Meteorological history | |
---|---|
Formed | November 20, 1990 |
Extratropical | December 1,1990 |
Dissipated | December 4, 1990 |
Category 3 severe tropical cyclone | |
10-minute sustained (FMS) | |
Highest winds | 140 km/h (85 mph) |
Lowest pressure | 960 hPa (mbar);28.35 inHg |
Category 4-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 230 km/h (145 mph) |
Overall effects | |
Fatalities | None |
Damage | $18.5 million (1990 USD) |
Areas affected | Fiji,Tonga,Niue,Southern Cook Islands |
IBTrACS | |
Part of the 1990–91 South Pacific cyclone season |
Severe Tropical Cyclone Sina was the only named tropical cyclone to develop within the South Pacific basin during the 1990–91 season. The system was first noted as a shallow depression within the South Pacific Convergence Zone to the west of Wallis Island. Over the next three days the system moved towards the west-northwest,before it was named Sina during November 24,after it had developed into a tropical cyclone. Over the next couple of days the system intensified further and developed an eye feature as it erratically moved towards Fiji. Sina subsequently peaked in intensity during November 26,before the system passed through the Fijian Islands over the next two days as it started to gradually weaken. Sina subsequently passed just to the north of Tongatapu in Tonga during November 29,before it passed about 160 km (100 mi) to the south of Niue and near the Southern Cook Islands during the next day. The system subsequently rapidly weakened and became an extratropical cyclone during December 1,before they were absorbed by an advancing trough of low pressure near 50°S on December 4.
The cyclone caused no deaths and over $18.5 million in damages,as it affected Fiji,Tonga,Niue and the Southern Cook Islands. Ahead of the system affecting Fiji,hundreds of people were evacuated from Fiji's outer island resorts to hotels on the mainland. High winds and heavy rain forced the closure of several local airports and the main Nadi International Airport. As Sina moved through the archipelago,the system destroyed or damaged houses and other building structures,while bringing down electric and telephone lines and uprooting trees. The system also washed away a railway bridge on Vanua Levu that was used to take sugar cane to Labasa's mills,leaving growers no choice but to go through the village of Korowiri. However,the workers refused to go into their fields unless they had police protection to go through the village,after Methodists from the local church attacked a group of growers for working on Sundays in defiance of Fiji's Sunday Observance Decree. Within Tonga only minor damage to weak structures,trees,banana plantations,electric and telephone lines was recorded. Within both Niue and the Southern Cook Islands only minor damage to crops and structures was reported.
On November 20, the Fiji Meteorological Service (FMS) started to monitor a shallow tropical depression that had developed within the South Pacific Convergence Zone to the west of Wallis Island. [1] [2] Over the next two days the system moved towards the west-northwest and the Fijian dependency of Rotuma, before the depression's chances of developing further became good during November 23, as upper outflow over the system became established. [1] [2] The United States Joint Typhoon Warning Center (JTWC) subsequently initiated advisories and classified the depression as Tropical Cyclone 03P at 1200 UTC the next day, after atmospheric convection surrounding the system organized further. [1] [3] Later that day, the FMS named the system Sina after the depression had developed into a category 1 tropical cyclone on the Australian tropical cyclone intensity scale, while it was located about 425 km (265 mi) to the northwest of Rotuma. [1] [4] During November 25, the cyclone continued to intensify and developed an eye as it moved erratically towards the west-southwest and performed a small clockwise loop. Early on November 26, the FMS reported that Sina had become a category 3 severe tropical cyclone. [1] [4] At around this time, the JTWC reported that Sina had become equivalent to a category 1 hurricane on the Saffir-Simpson hurricane wind scale (SSHWS). [4]
During that day, Sina's eye became very distinct on satellite imagery. [1] As the system intensified and came under the influence of a changeable upper level steering flow which resulted in Sina moving erratically towards the southeast and Fiji. [1] Later that day the FMS reported that the system had peaked as a category 3 severe tropical cyclone, with 10-minute sustained windspeeds of 75 kn (140 km/h; 85 mph). [4] [5] The JTWC subsequently reported early the next day that Sina had peaked with 1-minute sustained wind speeds of 125 kn (230 km/h; 145 mph), which made it equivalent to a category 4 hurricane on the SSHWS. [4] During that day, Sina remained at its peak intensity as it moved towards the east-southeast and started to be observed on the Nadi radar. [1] [4] Later that day, as the system started to gradually weaken, it passed about 40 km (25 mi) to the south of Viti Levu before it passed over the island groups of Vatulele and Moala and the Southern Lau Islands during November 28. [1] During that day the system moved across the 180th meridian, which prompted the JTWC to issue their final warning on Sina and pass the responsibility for warning the United States Government to the Naval Western Oceanography Center. [3] [4]
