Meteorological history | |
---|---|
Formed | December 19,2001 |
Dissipated | January 2,2002 |
Category 4 severe tropical cyclone | |
10-minute sustained (FMS) | |
Highest winds | 185 km/h (115 mph) |
Highest gusts | 250 km/h (155 mph) |
Lowest pressure | 930 hPa (mbar);27.46 inHg |
Category 3-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 185 km/h (115 mph) |
Overall effects | |
Fatalities | 1 indirect |
Damage | $51.4 million (2002 USD) |
Areas affected | Wallis and Futuna,Niue,Tonga;especially Vava'u,and New Zealand |
IBTrACS | |
Part of the 2001–02 South Pacific cyclone season |
Severe Tropical Cyclone Waka (Fiji Meteorological Service designation:03F,Joint Typhoon Warning Center designation:07P) was one of the most destructive tropical cyclones ever to affect the nation of Tonga. Waka originated within the near-equatorial trough in mid-December 2001,although the system remained disorganized for more than a week. The storm gradually matured and attained tropical cyclone status on December 29,2001. Subsequently,Waka underwent rapid intensification in which it attained its peak intensity as a Category 4 severe tropical cyclone (Australian tropical cyclone intensity scale) on December 31,with winds of 185 km/h (115 mph). Shortly thereafter,it passed directly over Vavaʻu,Tonga,resulting in widespread damage. By January 1,2002,the cyclone began to weaken as it underwent an extratropical transition. The remnants of Waka persisted for several more days and were last observed near the Southern Ocean on January 6,2002.
Although the storm affected several countries along its path,Waka left the most significant losses in Tonga,where it killed one person and wrought 104.2 million paʻanga ($51.3 million USD) in damage. Hundreds of structures,including 200 in the island's largest city,and much of the nation's agriculture were destroyed. Winds in excess of 185 km/h (115 mph) battered Vava'u,defoliating nearly every tree on the island. In addition to infrastructural and public losses,the environment was also severely affected;a native species of bat lost roughly 80% of its population due to the lack of fruit. Following the storm,Tonga requested international aid to cope with the scale of damage. Due to the severity of damage,the name Waka was later retired and replaced with Wiki. According to a study by Janet Franklin et al.,storms similar in intensity to Waka,on average,strike Tonga once every 33 years. [1]
In mid-December 2001, at the end of a Madden–Julian oscillation pulse, twin equatorial monsoonal troughs developed in the Northern and Southern Hemispheres. Although warm sea surface temperatures of 30 °C (86 °F) in the region favored development of a tropical cyclone, the southern trough developed substantially slower than the northern one. [2] On December 19, the southern component was classified as Tropical Depression 03F by the Fiji Meteorological Service; at this time the depression was situated just east of the Solomon Islands. [3] The northern component eventually developed into Typhoon Faxai, an extremely powerful Category 5 equivalent cyclone. [4] Unlike Faxai, the precursor to Cyclone Waka developed slowly, mainly because of moderate wind shear in the region. Moving southeastward, the system gradually became more organized. [2] On two occasions, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert; however, the agency later canceled them both times. [5] By December 27, the depression had entered a region of lesser shear, favoring significant development of the system. [2] [3] The following day, the JTWC classified the system as Tropical Depression 07P, when the storm was situated roughly 640 km (400 mi) northwest of Pago Pago, American Samoa. [6]
Tracking towards the southwest in response to a mid-level ridge to the southeast, the depression quickly intensified, attaining gale-force winds on December 29. Upon doing so, it was upgraded to a tropical cyclone and given the name Waka. Shortly thereafter, the storm underwent rapid intensification; [2] roughly 24 hours after being named, Waka attained sustained winds of 120 km/h (75 mph). [7] During December 30, the center of the storm brushed Wallis Island before turning towards the southeast and accelerating due to an approaching trough from the northwest. Continuing to intensify, Waka passed directly over Niuafo'ou on December 31 with winds of 150 km/h (93 mph). [2] Later that day, the cyclone attained its peak intensity as a Category 4 severe tropical cyclone with ten-minute sustained winds of 185 km/h (115 km/h) and a barometric pressure of 930 mbar (hPa; 27.46 inHg). [2] The JTWC assessed the storm to have attained similar one-minute sustained winds upon peaking; however, this was due to discrepancies between the two warning centers. [3] [6] At this time, Waka displayed a well-defined, circular eye roughly 60 km (37 mi) in diameter. Shortly after attaining its peak intensity, the center of Waka passed over Vava'u. [2]
