Meteorological history | |
---|---|
Formed | January 5, 1988 |
Dissipated | January 14, 1988 |
Category 4 severe tropical cyclone | |
10-minute sustained (FMS) | |
Highest winds | 185 km/h (115 mph) |
Lowest pressure | 925 hPa (mbar);27.32 inHg |
Category 5-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 260 km/h (160 mph) |
Overall effects | |
Fatalities | 2 |
Damage | $500,000 (1988 USD) |
Areas affected | Tuvalu,Solomon Islands,Vanuatu,New Caledonia |
IBTrACS | |
Part of the 1987–88 South Pacific cyclone season |
Severe Tropical Cyclone Anne was one of the most intense tropical cyclones within the South Pacific basin during the 1980s. The cyclone was first noted on January 5,1988 as a weak tropical depression to the northeast of Tuvalu,in conjunction with the future Typhoon Roy in the Northern Hemisphere. Over the next few days,the system gradually developed while moving southwestward. Once it became a tropical cyclone,it was named Anne on January 8. The next day,Anne rapidly intensified,becoming the fourth major tropical cyclone to affect Vanuatu within four years. On January 11,Anne peaked in intensity while it was equivalent to a Category 5 on the Saffir–Simpson hurricane wind scale,and a Category 4 on the Australian tropical cyclone intensity scale. After turning southward on January 12,Anne struck New Caledonia,becoming the strongest tropical cyclone to affect the French Overseas Territory. The system subsequently weakened as it started to interact with Tropical Cyclone Agi. Anne weakened into a depression and was last noted on January 14 to the south-east of New Caledonia.
Several islands within the Solomon Islands reported extensive property and crop damage. Within Vanuatu,Anne brought heavy rains,flooding,and a storm surge. These effects damaged houses,crops,and property,especially on Ureparapara islands and the Torres Islands. Extensive damage was reported in New Caledonia after it was exposed to a prolonged period of storm force winds,with the eastern and southern coasts particularly affected. On January 12,the system produced the highest daily rainfall totals since 1951 in several areas. Two people were killed after they attempted to cross a flooded river,and about 80 others were injured by the cyclone. Due to the impact of this storm,the name Anne was retired.
On January 5, 1988, the Fiji Meteorological Service (FMS) started to monitor a shallow tropical depression that developed within the monsoon trough about 540 km (335 mi) northeast of Tuvalu. [1] [2] [3] At around the same time, a twin depression developed within the Northern Hemisphere monsoon trough, which eventually became Typhoon Roy. [4] Over the next two days the Southern Hemisphere system developed further as it was steered towards the south-southwest along an area of high pressure, before it became equivalent to a tropical storm while passing through the Tuvaluan islands. [3] [1] [5] As a result, the United States Joint Typhoon Warning Center (JTWC) designated the system as Tropical Cyclone 07P and started to issue advisories on it. [3] [6] After organized further, the FMS named the storm Anne after it became equivalent to a modern-day Category 2 on the Australian tropical cyclone intensity scale. [1] [2] [3] On January 9, the cyclone started to rapidly intensify while continuing to move towards the south-southwest. Later that day, the JTWC reported that the system had become equivalent to a Category 1 on the Saffir–Simpson hurricane wind scale (SSHWS), and the FMS upgraded Anne to a Category 3 severe tropical cyclone on the Australian Scale. [1] [3] Early on January 10, the cyclone passed through Temotu Province and about 55 km (35 mi) to the northwest of Anuta Island. [1] [3]