Early on November 29, Sina weakened into a category two tropical cyclone on the Australian scale just before it passed to the north of Tongatapu in Tonga. [1] [4] During that day, as the system moved eastwards towards the Southern Cook Islands and gradually weakened further, the NWOC issued their final advisory on Sina while estimating that it was equivalent to a category one hurricane on the SSHWS. [3] [4] Early on November 30, the system passed about 160 km (100 mi) to the south of Niue, before it recurved sharply towards the south-southeast later that day as it approached the Southern Cook Islands. The system subsequently started to rapidly weaken under the influence of strong vertical wind shear and cooler sea surface temperatures. [1] The FMS subsequently passed the primary warning responsibility for Sina to the New Zealand Meteorological Service as it crossed 25°S, who quickly reported that the system had lost its tropical characteristics and had become an extratropical depression. [6] [1] Over the next couple of days, Sina's extratropical remnants maintained a south-eastward track, before it was absorbed by an advancing trough of low pressure near 50°S on December 4. [6]
Cyclone Sina affected Fiji, Tonga, Niue, and the Southern Cook Islands and was responsible for damages totaling over $18.5 million. [1] The system had initially appeared to threaten the Solomon Islands and Vanuatu as it performed a small clockwise loop and moved erratically towards the west-southwest during November 25. [1] After this usage of the name, Sina was retired from the tropical cyclone naming lists for the region. [7]
Late on November 25, the FMS issued a tropical cyclone alert for Fiji, while the system was located about 665 km (415 mi) to the northwest of the country. [1] During the next day, a gale-force wind warning was issued for the western half of Viti Levu, the Yasawa and Mamanuca island groups, which was later upgraded to a storm warning while a gale warning was also issued for the rest of Viti Levu. [1] These storm warnings were briefly dropped early on November 27, when the storm appeared to be moving away from the country, but as Sina came within range of the Nadi radar, it became apparent that southern Fiji would be directly hit by the system. [1] As a result, hurricane warnings were issued for Vatulele, Kadavu and smaller nearby islands, while storm warnings were re-issued for the western half of Viti Levu and the Mamanuca island group. [1] Over the next day as the cyclone approached, hurricane, storm and gale warnings were revised to cover various islands within the Koro and Southern Lau island groups, before all warnings were cancelled on November 28, as Sina moved away from Fiji. [1]
Ahead of Sina affecting the Fijian islands, from November 27 until November 29, with wind gusts of up to 175 km/h (110 mph), hundreds of people were evacuated from Fiji's outer island resorts to hotels on the mainland. [5] [8] [9] [10] As the cyclone affected Fiji high winds and heavy rain forced the closure of several local airports and the Nadi International Airport for around 20 hours. [9] [11] [12] [13] As the cyclone moved towards the east-southeast between November 27–28, it passed near to or over the south-western coast of Viti Levu, Vatulele, Bequa, Northern Kadavu and various islands within the Moala and Southern Lau island groups and caused some coastal erosion. [1] [14] As it moved through the archipelago, the system destroyed or damaged houses and other building structures, while bringing down electric and telephone lines and uprooting trees. [1] [5] The system also severely affected crops and vegetation including sugar cane and pine forests, however the extent of the damage was limited by the fact that many of the crops had already been harvested. [1] [15]
On December 7, the Australian Government via the international development bureau and Air Pacific provided emergency shelter materials, including tarpaulins, plastic sheeting and rope, after an appeal for international assistance was made by the Fijian government. [16] [17] After the cyclone damaged resorts were quickly repaired, while the Fijian government launched an international advertisement campaign for the islands with discounted airfares. [15] Overall Sina caused over $F26 million ($US18.5 million) worth of damage to the Fijian islands, with most of the damage accounted for by losses to agriculture, sugar cane, and pine forests. [6] [1] After Cyclone Sina had washed away a railway bridge on Vanua Levu that was used to take sugar cane to Labasa's mills, growers had no choice but to go through the village of Korowiri. [18] However, the workers refused to go into their fields unless they had police protection to go through the village, after Methodists from the local church attacked a group of growers for working on Sundays in defiance of Fiji's Sunday Observance Decree. [18] As a result, sugar cane that had been damaged by Sina was left rotting in Fiji's fields until the Fiji Sugar Corporation ordered that a temporary bridge be built to bypass the village. [18]
