Meteorological history | |
---|---|
Formed | 1 February 2012 |
Dissipated | 16 February 2012 |
Category 4 severe tropical cyclone | |
10-minute sustained (FMS) | |
Highest winds | 195 km/h (120 mph) |
Lowest pressure | 937 hPa (mbar);27.67 inHg |
Category 4-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 215 km/h (130 mph) |
Lowest pressure | 937 hPa (mbar);27.67 inHg |
Overall effects | |
Fatalities | None |
Areas affected | Cape York Peninsula,Solomon Islands,Vanuatu,New Caledonia,Tonga |
IBTrACS | |
Part of the 2011–12 Australian region and the South Pacific cyclone seasons |
Severe Tropical Cyclone Jasmine (RSMC Nadi designation:12F,JTWC designation:10P) 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.
The next day Jasmine entered an area of vertical wind shear,which consequently weakened the cyclone and caused its eye to expand. A high-pressure area south of Jasmine later steered the weakening cyclone to the northeast on 12 February. Although it entered an area of warmer sea surface temperatures,Jasmine subsequently entered extratropical transition and later degenerated into an extratropical cyclone on 16 February,and later dissipated completely on 19 February.
Cyclone Jasmine affected five countries during its existence. The predecessor to Jasmine brought heavy rainfall to areas of extreme northern Queensland. Jasmine also brought rainfall to areas of the Solomon Islands. As a result,pest infestations occurred across the region. In Vanuatu,heavy rains and wind from Jasmine destroy numerous crops. Banana trees in particular are affected by the cyclone. Jasmine inundated areas of Tonga that had already been affected by Cyclone Cyril just a week prior. Nuku'alofa recorded half of its average monthly rainfall in a 24‑hour span due to rains associated with the cyclone. After the season,the name Jasmine was retired from the Australian list of tropical cyclone names.
During 31 January the Australian Bureau of Meteorology started to monitor a tropical low, that had developed within the monsoon trough over the western Cape York Peninsula. [1] Over the next day the system moved into the southeastern part of the Gulf of Carpentaria, before it moved back over the Cape York Peninsula during 2 February. [1] [2] The system subsequently emerged into the Coral Sea to the north of Cairns later that day, where a strong northwest monsoon flow with gales developed to the north of the low. [2] The system subsequently moved eastwards and intensified into a category 1 tropical cyclone on the Australian tropical cyclone intensity scale.
On 1 February, the Australian Bureau of Meteorology's Brisbane tropical cyclone warning centre (TCWC Brisbane) and the United States Joint Typhoon Warning Center (JTWC) began to monitor a tropical low that had developed within a monsoon trough about 135 km (85 mi) to the north of Mornington Island. [2] [3] Over the next two days the low moved eastwards and passed over the Cape York Peninsula before it emerged into the Coral Sea to the north of Cairns. [1] After emerging into the Coral Sea the low continued to develop, and on 4 February, the JTWC and TCWC Brisbane reported that the system had become a tropical cyclone with the latter naming it as Jasmine while it was located about 420 km (260 mi) to the east of Cairns. [1] [4]
Tracking eastward, Jasmine entered a flow of dry air, which prevented the storm from strengthening quickly at the time. On 5 February, the low–level atmospheric circulation center of Jasmine became exposed due to the presence of strong vertical wind shear. However, the cyclone was able to maintain its intensity due to the existence of an area of moisture over Australia. Throughout the rest of the day, the wind shear subdued, and the system began to organize as convective banding wrapped around the center. As a result, Cyclone Jasmine intensified into the equivalent of a Category 2 on the Australian tropical cyclone intensity scale, with winds of 95 km/h (59 mph), sustained for 10 minutes. The next day, Cyclone Jasmine began to track to the east-southeast in response to a strengthening subtropical ridge. The cyclone continued to steadily intensify as convection continued to wrap tightly around the center of Jasmine. [5] At the same time, the storm moved out of the BOM's area of responsibility and into the area of responsibility of the Fiji Meteorological Service's (FMS) tropical cyclone warning center at Nadi, Fiji (RSMC Nadi). [6]
