mph), the cyclone rapidly weakened as it moved through northeastern India, degenerating into a remnant low over the Yunnan province in western China.
The 1999 Odisha cyclone was the most intense recorded tropical cyclone in the North Indian Ocean and among the most destructive in the region. The 1999 Odisha cyclone organized into a tropical depression in the Andaman Sea on 25 October, though its origins could be traced back to an area of convection in the Sulu Sea four days prior. The disturbance gradually strengthened as it took a west-northwesterly path, reaching cyclonic storm strength the next day. Aided by highly favorable conditions, the storm rapidly intensified, attaining super cyclonic storm intensity on 28 October, before peaking on the next day with winds of 260 km/h (160 mph) and a record-low pressure of 912 mbar. The storm maintained this intensity as it made landfall on Odisha on 29 October. The cyclone steadily weakened due to persistent land interaction and dry air, remaining quasi-stationary for two days before slowly drifting offshore as a much weaker system; the storm dissipated on 4 November over the Bay of Bengal.
The 1970 North Indian Ocean cyclone season had no bounds, but tropical cyclones in the North Indian Ocean tend to form between April and December, with peaks in May and November. The 1970 season 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 season was also the deadliest tropical cyclone season globally, with 500,805 fatalities, mostly due to the aforementioned Bhola cyclone.
Extremely Severe Cyclonic Storm Sidr was a tropical cyclone that resulted in one of the worst natural disasters in Bangladesh. The fourth named and the deadliest storm of the 2007 North Indian Ocean cyclone season, Sidr formed in the central Bay of Bengal, and quickly strengthened to reach peak 1-minute sustained winds of 260 km/h (160 mph), making it a Category-5 equivalent tropical cyclone on the Saffir–Simpson scale. The storm eventually made landfall in Bangladesh on November 15, 2007, causing large-scale evacuations. At least 3,447 deaths have been blamed on the storm, with some estimates reaching 15,000.
Extremely Severe Cyclonic Storm Nargis was an extremely destructive and deadly tropical cyclone that caused the worst natural disaster in the recorded history of Myanmar during early May 2008. The cyclone made landfall in Myanmar on Friday, 2 May 2008, sending a storm surge 40 kilometres up the densely populated Irrawaddy delta, causing catastrophic destruction and at least 138,373 fatalities. The Labutta Township alone was reported to have 80,000 dead, with about 10,000 more deaths in Bogale. There were around 55,000 people missing and many other deaths were found in other towns and areas, although the Myanmar government's official death toll may have been under-reported, and there have been allegations that government officials stopped updating the death toll after 138,000 to minimise political fallout. The feared 'second wave' of fatalities from disease and lack of relief efforts never materialised. Damage was at $12 billion, making Nargis the costliest tropical cyclone on record in the North Indian Ocean at the time, before that record was broken by Cyclone Amphan in 2020.
Hurricane Tara was one of the deadliest Pacific hurricanes on record. The final tropical cyclone of the 1961 Pacific hurricane season, Tara formed on November 10 about 230 mi (365 km) off the coast of Mexico. It strengthened to reach maximum sustained winds of 85 mph (140 km/h) before making landfall in the Mexican state of Guerrero near Zihuatanejo. Hurricane Tara dissipated on November 12, bringing heavy rainfall and strong winds to locations inundated by 10 days of precipitation. Damage was light in the major port city of Acapulco, though further west along the coast, the effects of Tara were much worse. The city of Nuxco in Tecpan de Galeana municipality received the most damage and deaths from the hurricane. Throughout Mexico, at least 436 fatalities were reported, and damage exceeded $16 million.
Severe Cyclonic Storm Aila was the second named tropical cyclone of the 2009 North Indian Ocean cyclone season. Warned by both the Regional Specialized Meteorological Center (RMSC) and Joint Typhoon Warning Center (JTWC), Aila formed over a disturbance over the Bay of Bengal on May 23, 2009 and started to intensify and organize reaching sustained wind speeds of 110 kmh (70 mph). It was the worst natural disaster to affect Bangladesh since Cyclone Sidr in November 2007. A relatively strong tropical cyclone, it caused extensive damage in India and Bangladesh.