Continuing into the new year, Waka gradually weakened on January 1, 2002, as it entered a less favorable region for tropical cyclones. As a result, wind shear displaced convection from the center and its eyewall broke apart. Moving over decreasing sea surface temperatures, Waka began to undergo an extratropical transition, which it completed on January 2. [2] Tracking southeastward, the remnant cyclone briefly slowed over open waters before again accelerating. Over the following few days, the system gradually weakened, with sustained winds decreasing below gale-force by January 5. The storm was last noted on January 6 near the Southern Ocean, about 2,200 km (1,400 mi) north-northwest of Antarctica, at which time it had a pressure of 972 mbar (972 hPa; 28.7 inHg). [7]
Precipitation | Storm | Location | Ref. | ||
---|---|---|---|---|---|
Rank | mm | in | |||
1 | 674.9 | 26.57 | Raja 1986 | Maopoopo, Futuna Island | [8] |
2 | 556.7 | 21.92 | Fran 1992 | Hihifo, Wallis Island | [8] |
3 | 291.2 | 11.46 | Val 1975 | Hihifo, Wallis Island | [8] |
4 | 220.6 | 8.69 | Hina 1997 | Maopoopo, Futuna Island | [8] |
5 | 186.0 | 7.32 | Evan 2012 | Futuna Island | [8] |
6 | 180.0 | 7.09 | Val 1980 | Maopoopo, Futuna Island | [8] |
7 | 171.6 | 6.76 | Keli 1997 | Hihifo, Wallis Island | [8] |
8 | 160.8 | 6.33 | Unnamed 1966 | Malaetoli, Wallis Island | [8] |
9 | 160.0 | 6.30 | Amos 2016 | Hihifo, Wallis Island | [9] |
10 | 119.0 | 4.69 | Waka 2001 | Hihifo, Wallis Island | [8] |
On December 30, just a day before Waka passed through Tonga, warnings were issued for numerous islands, including parts of Fiji and Samoa. Forecasts showed the storm passing directly over the low-lying Tongan capital of Nuku'alofa as a Category 3 cyclone. [10] Owing to warnings from local media, [11] all New Year's Eve celebrations were canceled as residents and tourists boarded up their homes. All airports in the region were shut down and ferry service was suspended. [12] Many residents on the small island of Niuafo'ou, about 35 km2 (14 sq mi) in size, evacuated to other islands prior to Waka's arrival. [13]
When the storm was moving through the islands of Tonga at peak strength, a few islands recorded hurricane-force winds; the city of Neiafu measured the strongest winds, peaking at 185 km/h (115 mph). In the southern islands, wind gusts up to 250 km/h (160 mph) affected isolated areas. In the Haʻapai islands, sustained winds reached 100 km/h (62 mph) and gusted to 140 km/h (87 mph). [14] Heavy rains also fell during Waka's passage, amounting to over 200 mm (7.9 in) in Haʻapai. [15]
Initial reports from Nukuʻalofa on December 31 indicated severe agricultural damage but few infrastructural losses. [16] Following the passage of Waka, communication with Niuas and Vava'u were lost. [17] According to local reports, high winds sandblasted Neiafu and downed nearly every tree. [18] Surveys by the Red Cross revealed that roughly 200 homes in the city were severely damaged or destroyed and those left standing lost their roofs. [19] Vava'u lost roughly 90% of its crops, including essential food crops such as taro, yams and bananas. In Ha'apai, one person died from cardiac arrest brought on by the storm. Fallen trees blocked numerous roads; power and water supplies were also interrupted to most residents. Severe damage also took place on Niuatoputapu where coastal homes were impacted by Waka's storm surge and several structures lost their roofs. [15] In one instance, a yacht was brought onshore by the surge and crashed into a restaurant, destroying both. [20]
According to damage surveys, 13 of the country's islands sustained damage; [21] 470 homes and 6 schools were destroyed and hundreds more damaged. [22] [23] Damage throughout Tonga amounted to 104.2 million paʻanga ($51.3 million USD). [24] [25] In addition to infrastructural and public damage, the environment sustained catastrophic losses on Tonga. The Insular Flying Fox (Pteropus tonganus), a native species of bat, suffered great losses from Waka. Compared to pre-cyclone population levels, 79.8% (±9.9%) of the species was killed across six islands. This was due to widespread destruction of their natural food source, which decreased by 85% (±11.8%) following Waka. Trees across Vava'u were completely defoliated, [21] although only 6.6% were killed, [1] leaving no food for the bats. The greatest decline in bats was on Utula'aina Island at 95.7%; A'a Island sustained a complete loss of food-bearing plants. Six months after the storm, the bat population in Vava'u was still only 20% of the pre-storm level. [21]