Late on November 27, as Sina affected the Fijian island of Viti Levu, a tropical cyclone alert was issued by the FMS, for the Tongatapu, Haʻapai and Vavaʻu groups of islands. [1] [19] During the next day the tropical cyclone alert for Vavaʻu was cancelled, while gale and storm force wind warnings were issued for the island groups of Haʻapai and the Tongatapu. [1] The system subsequently moved in between the Tongatapu and Haʻapai groups of islands where sustained windspeeds of up to 96 km/h (60 mph) and wind gusts of up to 139 km/h (86 mph) were recorded at the Nukuʻalofa weather station. [1] Parts of the Tongan capital city Nuku'alofa were left without power, after electric lines were brought down, while several homes were partially damaged after the roofs lost their iron. [20] Overall only minor damage to weak structures, trees, banana plantations, electric and telephone lines was recorded within the island nation. [1]
During November 29, strong wind warnings were issued for Niue as the island experienced marginal gale-force winds from the system, as it passed about 185 km (115 mi) to the south of the island. [1] [21] High seas salt spray and waves caused some damage to crops and the island's wharf. They also washed away two temporary roads that were installed after Cyclone Ofa had affected the island earlier in the year. [1] [22]
Early on November 30, as the system moved towards the east-southeast, a gale warning was issued for the Cook Islands of Rarotonga and Mangaia, while issuing strong wind warnings and tropical cyclone alerts for the rest of the Southern Islands. [1] [21] The warnings were subsequently maintained until later that day, as Sina spared the Cook Islands its major effects and re-curved sharply towards the south-southeast. [1] Only minor damage to shallow rooted crops and weak structures was reported, after high seas and gale-force winds buffeted the northern side of Rarotonga. [1] [23]
The 2005–06 South Pacific cyclone season was an event in the annual cycle of tropical cyclone formation. It began on November 1, 2005, and ended on April 30, 2006. 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, 2005, to June 30, 2006.
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 2008–09 South Pacific cyclone season was a below average tropical cyclone season, which featured six named tropical cyclones compared to an average of about nine. Ahead of the season officially starting on November 1, 2008, the Island Climate Update tropical cyclone outlook predicted that the season, would feature an average risk of tropical cyclones impacting the South Pacific between 160°E and 120°W. The first tropical disturbance of the season developed to the northeast of the Samoan Islands on December 1, however, it remained weak and was last noted during the next day.
Tropical Cyclone Cliff was first noted as a weak tropical disturbance on April 1, 2007, within a trough of low pressure about 210 km (130 mi) to the southwest of Rotuma. Over the next couple of days the system drifted towards the southeast and Fiji, in an area of strong wind shear. During April 3, the system slightly accelerated, as it moved towards the south-southeast before the westerly wind shear around the system relaxed sufficiently to allow the depression to consolidate while it was located near Vanua Levu.
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 1992–93 South Pacific cyclone season was an above-average tropical cyclone season with ten tropical cyclones occurring within the South Pacific to the east of 160°E. The season officially ran from November 1, 1992, to April 30, 1993, with the first disturbance of the season forming on December 3 and the last disturbance dissipating on April 6.
The 1996–97 South Pacific cyclone season was one of the most active and longest South Pacific tropical cyclone seasons on record, with 12 tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. The season officially ran from November 1, 1996 - April 30, 1997, however, the season ended later than normal with three systems monitored after the official end of the season. The strongest tropical cyclone of the season was Cyclone Gavin which had a minimum pressure of 925 hPa (27.32 inHg). After the season had ended 4 tropical cyclone names were retired from the naming lists, after the cyclones had caused significant impacts to South Pacific islands.