Later on January 10, Anne directly passed over Vanuatu's Torres Islands and came within 65 km (40 mi) of Ureparapara in the Banks Islands. [1] The cyclone continued to move to the south-southwest and affected the northern islands of Vanuatu. [1] Early on January 11, the FMS reported that Anne had peaked, with estimated 10-minute sustained winds near its center of 185 km/h (115 mph), equivalent to a Category 4 severe tropical cyclone on the Australian scale. [1] [3] At around the same time the JTWC reported that Anne had peak 1-minute peak sustained winds of 260 km/h (160 mph), which made it equivalent to a Category 5 hurricane on the SSHWS. [3] [6] This made it one of the most intense tropical cyclones of the 1980s. [1] Over the next day, Cyclone Anne turned south and rapidly weakened as it encountered upper-level wind shear, approaching the French overseas territory of New Caledonia. [1] Late on January 12, Anne weakened into a modern-day Category 2 tropical cyclone, before it made landfall on New Caledonia about 110 km (70 mi) to the north-northwest of Noumea. [1] After the cyclone re-emerged into the Coral Sea, the JTWC downgraded Anne to tropical storm status. [3] Later on January 13, Cyclone Anne started to interact with Cyclone Agi, which had rapidly moved south-eastward towards the "relatively deeper" Anne. [1] [3] [7] Agi had developed two days prior near the Louisiade Archipelago, about 1,200 km (745 mi) northwest of Cyclone Anne. [3] [7] Early on January 14, Anne weakened into a depression and subsequently dissipated southeast of New Caledonia as it was caught up in the upper westerly flow. [2] [6] [3]
During its early stages of development, Anne passed through the central islands of Tuvalu, causing minor damage to houses and crops such as bananas and coconuts. [1] The storm passed to the north of Funafuti where strong gale force winds of 70 km/h (45 mph) were recorded. [8] The system subsequently affected the Solomon Island province of Temotu between January 9 – 10 while it had sustained winds of 150 km/h (95 mph). [1] However, the cyclone's center did not pass directly over any island, and the smaller islands escaped the destructive hurricane-force winds. [1] Because Anne moved through the province at about 30 km/h (20 mph), any gale and storm force winds that affected the islands were not prolonged. [9] Anuta, Utupua, the Duff Islands and the Reef Islands all reported extensive damage to property and crops, with at least 25 houses and 5 classrooms damaged. [9] [10]
The system affected the Northern Vanuatu Islands between January 10 – 11 and was the fourth major tropical cyclone to affect the island nation since 1985, after Severe Tropical Cyclones Eric, Nigel and Uma. [11] Ahead of Anne affecting Vanuatu, various alerts and warnings were issued including a hurricane warning. [10] During January 10, the cyclone directly passed over the Torres Islands and came within 65 km (40 mi) of the Banks Islands, although it missed Vanuatu's most populated districts around Port Vila and the rest of Espiritu Santo. [1] [12] Within Vanuatu, over 1600 people were made homeless while wind gusts of up to 225 km/h (140 mph) were recorded. [11] [13] [14] Torrential rain, flooding and storm surge caused damage to houses, crops and property while triggering a landslide on the island of Epi. [11] [13] [14] The hardest hit area was Torba Province with severe damage recorded on the islands of Ureparapara and the Torres Islands, while extensive damage was recorded on the islands of Vanua Lava and Gaua. [10] [11] [15] Within the province, virtually the whole population lost their houses, as well as their cash crops. [15] [16] There were reports of 4–5 m (13–16 ft) tidal waves, washing away houses on the west coast of Ureparapara, while significant wave heights of over 11 m (36 ft) were recorded. [1] [17] Within the province of Sanma, severe damage was recorded on Espiritu Santo after Anne flooded huts, unroofed school buildings, uprooted coconut trees and destroyed the main wharf. [16] [18] Overall the total damages from Anne in Vanuatu, were estimated at US$500,000. [19]
In conjunction with Tropical Cyclone Agi, Anne affected the whole of New Caledonia between January 11–15, becoming the most powerful tropical cyclone to affect the French overseas territory in 12 years. [20] Winds in Noumea reached up to 150 km/h (95 mph), although there was no serious damage there. [21] Prolonged storm force winds left extensive damage to the island, with the eastern and southern coasts particularly affected. [1] [10] On January 12, the system produced the highest daily rainfall totals since 1951, with Noumea recording 262 mm (10.3 in). [22]