During the cyclone's formative stages, it brought significant winds and swells to Tokelau, resulting in localized flooding and crop damage. American Samoa also experienced heavy rains, amounting to 56.9 mm (2.24 in), and gusts up to 90 km/h (56 mph). [26] The winds downed a few trees and caused minor crop damage, with losses amounting to US$120,000. [27] Large swells affected the island for roughly a week as the storm developed and moved away from the region. [28] [29] Cyclone Waka also affected Wallis and Futuna, prompting tropical cyclone watches and warnings from December 28 to 31, and later impacted Niue, prompting warnings there from December 30 to January 1. [30] On Wallis Island, one home was destroyed and 50% of the banana crop was lost. [3] A maximum of 112 mm (4.4 in) of rain fell in Hihifo during the passage of Waka. [31] A wind gust of 126 km/h (78 mph) and swells up to 7 m (23 ft) were recorded in Wallis. Niue received more significant damage, experiencing a storm surge of up to 8 m (26 ft) and sea spray up to 100 m (330 ft) inland. Numerous fallen trees and power lines blocked roads and left southern areas of the island without power for roughly six hours. [3] Damage in Niue amounted to US$10,000. [26]
After moving through the Tongan islands, the remnants of Waka brought large swells, estimated up to 2.5 m (8.2 ft), to the North Island of New Zealand. Thousands of residents and tourists were in the region following the New Year's holiday. Meteorologists warned that the oceans would be increasingly dangerous and advised people not to venture into the water. Every lifeguard in Whangamatā, as well as former lifeguards, were called in to assist in keeping an estimated 8,000 people out of the water. [32] Although most people stayed within a designated swimming area, several rescues had to be made. [33] Rip currents also pulled 38 people out to sea in Mount Maunganui Main Beach; all were quickly rescued by lifeguards. [34]
Within a day of Cyclone Waka's passage in Tonga, the Government of New Zealand deployed an aircraft to survey the scale of damage and reestablish contact with the Tongan Islands. [18] This aircraft was sent in accordance with the FRANZ Agreement, enacted in 1992, which states that assets from one country would be used in relief operations. [35] On January 2, the head of Tonga's Disaster Office announced that they would likely need international assistance to recover from the storm. [36] Due to the substantial damage to agriculture, food shortages were expected to impact the region over the following months. [15] [37] By January 7, the Red Cross began sending supplies to Tonga. Hundreds of tents and tarpaulins were brought in by an Australian AC-130 to help with the recovery process. [38] On January 12, a New Zealand Lockheed C-130 Hercules carrying US$700,000 worth of supplies flew to the area to deliver aid. [39] An additional US$700,000 was given in relief funds to repair damage wrought by the storm. Of this, US$500,000 would be used to repair schools that were damaged or destroyed and the remaining US$200,000 would be used for emergency lighting, cooking and food supply recovery. [22] [40]
Further funds came from the United States Agency for International Development, which offered US$25,000 by mid-January. [41] [42] The French Polynesian assembly in Tahiti also provided US$770,000 worth of relief supplies and aid. [43] The main industry of Tonga, tourism, was devastated by the storm as no tourists were allowed to travel to the region for at least two weeks after Waka's passage. [44] The Government of Tonga requested a total of US$39.2 million in international aid, most of which was dedicated to rehabilitation of infrastructure. Medical supplies and personnel were later deployed by the World Health Organization. [45] In early March, a relief fund based on donations was set up by the United Methodist Committee on Relief to provide US$210,000 for 30 families impacted by the storm. [46] About 180 people were given assistance in rebuilding their homes by the Church World Service later that month. [47] As food shortages became severe in April, emergency supplies were sent to the outlying Niuas islands of Tonga. [37] In May, US$5.85 million was approved for emergency funds by the World Bank to assist in infrastructural rehabilitation. [48]
Vava'u suffered a tremendous decrease in agricultural exports due to Waka, dropping 86.5% from the previous year. [49] Despite substantial agricultural losses, the sector ended up expanding roughly 2% by the end of 2002 and the overall economy grew by 2.9%. [50] Owing to the severity of damage wrought by the cyclone, the World Meteorological Organization retired the name Waka following its using. [51]
Severe Tropical Cyclone Heta was a Category 5 tropical cyclone that caused moderate damage to the islands of Tonga, Niue, and American Samoa during late December 2003 and early January 2004. Heta formed on December 25, 2003; it reached a maximum intensity of 260 km/h (160 mph) and an estimated pressure of 915 hPa before dissipating on January 11, 2004. It was the first named tropical cyclone to form during the 2003–04 South Pacific cyclone season.