The 1990–91 South Pacific cyclone season was one of the least active tropical cyclone seasons on record, with only two tropical cyclones occurring within the South Pacific basin to the east of 160°E. The season officially ran from November 1, 1990 to April 30, 1991, with the first disturbance of the season forming on November 23, 1990, while the final disturbance dissipated on May 19, 1991. During the season there were no deaths recorded from any of the tropical cyclones while they were within the basin. However, six people were killed by Cyclone Joy, when it made landfall on Australia. As a result of the impacts caused by Joy and Sina, the names were retired from the tropical cyclone naming lists.
The 1989–90 South Pacific cyclone season was a below-average season with only five tropical cyclones occurring within the South Pacific to the east of 160°E. The season officially ran from November 1, 1989, to April 30, 1990, with the first disturbance of the season forming on November 8 and the last disturbance dissipating on March 19. This is the period of the year when most tropical cyclones form within the South Pacific Ocean.
The 1982–83 South Pacific cyclone season was one of the most active and longest South Pacific tropical cyclone seasons on record, with 16 tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. During the season tropical cyclones were monitored by the meteorological services of Australia, Fiji, French Polynesia and New Zealand. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) and Naval Pacific Meteorology and Oceanography Center (NPMOC), also monitored the basin and issued unofficial warnings for American interests. The first tropical cyclone of the season developed a day before the season officially began on October 30, while the last tropical cyclone of the season dissipated on May 16. Most of the activity during the season occurred within the central and eastern parts of the basin with French Polynesia affected by several systems.
Severe Tropical Cyclone Joni was a damaging tropical cyclone that impacted the island nations of Tuvalu and Fiji. It was first noted within the South Pacific Convergence Zone at the start of December 1992, as a shallow tropical depression in the vicinity of the island nation Tuvalu. Over the next few days the system gradually developed further as it affected Tuvalu, before it was declared to be a tropical cyclone and named Joni by the Fiji Meteorological Service (FMS) during December 7. Over the next couple of days the system intensified further as it was steered south-westwards and posed a threat towards the Fijian dependency of Rotuma and the French territory of Wallis and Futuna. The system subsequently peaked as a Category 4 severe tropical cyclone on the Australian tropical cyclone intensity scale as it approached the Fijian Islands during December 10. Over the next couple of days the system moved through the Fijian Islands, before it became an extratropical cyclone during December 13. The system was last noted during the next day as it was absorbed by a mid-latitude trough of low pressure to the east of New Zealand.
Severe Tropical Cyclone Kina was at the time the costliest storm to impact Fiji on record. Total losses from Kina are estimated to be near $F170 million ($US110 million). The system was first noted as a tropical depression, to the east of the Solomon Islands on 23 December. Over the next few days the system moved south-eastwards and gradually developed further, before it was named Kina, after it had developed into a tropical cyclone on 26 December.
Severe Tropical Cyclone Ofa was a powerful tropical cyclone that caused severe damage in Polynesia in February 1990. The system was first noted on January 27, 1990, near Tuvalu, as a shallow tropical depression that had developed within the South Pacific Convergence Zone. The cloud pattern slowly organized, and on January 31, while located east of Tuvalu, Ofa attained cyclone intensity. Moving slowly southeast, Ofa developed storm-force winds. It attained hurricane-force winds on February 2. Cyclone Ofa reached peak intensity on February 4. Shortly after, its peak Ofa began to weaken over a less favourable environment. Ofa was declared an extratropical cyclone on February 8, though the system was still tracked by meteorologists until February 10.
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 peaked 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 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.
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.
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.
The following is a list of all reported tropical cyclones within the South Pacific Ocean to the east of 160°E during the 1950s decade.
Severe Tropical Cyclone Ana was one of three tropical cyclones to impact the island nation of Fiji towards the end of January 2021. The fifth tropical disturbance, third tropical cyclone and second severe tropical cyclone of the 2020–21 South Pacific cyclone season, Ana was first noted as Tropical Disturbance 05F during January 26, while it was located about 220 km (135 mi) to the northeast of Port Vila in Vanuatu. Over the next few days, the system moved eastwards and gradually developed further, before it was declared to be a tropical cyclone and named Ana during January 29. Over the next day, the system moved south-eastwards towards Fiji before it made landfall on the island of Viti Levu. After emerging into the Pacific Ocean, the system intensified into a Category 3 severe tropical cyclone, before it rapidly degenerated into a subtropical low during February 1.
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.