At least 29 tropical cyclones have affected Myanmar, a country adjacent to the Bay of Bengal in mainland Southeast Asia. Myanmar has witnessed some of the deadliest storms in the Bay of Bengal, including Cyclone Nargis in May 2008, which struck the low-lying Irrawaddy Delta near Yangon. Its winds and storm surge killed an estimated 140,000 people and left nearly $10 billion in damage. The country's worst natural disaster in the 20th century was a cyclone in 1968, which killed more than 1,000 people when it hit Rakhine State in northwestern Myanmar. One of the most powerful storms to ever hit the country was Cyclone Mocha, which it moved ashore northwestern Myanmar in May 2023, killing at least 413 people.
The 1971 Odisha cyclone was a devastating tropical cyclone that struck the Indian state of Odisha on October 29, 1971. The cyclone also affected the Indian state of West Bengal as well as East Pakistan, which had been devastated by the 1970 Bhola cyclone just less than a year prior and was in the middle of Bangladesh Liberation War.
The 1988 Bangladesh cyclone was one of the worst tropical cyclones in Bangladesh history. Striking in November 1988, the tropical system exacerbated the catastrophic damage from what was then considered the worst floods in Bangladesh's history. The tropical cyclone originated from a disturbance that developed within the Strait of Malacca on November 21. Tracking slowly westward, the initial tropical depression reached tropical storm status in the Andaman Sea. On November 26, the storm reached an intensity equivalent to that of a modern-day severe cyclonic storm and subsequently turned northward. Gradually intensifying as it had previously, the tropical cyclone reached peak intensity with winds of 125 mph (201 km/h) as it was making landfall near the Bangladesh–India border on November 29. Although the storm retained strong winds well inland, it was last monitored over central Bangladesh as a moderate cyclonic storm-equivalent on November 30.
Cyclonic Storm Komen was an unusual tropical cyclone that originated near the southern coast of Bangladesh and later struck the same country while drifting over the northern Bay of Bengal. The second named storm of the 2015 season, Komen brought several days of heavy rainfall to Myanmar, Bangladesh, and India. It formed as a depression on July 26 over the Ganges delta and moved in a circular motion around the northern Bay of Bengal. Komen intensified into a 75 km/h (45 mph) cyclonic storm and moved ashore southeastern Bangladesh on July 30. The system turned westward over land and was last noted over eastern India on August 2.
Intense Tropical Cyclone Idai was one of the worst tropical cyclones on record to affect Africa and the Southern Hemisphere. The long-lived storm caused catastrophic damage, and a humanitarian crisis in Mozambique, Zimbabwe, and Malawi, leaving more than 1,500 people dead and many more missing. Idai is the deadliest tropical cyclone recorded in the South-West Indian Ocean basin. In the Southern Hemisphere, which includes the Australian, South Pacific, and South Atlantic basins, Idai ranks as the second-deadliest tropical cyclone on record. The only system with a higher death toll is the 1973 Flores cyclone that killed 1,650 off the coast of Indonesia.
The 1994 Bangladesh cyclone was a powerful tropical cyclone in the Bay of Bengal. The cyclone closely followed the path, strength, and time of year of a deadly cyclone in 1991 that killed more than 138,000 people. The 1994 cyclone formed on April 29 as a depression, which organized and intensified significantly over the subsequent few days. On May 2, the cyclone attained winds of 215 km/h (135 mph), according to the India Meteorological Department (IMD). That day, the storm made landfall in southeastern Bangladesh, and rapidly weakened over land, before dissipating on May 3.
Tropical cyclones regularly affect the coastlines of most of Earth's major bodies of water along the Atlantic, Pacific, and Indian oceans. Also known as hurricanes, typhoons, or other names, tropical cyclones have caused significant destruction and loss of human life, resulting in about 2 million deaths since the 19th century. Powerful cyclones that make landfall – moving from the ocean to over land – are some of the most impactful, although that is not always the case. An average of 86 tropical cyclones of tropical storm intensity form annually worldwide, with 47 reaching hurricane/typhoon strength, and 20 becoming intense tropical cyclones, super typhoons, or major hurricanes.
Provincial elections were held in East Pakistan on 17 December 1970, ten days after general elections. A total of 1,850 candidates ran for the 300 seats in the East Pakistan Provincial Assembly. The result was a landslide victory for the Awami League, which won 288 of the 300 seats.