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 Daman was the strongest cyclone of the 2007–08 South Pacific cyclone season. Cyclone Daman was the fourth tropical depression and the first severe tropical cyclone to form east of longitude 180° during the 2007–08 South Pacific cyclone season. Due to the severity of the storm, the name Daman was retired and replaced with Denia.
The 2001–02 South Pacific cyclone season was a below-average year in which only five named storms formed or entered the South Pacific basin. It began on November 1, 2001, and ended on April 30, 2002. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season, and the "tropical cyclone year" runs from July 1, 2001, to June 30, 2002. The season's sixteen tropical depressions existed within these dates with the first developing on November 29 and the last dissipating on April 22.
Tropical Cyclone Urmil was a short lived storm of January 2006 that explosively intensified to reach its peak intensity as a high-end Category 2 cyclone on the Australian Scale, just 12 hours after being named. Forming out of a tropical disturbance early on January 14, Urmil quickly intensified before weakening just as quickly. The intensification was a result of the main convective banding feature wrapping around the center of circulation. However, the combination of high wind shear and the rapid movement of the cyclone caused convection to become separated from the center. By January 15, the storm transitioned into an extratropical cyclone shortly before dissipating. Urmil had only minor effects on land; scattered vegetation damage was reported in Tonga.
Tropical Cyclone Tam was the first named storm of the 2005–06 South Pacific cyclone season. Forming out of a tropical depression on January 6, the storm gradually intensified, becoming a tropical cyclone on January 12 and receiving the name Tam. Although it was traveling at a quick pace, the storm gained organization and reached its peak intensity with winds of 85 km/h (53 mph) the following day. However, the increasing forward motion of the storm, combined with strengthening wind shear, caused Tam to rapidly weaken on January 14. Around that time, it entered the Tropical Cyclone Warning Centre in Wellington, New Zealand's area of responsibility. Shortly thereafter, the storm transitioned into an extratropical cyclone and dissipated early the next day. Cyclone Tam produced heavy rainfall and strong winds over American Samoa upon being named. The precipitation caused several mudslides and flooding, which inflicted $26,000 in damage. The storm also had minor effects on Niue, Tonga, and Futuna.
The 2009–10 South Pacific cyclone season began on December 3, 2009 with the formation of Tropical Disturbance 01F, 32 days after the cyclone season had officially begun on November 1, 2009. The season ended on April 30, 2010. These dates conventionally delimit the period of each year when most tropical cyclones form in the southern Pacific Ocean east of 160°E. Additionally, the regional tropical cyclone operational plan defines a tropical cyclone year separately from a tropical cyclone season; the "tropical cyclone year" began on July 1, 2009 and ended on June 30, 2010. Tropical cyclones between 160°E and 120°W and north of 25°S are monitored by the Fiji Meteorological Service. Those that move south of 25°S are monitored by the Tropical Cyclone Warning Centre in Wellington, New Zealand. The first tropical disturbance of the season formed on December 3, about 1015 km (700 mi) to the north of Suva, Fiji and later intensified into Tropical Cyclone Mick. The last system, 15F, dissipated on April 5 of the following year.
The 1981–82 South Pacific cyclone season was a slightly-below average South Pacific tropical cyclone season, with 6 tropical cyclones occurring within the South Pacific Ocean basin between 160°E and 120°W during the season. After this season, the names Gyan and Isaac were retired from the lists of names, after they caused significant impacts to South Pacific island nations.
