In Vanuatu, Bola dropped heavy rainfall, which destroyed two bridges and caused severe damage to islands in the group. At least 500,000 people lost their lives in the storm, primarily as a result of the storm surge that flooded [6] However, as Bola moved further southwards it entered a region of light and variable wind during February 27, which along with an area of high pressure in the Tasman Sea blocked Bola's movement southwards. The next day it generated peak wind velocities of 195 km/h (120 mph), though it quickly weakened as it accelerated southward. The winds damaged a few homes, including some in which the roofs were damaged or destroyed. [1][9] In addition, the strong winds downed several trees, and at the same time, erosion and landslides left hillsides bare without grass or trees.

It weakened further and was absorbed by a stationary trough near the South Island on March 12. [14], Cyclone Bola created some of the largest rainfall totals for a single storm in the history of New Zealand, with some locations receiving more than half of their annual rainfall totals from the storm. Water supplies were disrupted in two cities due to flooding. A building ridge of high pressure to its south caused the extratropical remnants of Bola to slow and turn to the west on March 7. 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. [8] Which turned south and began to affect the North Island of New Zealand on March 6. [13][14] As it impacted the island nation for a second time, gale-force winds of up to 81 km/h (50 mph) and waves of up to 5 m (16 ft) were observed. The UN General Assembly adopted a proposal to improve its ability to provide aid to disaster-stricken countries. Two bridges on Malakula were destroyed, and several other bridges were flooded or damaged. The Bhola cyclone made landfall in East Pakistan (today known as Bangladesh). Rainfall in Northland Region caused flooding and outages to telephone and power. [13] The system subsequently affected the island nation for a second time between March 3 and 4. It turned southward on March 9, and on March 12 was absorbed by a stationary trough in the Westerlies near the western coast of the South Island. [4][5] During that day the system moved south-westwards and passed about 260 km (160 mi) to the north of Nadi, Fiji, before it started to move north-westwards during February 25. Damage totaled over $82 million (1988 USD). The exact death toll will never be known. The passage of the cyclone also left several buildings, roads, and crop fields damaged. [8][9] On March 3, its winds dropped below hurricane-force,[8] and it gradually lost its tropical characteristics. The next day, the storm passed about 110 km (70 mi) north of the North Island. A total of 1,765 farmers were affected by the flooding, accounting for about 3,600 hectares (8,900 acres) of damaged crop fields and about $90 million in crop damage (1988 NZD, $82 million 1988 USD). [8] The most affected locations were Epi island, the Shepherd Islands, and the islands in Malampa Province, and throughout the country the cyclone affected more than 15,000 people and 3,000 houses. 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.

The 1970 Bhola cyclone was the strongest storm of the 1970 North Indian Ocean cyclone season. However, the 1991 storm was significantly more destructive, causing 1.5 billion dollars in damage (2 billion inflation-adjusted) compared to the 1970 storm's 86.4 million dollars in damage (inflation-adjusted: 480 million).

[9], Cyclone Bola remained near Vanuatu for about a week,[11] during which it reached its peak intensity while executing a cyclonic loop. [14] All six fishermen were subsequently presumed dead after repeated air searches had failed to find them. Most of the people that were killed, were killed in East Pakistan (Bangladesh), because of the storm surge that caused flooding. [11] In a five-day period the cyclone dropped about 450 mm (17.7 in) of rainfall. 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. It also affected India and left $86.4 million in damage. The system traveled north and intensified, driving into the low-lying delta area overnight on 12 November, during an … [1] Heavy rainfall totals of up to and over 300 mm (12 in) were observed in the regions of Auckland and Northland. In Whangaruru Harbour, Northland, a samaritan act accounted for another Bola fatality when an elderly male long time resident of Rapata road Oakura Bay attempted to tie down a neighbours empty water tank.

[3], The system that was to become Severe Tropical Cyclone Bola was first noted during February 24, as a depression that had developed within the South Pacific Convergence Zone about 850 km (530 mi) to the north-east of Nadi, Fiji. [2] Three people were killed due to flooding, and hundreds were evacuated when a swollen river threatened Wairoa. The 1970 Bhola cyclone was a devastating tropical cyclone that struck East Pakistan and India's West Bengal on November 3, 1970. For the deadly cyclone in 1970 that struck Bangladesh, see, Satellite image of Cyclone Bola near peak intensity, CS1 maint: multiple names: authors list (, Australian tropical cyclone intensity scale, "Priority Setting for Government Investment in Forestry Conservation Schemes-An Example from New Zealand", "Tropical Cyclone Operational Plan for the South Pacific and Southeast Indian Ocean", "TCWC Wellington Best Track Data 1967–2006", Final report on Tropical cyclone Bola: 26 February - 4 March, 1988, Chapter IV — Summary of South Pacific and South Indian Ocean Tropical Cyclones, "A Diagnostic Study of the Extratropical Precipitation Resulting from Tropical Cyclone Bola", 10.1175/1520-0493(1993)121<2690:ADSOTE>2.0.CO;2, "Cyclone Bola : A study of the psychological after-effects".

Marine life, essential part of … [1] Additionally, beginning on about 6 March, the cyclone began affecting the North Island with strong easterly winds of over hurricane force, caused by the interaction between the extratropical remnants of Bola and a ridge of high pressure to its south.
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[4] The system subsequently moved south-westwards which meant that the islands of Maewo and Pentecost were threatened. In Te Karaka in Gisborne, a flooded river forced 500 residents to evacuate. The Bhola cyclone formed over the Bay of Bengal and travelled north, gusting to 205 kph (130 mph) before making landfall in East Pakistan on the evening of November 12, unfortunately coinciding with high tide. [9] By March 4, Bola had completed the transition into an extratropical cyclone. From Simple English Wikipedia, the free encyclopedia, The Bhola cyclone on November 11, 1970, at 0858, "NOAA Researcher's Warning Helps Save Lives in Bangladesh", National Oceanic and Atmospheric Administration, Spiritus-temporis.com - 1970 Bhola Cyclone, https://simple.wikipedia.org/w/index.php?title=1970_Bhola_cyclone&oldid=6653406, Creative Commons Attribution/Share-Alike License. The cyclone first affected Fiji, where it produced gale-force winds and strong waves.