Late on 7 February, while still tracking to the east-southeast, Jasmine rapidly intensified, with wind speeds increasing to 185 km/h (115 mph), sustained for one minute. The cyclone developed a ragged eye stretching 40 km (25 mi) across. Later that day, Jasmine reached its peak intensity as it passed 280 km (170 mi) to the northeast of New Caledonia, with wind speeds of 215 km/h (134 mph), equivalent to a Category 4 cyclone on both the Australian and Saffir-Simpson hurricane scales (SSHS). Throughout 8 February, Jasmine began to show characteristics of an annular hurricane, maintaining a large, asymmetric eye and rather shallow convective features. In addition, multiple eyewall mesovortices developed within the eye. [5]
However, Jasmine did not maintain its peak intensity for an extended period of time. By 9 February, the cloud tops surrounding Jasmine began to warm, and thus weakened. In addition, the cyclone began to enter cooler SSTs. Although Jasmine's convective bands continued to thin out, the cyclone maintained a gradually expanding eyewall and remained a compact system. By 10 February, the eyewall of Cyclone Jasmine measured 95 km (59 mi) in diameter. The next day, the subtropical ridge that had been forcing Jasmine toward the southeast had weakened, and as a result the cyclone began to track east-northeast, toward a weakness in the ridge. The storm continued to disorganize, with its eye later becoming cloud–filled. By the end of 11 February, Jasmine had already weakened to a cyclone with wind speeds of just 85 km/h (53 mph), sustained for one minute, due to the presence of strong vertical wind shear. The low–level circulation center of Jasmine became partly exposed for a period of time on 12 February, before convection redeveloped over the center. As a weakening cyclone, Jasmine only maintained an area of weak convection displaced to its east as it approached Tonga. [5]
On 13 February, convection re-developed and later strengthened over Jasmine's center of circulation due to the presence of the South Pacific convergence zone and warm SSTs. Cyclone Jasmine was able to attain a secondary peak intensity of 85 km/h (53 mph), sustained for one minute, as the system's banding features became better defined. Due to Jasmine's position between two anticyclones, the cyclone erratically moved in a loop in the vicinity of Tonga from 14 to 15 February, before moving to the southeast. The system later exited the favorable conditions and moved into an area of strong wind shear once again. Convection became sheared apart and Jasmine's center of circulation once again became ill-defined and exposed. Late on 15 February, the JTWC issued their last advisory on the system, and on the next day, RSMC Nadi reported that Cyclone Jasmine had degenerated into an extratropical cyclone. [7]
During its existence, parts of Queensland, the Solomon Islands, Vanuatu, New Caledonia, Fiji and Tonga were affected by Cyclone Jasmine. The name Jasmine was retired from the Australian list of tropical cyclone names after the season by the World Meteorological Organization, and was replaced by the name Jenna. [8]
Early in its existence, Jasmine produced numerous rain showers over northern areas of Queensland. Gusty winds in Weipa, Queensland from Jasmine damaged trees on 2 February. A strong rainband associated with the cyclone produced heavy rainfalls over southern parts of Queensland. After Jasmine entered the Coral Sea, a surface trough extending from the cyclone produced rainfall over coastal areas of eastern Australia. [1] In Cairns, Queensland, several roads were closed due to severe weather associated with the cyclone, and trees were uprooted by strong winds. [9] Power lines in the northern suburbs of Cairns were also damaged due to strong winds. [10] Other areas of Queensland recorded rain totals in excess of 100 mm (3.9 in). [11]
Prior to Cyclone Jasmine, the Vanuatu National Disaster Management Office was preparing for the cyclone after the storm was forecast to impact the country. [12] The aid agency Oxfam prepared for food and water shortages, using the previous year's severe weather to gauge potential impacts from Cyclone Jasmine. [13] The Save the Children Fund prepared materials prior to the cyclone that could supply area schools with materials, known as a "school-in-a-box." [14] People in affected areas were evacuated to care centers prior to the storm. [15]