Tropical Cyclone Cilla was a tropical cyclone that brought minor damage to several islands in the South Pacific in January 2003. The fifth cyclone of the 2002–03 South Pacific cyclone season, Cyclone Cilla developed from a monsoon trough on January 26 northwest of Fiji. Initially, Cilla moved east, and due to decreased wind shear, Cilla was able to intensify. On January 28, Cilla reached its peak intensity of 75 km/h (45 mph). After slightly weakening, Cilla briefly re-intensified the next day. However, Cilla transitioned into an extratropical cyclone on January 30. Along its path, Cilla dropped heavy rainfall over islands it passed. During its formative stages, the low dropped heavy rain over Fiji, which had already been affected by Cyclone Ami two weeks prior. Damage in Tonga was mostly limited to vegetation and fruit trees; infrastructural damage was also relatively minor. Cilla also brought moderate rain to American Samoa.
Severe Tropical Cyclone Vaianu was the fourth named tropical cyclone of the 2005–06 South Pacific cyclone season. The system formed on February 11, and moved generally towards the south throughout its life. Vaianu ultimately peaked with winds corresponding to Category 1 status on the Saffir-Simpson Hurricane Scale, and passed between Fiji and Tonga. Moving into cooler waters, the storm dissipated on February 16. Although the cyclone avoided land for the most part, it caused heavy rainfall and gusty winds in portions of Tonga. Flooding hit the capital city of Nuku'alofa, and on some islands, the storm destroyed crops.
Severe Tropical Cyclone Wilma was a powerful tropical cyclone that affected the Samoan Islands, Tonga and New Zealand. Forming out of a trough of low pressure on 19 January 2011 to the northwest of Fiji, Cyclone Wilma initially tracked eastward towards the Samoan Islands. On 22 January, the system took a sharp southward turn, bringing its centre directly over American Samoa the following day. After turning towards the southwest and accelerating, Wilma steadily intensified into a severe tropical cyclone before striking Tonga. The storm reached its peak intensity on 26 January as a Category 4 cyclone with winds of 185 km/h (115 mph) and a barometric pressure of 930 mbar. Gradually re-curving towards the southeast, Wilma weakened quickly as it moved over cooler sea surface temperatures; by 28 January, it was downgraded to a tropical cyclone. Later that day, the storm brushed the North Island of New Zealand before transitioning into an extratropical cyclone.
Severe Tropical Cyclone Ami was one of the worst cyclones to affect Fiji. The system was the third cyclone and the second severe tropical cyclone of the 2002–03 South Pacific cyclone season. Cyclone Ami developed from a low-pressure area east of Tuvalu on January 12. Originally, the storm moved slowly towards the southwest early in its existence. Influenced by an upper-level trough, Ami slowed and began moving towards the south and then southeast. The cyclone attained severe tropical cyclone intensity on January 13. Ami made its first landfall at Vanua Levu, before subsequently making another landfall on Taveuni. Still intensifying, Ami reached peak intensity as a Category 3 cyclone on the Australian and Fiji cyclone scales on January 14. Accelerating to the southeast, the cyclone began to cross over cool sea surface temperatures and encountered wind shear. Ami transitioned into an extratropical cyclone the day after.
Severe Tropical Cyclone Ron was the strongest tropical cyclone on record to impact Tonga. The system was first noted as a tropical depression, to the northeast of Samoa on January 1, 1998. Over the next day the system gradually developed further and was named Ron as it developed into a Category 1 tropical cyclone on the Australian tropical cyclone intensity scale during the next day. The system subsequently continued to move south-westwards and became a Category 3 severe tropical cyclone, as it passed near Swains Island during January 3.
The 2019–20 South Pacific cyclone season was a slightly above-average season in which tropical cyclones formed within the South Pacific Ocean to the east of 160°E. The season officially ran from November 1, 2019, to April 30, 2020, however a tropical cyclone could form at any time between July 1, 2019, and June 30, 2020, and would count towards the season total. The season began on November 22 with the formation of Tropical Cyclone Rita, which would later become a severe tropical cyclone. The season has been near-average in terms of activity, with 8 tropical cyclones and 4 severe tropical cyclones forming during the season. The season featured Cyclone Harold, the first Category 5 severe tropical cyclone in the basin since Cyclone Gita, and one of the strongest since Cyclone Winston. During the season, tropical cyclones are officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BOM) and New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) also monitors the basin and issue unofficial warnings for American interests. The FMS attaches a number and an F suffix to tropical disturbances that form in or move into the basin while the JTWC designates significant tropical cyclones with a number and a P suffix. The FMS, BoM and MetService all use the Australian Tropical Cyclone Intensity Scale and estimate wind speeds over a period of ten minutes, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHWS).