Larger rainfall totals included 713 mm (28.1 in) in Goro and 519 mm (20.4 in) in Thio. [23] Two people were killed after they attempted to cross a flooded river. [20] Floods also swept away crops, huts and topsoil belonging to indigenous Melanesians that lived in coastal villages. [24] [25] Some areas reported crop damage between 90 and 100%. [10] [26] Most of the roads within the territory were left unusable while all international flights to the territory were cancelled. [21] About half of the houses in Poindimié were damaged or destroyed. [21] The last wooden Royal Navy boat was scheduled to be sunk on January 12, but was moved to January 19 due to the cyclones. [27] [28] Overall, there were about 80 injuries related to the cyclone in New Caledonia. [20]
The aftermath of the cyclone was marked by a distinct lack of a quantitative assessment within the Solomon Islands; with few boats or aircraft near the remote islands, relief measures were slow to get underway. [9] However, 11 men aboard the United States Navy vessel USS Barbour County received Humanitarian Service Medals from the United States Department of Defense after aiding storm victims on Tikopia and Anuta from January 16 to 19. [29] [30] [31]
With some residents forced to seek refuge in caves, the Government of Vanuatu asked the Australian, New Zealand and American governments for emergency food supplies and other assistance. [10] [15] [16] In accordance, the Royal Australian Air Force (RAAF) dispatched two Hercules transport planes to help with recovery efforts. [32] The first carried a helicopter that transported Vanuatu military forces, medical teams and supplies to the affected northern islands, especially remote villages inaccessible to larger aircraft. [12] [32] [33] The other plane was used to transport more than 16,000 kilograms (35,000 lb) of fuel and relief supplies including food and shelter provisions. [32] [34] The Royal New Zealand Air Force also provided a plane, which transported relief supplies from Espiritu Santo to the northern islands up to three times daily, with the bulk of supplies donated by Australia. [12] The European Commission provided Vanuatu with €100,000 in emergency aid to purchase local foods, including rice, preserved meat, and fish, and to distribute it to Anne's victims. [35] The total cost of relief and reconstruction efforts was estimated between US$1.2–2 million. [11] [16]
Within the Paiti-la-Tonuatua area to the north of Noumea, New Caledonia Air Force helicopters rescued several people who had moved to the roofs of their houses. [36] Despite the severe crop damage, no areas were declared disasters by January 20. The South Pacific division of the Adventist Development and Relief Agency sent AU$5,000 to New Caledonia for relief efforts. [10] [26] Emergency funding of F300,000 was given to New Caledonia to help with the relief effort by the French Minister of the Interior and Minister of Overseas Territories. [37] The European Commission also provided New Caledonia with €85,000, which was distributed by the United Nations High Commissioner for Refugees in the form of cash donations to the worst-affected families. [38] After the season, the name "Anne" was retired by the World Meteorological Organization. [39]
The 2002–03 South Pacific cyclone season was the most active and longest tropical cyclone season since 1997–98, with ten tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. The season started earlier than normal, with two systems developing before the official start of the season on November 1, 2002, while the final system dissipated on June 9, 2003, after the season had officially ended on April 30. During the season, tropical cyclones were officially monitored by the Regional Specialized Meteorological Centre (RSMC) in Nadi, Fiji and the Tropical Cyclone Warning Centres in Brisbane, Australia and Wellington, New Zealand. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC), also monitored the basin and issued unofficial warnings for American interests. RSMC Nadi attaches a number and an F suffix to tropical disturbances that occur within the basin, while the JTWC designates significant tropical cyclones with a number and a P suffix. RSMC Nadi, TCWC Wellington and TCWC Brisbane all use the Australian Tropical Cyclone Intensity Scale and estimate windspeeds over a ten-minute period, while the JTWC estimates sustained winds over a one-minute period, which are subsequently compared to the Saffir–Simpson Hurricane Scale (SSHS).