In Vanuatu, Bola dropped heavy rainfall, which destroyed two bridges and caused severe damage to islands in the group. At least 500,000 people lost their lives in the storm, primarily as a result of the storm surge that flooded [6] However, as Bola moved further southwards it entered a region of light and variable wind during February 27, which along with an area of high pressure in the Tasman Sea blocked Bola's movement southwards. The next day it generated peak wind velocities of 195 km/h (120 mph), though it quickly weakened as it accelerated southward. The winds damaged a few homes, including some in which the roofs were damaged or destroyed. [1][9] In addition, the strong winds downed several trees, and at the same time, erosion and landslides left hillsides bare without grass or trees.

It weakened further and was absorbed by a stationary trough near the South Island on March 12. [14], Cyclone Bola created some of the largest rainfall totals for a single storm in the history of New Zealand, with some locations receiving more than half of their annual rainfall totals from the storm. Water supplies were disrupted in two cities due to flooding. A building ridge of high pressure to its south caused the extratropical remnants of Bola to slow and turn to the west on March 7. 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. [8] Which turned south and began to affect the North Island of New Zealand on March 6. [13][14] As it impacted the island nation for a second time, gale-force winds of up to 81 km/h (50 mph) and waves of up to 5 m (16 ft) were observed. The UN General Assembly adopted a proposal to improve its ability to provide aid to disaster-stricken countries. Two bridges on Malakula were destroyed, and several other bridges were flooded or damaged. The Bhola cyclone made landfall in East Pakistan (today known as Bangladesh). Rainfall in Northland Region caused flooding and outages to telephone and power. [13] The system subsequently affected the island nation for a second time between March 3 and 4. It turned southward on March 9, and on March 12 was absorbed by a stationary trough in the Westerlies near the western coast of the South Island. [4][5] During that day the system moved south-westwards and passed about 260 km (160 mi) to the north of Nadi, Fiji, before it started to move north-westwards during February 25. Damage totaled over $82 million (1988 USD). The exact death toll will never be known. The passage of the cyclone also left several buildings, roads, and crop fields damaged. [8][9] On March 3, its winds dropped below hurricane-force,[8] and it gradually lost its tropical characteristics. The next day, the storm passed about 110 km (70 mi) north of the North Island. A total of 1,765 farmers were affected by the flooding, accounting for about 3,600 hectares (8,900 acres) of damaged crop fields and about $90 million in crop damage (1988 NZD, $82 million 1988 USD). [8] The most affected locations were Epi island, the Shepherd Islands, and the islands in Malampa Province, and throughout the country the cyclone affected more than 15,000 people and 3,000 houses. 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.

The 1970 Bhola cyclone was the strongest storm of the 1970 North Indian Ocean cyclone season. However, the 1991 storm was significantly more destructive, causing 1.5 billion dollars in damage (2 billion inflation-adjusted) compared to the 1970 storm's 86.4 million dollars in damage (inflation-adjusted: 480 million).

[9], Cyclone Bola remained near Vanuatu for about a week,[11] during which it reached its peak intensity while executing a cyclonic loop. [14] All six fishermen were subsequently presumed dead after repeated air searches had failed to find them. Most of the people that were killed, were killed in East Pakistan (Bangladesh), because of the storm surge that caused flooding. [11] In a five-day period the cyclone dropped about 450 mm (17.7 in) of rainfall. 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. It also affected India and left $86.4 million in damage. The system traveled north and intensified, driving into the low-lying delta area overnight on 12 November, during an … [1] Heavy rainfall totals of up to and over 300 mm (12 in) were observed in the regions of Auckland and Northland. In Whangaruru Harbour, Northland, a samaritan act accounted for another Bola fatality when an elderly male long time resident of Rapata road Oakura Bay attempted to tie down a neighbours empty water tank.

[3], The system that was to become Severe Tropical Cyclone Bola was first noted during February 24, as a depression that had developed within the South Pacific Convergence Zone about 850 km (530 mi) to the north-east of Nadi, Fiji. [2] Three people were killed due to flooding, and hundreds were evacuated when a swollen river threatened Wairoa. The 1970 Bhola cyclone was a devastating tropical cyclone that struck East Pakistan and India's West Bengal on November 3, 1970. For the deadly cyclone in 1970 that struck Bangladesh, see, Satellite image of Cyclone Bola near peak intensity, CS1 maint: multiple names: authors list (, Australian tropical cyclone intensity scale, "Priority Setting for Government Investment in Forestry Conservation Schemes-An Example from New Zealand", "Tropical Cyclone Operational Plan for the South Pacific and Southeast Indian Ocean", "TCWC Wellington Best Track Data 1967–2006", Final report on Tropical cyclone Bola: 26 February - 4 March, 1988, Chapter IV — Summary of South Pacific and South Indian Ocean Tropical Cyclones, "A Diagnostic Study of the Extratropical Precipitation Resulting from Tropical Cyclone Bola", 10.1175/1520-0493(1993)121<2690:ADSOTE>2.0.CO;2, "Cyclone Bola : A study of the psychological after-effects".

Marine life, essential part of … [1] Additionally, beginning on about 6 March, the cyclone began affecting the North Island with strong easterly winds of over hurricane force, caused by the interaction between the extratropical remnants of Bola and a ridge of high pressure to its south.

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