Severe Tropical Cyclone Hina in March 1997 was the worst tropical cyclone to affect the South Pacific island nation of Tonga since Cyclone Isaac in 1982. The system was first noted within the monsoon trough on March 11, 1997, as a weak shallow depression within the vicinity of Rotuma. Over the next two days, the depression remained near Rotuma with no preferred movement, as it started to develop further within favorable conditions for further development. The system was subsequently named Hina on March 15, after it had started to move eastwards and had passed to the southeast of Niulakita, Tuvalu. During that day the system moved south-eastwards and impacted Wallis and Futuna, before it passed over Tonga's southern islands of Tongatapu and 'Eua during March 16. After impacting Tonga the system moved rapidly towards the south-southeast and weakened below tropical cyclone intensity, before it was last noted on March 21 about 1,500 km (930 mi) to the south of the Pitcairn Islands. During the system's post-analysis, it was determined that the warning centers had underestimated Hina's intensity as it passed over Tonga, after damage in the island nation had been greater than expected.
Severe Tropical Cyclone Ian was a powerful tropical cyclone that formed on January 2, 2014, and dissipated on January 15, 2014. Areas affected by the tropical cyclone include Fiji and Tonga. In Tonga, Ian caused destruction in the Ha'apai islands, as well as one fatality.
Severe Tropical Cyclone Ula was a powerful and long-lived tropical cyclone during late December 2015 and mid-January 2016. It originated from a tropical disturbance on December 26, 2015, east of the Solomon Islands. Moving generally east, development was initially slow and the system finally reached cyclone strength—having gale-force winds—on December 30. The newly christened Tropical Cyclone Ula turned sharply south and rapidly intensified, attaining hurricane strength the following day. A shift to the southwest brought the system close to the northern islands of Tonga on January 2, 2016. It subsequently brushed several islands in the Lau Group of Fiji before weakening. Nearly degrading to a tropical depression, Ula turned to the northwest and regained strength. After turning back to the southwest, it achieved its peak intensity as a Category 4 on the Australian scale with winds of 185 km/h (115 mph) on January 10. Thereafter, the storm bypassed Vanuatu to the southeast and New Caledonia to the east as it accelerated southward.
Severe Tropical Cyclone Gita was the most intense tropical cyclone to impact Tonga since reliable records began. The second named storm and first major tropical cyclone of the 2017–18 South Pacific cyclone season, Gita originated from a monsoon trough that was active in the South Pacific in early February 2018. First classified as a tropical disturbance on 3 February, the nascent system meandered near Vanuatu for several days with little development. After acquiring a steady east trajectory near Fiji, it organized into a Category 1 tropical cyclone on 9 February near Samoa. Arcing south in a clockwise turn, the system rapidly intensified, and became a severe tropical cyclone on 10 February near Niue.
Severe Tropical Cyclone Tino was a tropical cyclone which itself and an associated convergence zone caused significant damage across ten island nations in the South Pacific Ocean during January 2020. First noted as a tropical disturbance during January 11, to the southwest of Honiara in the Solomon Islands, the system gradually developed over the next few days as it moved eastwards in between the Solomon Islands and Vanuatu prior to being named Tino as it approached Fiji during January 16. Continuing to track south-eastward, Tino continued strengthening as it passed near Fiji, bringing copious amounts of rainfall to the area. Whilst losing latitude, the system continued to strengthen and peaked as a category 3 tropical cyclone on January 17, with signs of an eye forming. Shortly after peak intensity, Tino was impacted by high wind shear and decreasing sea surface temperatures, triggering a weakening trend. Tino moved out of the tropics shortly thereafter and became an extratropical cyclone during January 19.
Tropical Cyclone Sarai was a moderately strong tropical cyclone that impacted several island nations and countries in late-December 2019. The third tropical cyclone and the second named storm of the 2019-20 South Pacific cyclone season, Sarai formed from an area of low pressure to the south of Tuvalu. Over the next days, the low pressure became organized and was designated by the Fiji Meteorological Service as Tropical Disturbance 03F on December 23. Under favorable conditions, the disturbance gradually organized, becoming a depression two days later, before strengthening to a tropical cyclone, earning the name Sarai. It moved to the south, before a high-pressure steered the system to the east, passing to the south of Fiji, near Suva before weakening. Sarai passed near the Tongan islands of Haʻapai and Tongatapu as a Category 1 cyclone, before rapidly degrading to a tropical depression due to the system entering unfavorable conditions. It was last noted on January 2 to the southeast of Cook Islands.
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