Severe Tropical Cyclone Ivy was a tropical cyclone that affected about 25% of the population of Vanuatu in February 2004. It was first classified as a tropical disturbance on February 21 between Vanuatu and Fiji. The system tracked northwestward, gradually organizing and intensifying. After attaining tropical storm status on February 23, Ivy strengthened more quickly as it turned southwestward toward Vanuatu. It attained peak winds of 165 km/h (103 mph) while moving over Vanuatu, making it an intense Category 4 cyclone on the Australian Region Tropical Cyclone Intensity Scale. By the time it passed through Vanuatu, Ivy had turned southeastward, and it gradually weakened while accelerating. After becoming extratropical on February 28, it passed just east of New Zealand and eventually dissipated on March 2.
Severe Tropical Cyclone Bola was one of the costliest cyclones in the history of New Zealand, causing severe damage as an extratropical cyclone when it passed near the country in March 1988. It formed on February 24 to the north of Fiji, and tracking generally southwestward it reached hurricane-force winds near Vanuatu on February 28. The next day it generated peak wind velocities of 195 km/h (120 mph), though it quickly weakened as it accelerated southward. On March 4, Bola transitioned into an extratropical storm, passing to the north of the North Island of New Zealand on March 8. It weakened further and was absorbed by a stationary trough near the South Island on March 12.
The 1987–88 South Pacific cyclone season was a quiet tropical cyclone season with five tropical cyclones and 2 severe tropical cyclones, observed within the South Pacific basin to the east of 160°E.
The 1988–89 South Pacific cyclone season was an active tropical cyclone season with an above average number of tropical cyclones observed.
The 1991–92 South Pacific cyclone season was an above average tropical cyclone season, with eleven tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. The first tropical cyclone of the season was first noted on November 13, 1991, while the last tropical cyclone dissipated on May 2, 1992. During the season at least 21 people were killed by tropical cyclones, while Tropical Cyclones Cliff and Innis were the only tropical cyclones not to cause any damage to any country in the Southern Pacific.
Severe Tropical Cyclone Rewa affected six countries and caused 22 deaths on its 28-day journey across the South Pacific Ocean in December 1993 and January 1994. Cyclone Rewa developed from a tropical disturbance on 28 December south of Nauru. After forming, Rewa moved southwest through the Solomon Islands, crossing the 160th meridian east from the South Pacific basin into the Australian region. The cyclone began to strengthen steadily and turned southward, paralleling the eastern Australian coast through 31 December. Rewa reached its initial peak intensity as a Category 4 tropical cyclone on 2 January. It maintained this intensity for about 12 hours before an increase in wind shear induced its weakening by 3 January. The cyclone turned southeastward and moved back into the South Pacific basin on 4 January, before it passed over New Caledonia between 5–6 January. After affecting New Caledonia, Rewa weakened to a tropical depression and turned northwestward before re-entering the Australian basin on 10 January.
The 1995–96 South Pacific cyclone season was a below average South Pacific tropical cyclone season's on record, with only five tropical cyclones occurring within the South Pacific Ocean to the east of 160°E. The season officially ran from November 1, 1995, until April 30, 1996. The first storm developed on January 12, while the last one dissipated on April 2. During the season the most intense tropical cyclone was Severe Tropical Cyclone Beti, which reached a minimum pressure of 935 hPa (27.61 inHg) as it affected New Caledonia. After the season ended Beti's name was the only name to be retired from the tropical cyclone naming lists and was replaced with Bune, after it inflicted over 5.6 million (USD) worth of damage to Australia, Vanuatu, New Caledonia and New Zealand.
Severe Tropical Cyclone Jasmine was a powerful and long-lived annular tropical cyclone that affected several countries, particularly Vanuatu and Tonga, over a 16-day span in February 2012. The system was the second cyclone and the only severe tropical cyclone of the relatively quiet 2011–12 South Pacific cyclone season. Cyclone Jasmine developed from an area of disturbed weather on 1 February in the Gulf of Carpentaria. Initially, the storm moved towards the east and across the Cape York Peninsula. As it moved across the South Pacific, earlier existing wind shear conditions lessened, and Jasmine began to strengthen at a faster rate. Steadily intensifying, Jasmine reached peak intensity on 8 February as a Category 4 equivalent on the Saffir–Simpson Hurricane Scale, while beginning to show annular characteristics.