Within Vanuatu, gale-force winds caused damage to crops, houses and water systems. [16] Across the southern islands of Vanuatu, Jasmine impacted the area with winds of 165 km/h (103 mph). [13] Warnings for maritime activities including small craft warnings were issued for areas offshore the islands. [17] The cyclone produced rough seas at Port Vila, Vanuatu. [14] Damage associated with Jasmine was mostly of agricultural nature, primarily to crops and fruit trees. [15] Casava and banana crops were hampered by the storm, but did not pose any threat to food security. [18] Damage to infrastructure was reported in Tanna, though the island suffered from primarily losses to food crops. Areas that had traditions of not consuming severed crops were especially impacted by the damage to food crops. Water sources in southwest Tanna were destroyed, and other sources were contaminated from mud from runoffs. In addition, three classrooms at Enukas Primary School were destroyed by Jasmine. Aniwa Island also suffered from food damage, especially to banana and manioc crops, as well as orange trees. At Aniwa Airport, high frequency radio services were cut off. Futuna Island was also cut off due to loss of communication. At Dillon's Bay, one of Erromango's primary water sources, water became contaminated. [19] In addition, several air strips were closed due to water logging and debris. [15] An aerial and ground damage survey began in the southern areas of the island chain after cyclone effects had subsided. [20]
Jasmine caused intense rain showers across the island chain. The Solomon Islands Meteorological Service (SIMS) issued a Tropical Cyclone Watch Advisory throughout the day for affected areas. Isabel Province reported damage to kumara vines after three days of rain from the cyclone. Pest infestations also resulted from the rains. Most of the damage in the province resulted from overflowing rivers and inundated gardens. Makira-Ulawa Province also suffered from damaged food gardens. Cocoa bean, coconut, nut, and banana crops and plantations were damaged. In addition, bridges were washed out by flooding. The ship MV Haourosi was grounded in Maro’u Bay due to high waves offshore. [21]
Jasmine brought heavy rains and flooding to Tonga, which had already been impacted by heavy rains from Cyclone Cyril just a week prior. [22] Power outages occurred across Tonga due to the storm, but power was quickly restored. [23] International and domestic flights in Tonga were disrupted for two days due to Jasmine. [22] Tongatapu suffered from severe flooding. Affected families were sent to evacuation shelters. [24] Some houses reportedly collapsed and fell into creeks due to the flooding. [23] In Nuku'alofa, a total of 400 people were evacuated. [25] In a 24–hour period extending from 14 February to 15 February, 120 mm (4.7 in) of rain was recorded in Nuku'alofa, equal to more than half of the city's average recorded rainfall in the month of February. [26] On Atata Island, a resort was closed for two weeks due to damage sustained from the storm. [22] An offshore South Korean fishing boat sunk during the storm. However, its three crew members were rescued by Tongan police. [25] An additional two fishing boats broke away from Nuku'alofa Harbor and washed up on a nearby reef. [26] The Tongan Ministry of Health monitored the potential for diseases after the storm, particularly in low–lying areas of the island chain, where septic leakage was a potential health threat. [23]
The 2007–08 South Pacific cyclone season was one of the least active South Pacific tropical cyclone seasons on record, with only four tropical cyclones occurring within the South Pacific basin to the east of 160°E. The season officially ran from November 1, 2007, until April 30, 2008, although the first cyclone, Tropical Depression 01F, developed on October 17. The most intense tropical cyclone of the season was Severe Tropical Cyclone Daman, which reached a minimum pressure of 925 hPa (27.32 inHg) as it affected Fiji. After the season had ended, the names Daman, Funa, and Gene were retired from the tropical cyclone naming lists.
The 2006–07 South Pacific cyclone season was an event in the annual cycle of tropical cyclone formation. It began on November 1, 2006 and ended on April 30, 2007. 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, 2006 to June 30, 2007.
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.
The 2004–05 South Pacific cyclone season was an 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, 2004 to April 30, 2005, however a tropical cyclone could form at any time between July 1, 2004 and June 30, 2005 and would count towards the season total. The season got off to an early start, when Tropical Depression 01F developed near the Solomon Islands on October 28, three days before the official start of the season. The final disturbance of the season dissipated as the season was drawing to a close on May 1. The season was above-average in terms of activity, with 9 tropical cyclones and 5 severe tropical cyclones forming during the season. The season featured Cyclone Percy, the most intense of the season in terms of pressure.
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.
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.
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.
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.