Severe Tropical Cyclone Tia was the first of six tropical cyclones to affect Vanuatu during the 1991–92 South Pacific cyclone season. The system was first noted within the South Pacific convergence zone as a small tropical depression on November 13, to the northeast of the Solomon Islands. Over the next few days the system gradually developed further within an area of light winds in the upper troposphere, before it was named Tia early on November 16. Later that day due to a developing northerly steering current, the system slowed and undertook a small anticlockwise loop before starting to move towards the southwest and rapidly intensify. After rapidly intensifying throughout November 16 and 17, Tia passed within 55 km (35 mi) of the Solomon Island: Anuta at around 1800 UTC on November 17, before passing near Tikopia Island six hours later. As Tia moved near Tikopia, the system reached its peak intensity as a category 3 severe tropical cyclone, with 10‑minute sustained windspeeds of 140 km/h (85 mph).
Severe Tropical Cyclone Fran was the third tropical cyclone within four weeks to impact Vanuatu in 1992. Fran formed on 4 March and then gradually intensified, with winds reaching gale-force on 5 March, and hurricane-force a few days later. Few days later, Cyclone Fran reached severe tropical cyclone status near Vanuatu, and also became a powerful Category 5-equivalent on the Saffir–Simpson Hurricane Scale. The storm weakened somewhat due to land interaction, but briefly re-intensified after moving away from land. Fran gradually weakened over the next several days over less favorable conditions. Meanwhile, the storm passed north of New Caledonia. Eventually, as a Category 2 system on the Australian scale, Fran made landfall on Queensland on 16 March. Afterwards, Cyclone Fran turned towards the southeast and eventually headed back out to sea, eventually dissipating the next day. On Efate, over 130 houses lost roofs. Along Queensland, two rivers sustained major flooding, but no deaths were attributed to this cyclone. Total damage from the system was AU$8–10 million. Moderate damage was also reported in Fiji. In New Caledonia, the storm brought flooding and landslides.
Severe Tropical Cyclone Beni was an intense tropical cyclone that affected four countries, on its 18-day journey across the South Pacific Ocean during January and February 2003. The system originally developed during 19 January as a weak tropical disturbance within the monsoon trough, to the northeast of the Santa Cruz Islands. Over the next few days the system gradually developed further before it was classified as a tropical cyclone and named Beni during 24 January.
Severe Tropical Cyclone Drena was a powerful tropical cyclone that caused significant damage throughout New Zealand. A tropical depression formed on January 2, 1997. After crossing Vanuatu and emerging into the Coral Sea, the storm began to intensify, and by January 6, had attained peak intensity. After attaining peak intensity, Drena began to weaken. Cyclone Drena later brushed New Caledonia, bringing some damage. After transitioning into an extratropical cyclone on January 9, Drena brought impact to New Zealand. Damage totaled to $6.7 million and 3 people were killed. Roughly 140 people were evacuated after 44 homes were flooded. After the season, Drena was retired.
Severe Tropical Cyclone Yali was one of seven severe tropical cyclones to develop during the 1997–98 South Pacific cyclone season. The system that was to become Yali was first noted as a tropical disturbance, to the northeast of Vanuatu during March 17. Over the next couple of days, the system moved towards the south-west and gradually developed further, before it was named Yali during March 19, after it had developed into a tropical cyclone. After it was named Yali re-curved and started moving towards the south-southeast, as the monsoonal flow to the north of the system strengthened. While the system was active, Yali affected Vanuatu and New Caledonia before the extra-tropical remnants impacted New Zealand where a man was killed and widespread power outages and damage were reported.
Severe Tropical Cyclone Eric was one of two tropical cyclones to affect the island nations of Vanuatu and Fiji within a week during January 1985. The precursor shallow depression developed within the monsoon trough during 13 January, to the west of Espiritu Santo, Vanuatu. On 16 January, the storm developed-hurricane-force winds and Eric began to undergo rapid deepening. While two different agencies differ on when and how strong Eric was at its peak, it was believed to have peak on 17 January while passing through the Fiji island group. Shortly after its peak, Eric began to weaken steadily, and by 20 January, Severe Tropical Cyclone Eric had ceased to exist as a tropical cyclone. Combined with another storm – Cyclone Nigel – Eric caused 25 fatalities and $40 million worth of damage. A total of 299 farms were affected as well as the airport in Nadi. About 30,000 people were left homeless. Severe crop damage was also reported. Viti Levu sustained the worst effects from Cyclone Eric. During the aftermath of the storm, a number of first world countries distributed aid for victims of Eric.
Severe Tropical Cyclone Esau was the strongest tropical cyclone to affect New Caledonia on record. A shallow tropical depression developed within the monsoon trough during 24 February 1992, about 370 km (230 mi) to the northeast of Port Vila, Vanuatu. Over the next day, the system gradually developed further as it moved towards the south-west under the influence of a northerly steering flow, before it passed over Pentecost Island in northern Vanuatu during 25 February. After passing over Pentecost the system continued to move towards the southwest and passed near the island of Malampa before the depression turned northwards and executed a small clockwise loop as it passed over the island of Espiritu Santo. The system was subsequently named Esau during 26 February, after it had developed into a tropical cyclone. Over the next couple of days, the system moved south-westwards towards Australia and away from the islands of Vanuatu. Esau subsequently executed a second clockwise loop during 28 February, before it peaked as a Category 4 tropical cyclone on both the Australian tropical cyclone intensity scale and the Saffir-Simpson hurricane wind scale. After it had peaked the system moved south-eastwards and threatened Southern Vanuatu, before turning southwards and threatening the French overseas territory of New Caledonia. Esau made landfall on the French territory during 4 March, as a category 3 severe tropical cyclone before degenerating into an extratropical cyclone during 5 March. The systems remnants made landfall on New Zealand's North Island during 8 March, before they were last noted during the next day over the South Pacific Ocean.
Severe Tropical Cyclone Betsy was a strong and long-lived tropical cyclone which impacted 8 island nations.
Tropical Cyclone Sose was a moderate storm system that chiefly impacted the island nation of Vanuatu in early April 2001. The developing cyclone was first detected on April 3, while situated well to the northeast of Vanuatu. As atmospheric conditions became more conducive to intensification, the disturbance gradually consolidated as it drifted toward the west-southwest. After receiving the name Sose on April 5, the cyclone was driven southeastward, passing just west of Espiritu Santo and neighboring islands. Although it never made landfall, Sose was particularly expansive, producing a wide area of gale-force winds. The cyclone peaked in strength between April 7 and 8 with maximum 10-minute sustained winds of 110 km/h (68 mph) and 1-minute sustained winds of 130 km/h (81 mph), placing it at Category 2 intensity on the Australian tropical cyclone intensity scale. Ultimately, stronger wind shear and an increasingly hostile upper-air pattern took their toll on the cyclone as it progressed due south; Sose lost tropical characteristics to the northeast of Norfolk Island by April 12. The extratropical remnants of Sose continued into the Tasman Sea.
Severe Tropical Cyclone Hola had significant effects across Vanuatu in March 2018, resulting in the deaths of three people. Forming as a broad tropical disturbance on 5 March, the system slowly consolidated over the next few days before developing into a tropical cyclone on 6 March. Afterwards, a pinhole eye began to emerge and rapid intensification ensued.
The following is a list of all reported tropical cyclones within the South Pacific Ocean to the east of 160°E after the start of World War II in September 1939 and before the start of the 1950s decade.