The 2010–11 South Pacific cyclone season was an average tropical cyclone season, with seven tropical cyclones and five severe tropical cyclones developing during the season. The season ran from November 1, 2010 until April 30, 2011, though if any tropical cyclones had developed between July 1, 2010 and June 30, 2011, the official tropical cyclone year, they would have been counted towards the season's total. Within the South Pacific basin tropical cyclones were officially monitored by the Fiji Meteorological Service's Regional Specialized Meteorological Center in Nadi, Fiji, north of 25°S, and to the south the Meteorological Service of New Zealand's Tropical Cyclone Warning Center in Wellington, New Zealand. Any disturbances forming in the region were designated with a sequential number suffixed by the letter F. In addition, the United States Military's Joint Typhoon Warning Center unofficially monitored parts of the basin during the season, where any systems judged to have achieved tropical storm strength or greater received a number suffixed with the letter P. RSMC Nadi and TCWC Wellington both use the Australian Tropical Cyclone Intensity Scale, and measure wind speeds over a period of ten minutes, while the JTWC measures sustained winds over a period of one minute which can be applied to the Saffir–Simpson hurricane scale. Seven named storms formed or moved into the South Pacific basin during the 2010–11 season, the strongest of which was Severe Tropical Cyclone Wilma in late January.
The 2011–12 South Pacific cyclone season was one of the least active South Pacific tropical cyclone seasons on record, with only three tropical cyclones occurring during the season. The season ran from November 1, 2011, to April 30, 2012, however, any tropical cyclones that form before June 30, 2012, would have fallen within the 2011–12 tropical cyclone year and would have counted towards the season total. The strongest and only severe tropical cyclone that occurred during the season was Severe Tropical Cyclone Jasmine, which tracked in from out of the South Pacific basin. Within the basin, tropical cyclones are monitored by the Regional Specialized Meteorological Center (RSMC) in Nadi, Fiji, and the Tropical Cyclone Warning Center (TCWC) in Wellington, New Zealand. RSMC Nadi attaches an F designation to tropical disturbances that form in or move into the South Pacific. The United States Joint Typhoon Warning Center (JTWC) issues unofficial warnings within the South Pacific, designating tropical storm-equivalent or greater tropical cyclones with a number and a P suffix. RSMC Nadi and TCWC Wellington both use the Australian Tropical Cyclone Intensity Scale, and measure windspeeds over a period of ten minutes, while the JTWC measures sustained winds over a period of one minute and uses the Saffir–Simpson hurricane scale.
Tropical Cyclone Trina was a weak but destructive tropical cyclone in late 2001 which caused some of the worst flooding in the South Pacific island of Mangaia, Cook Islands, in nearly 50 years. Forming out of an upper-level low pressure system on November 29 near the island of Rarotonga, or roughly 1,470 mi (2,365 km) southeast of Fiji, Trina remained practically stationary as it meandered in the same general area for over a week. Due to unfavorable conditions for tropical cyclogenesis, the storm struggled to develop significant convection, preventing it from intensifying beyond 65 km/h (40 mph). After finally succumbing to wind shear on December 2, the system weakened to a tropical depression near Mangaia and dissipated several days later.
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 an equivalent 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 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 Paula was a tropical cyclone which caused extensive damage to areas of Vanuatu. The cyclone was the second cyclone and only severe tropical cyclone of the relatively inactive 2000–01 South Pacific cyclone season. Cyclone Paula developed from an area of disturbed weather embedded within a monsoon trough on February 25, 2001, near Vanuatu. Situated in an area of favorable conditions, Paula steadily intensified as it moved in a general direction towards the southeast. On March 1, Paula reached peak intensity with winds of 175 km/h (109 mph), sustained for ten minutes. However, the cyclone began to accelerate further to the southeast into more unfavorable conditions. As a result, Paula quickly weakened, and thus degenerated into an extratropical cyclone on March 4.
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 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.
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 Harold was a very powerful tropical cyclone which caused widespread destruction in the Solomon Islands, Vanuatu, Fiji, and Tonga during April 2020. It was the first Category 5 tropical cyclone in 2020. The seventh named storm of the 2019–20 Australian region cyclone season, eighth named storm, and fourth severe tropical cyclone of the 2019–20 South Pacific cyclone season, Harold was first noted as a developing tropical low within a trough of low pressure during April 1, while it was located to the east of Papua New Guinea. Over the next day, the system moved south-eastwards over the Solomon Sea, before it was classified as a tropical cyclone and named Harold by the Australian Bureau of Meteorology. The system moved into the Fiji Meteorological Service's area of responsibility on April 2 and began to explosively intensify by April 3, reaching Category 4 status by April 4 on both scales. The next day, it further strengthened into a Category 5 severe tropical cyclone, the highest rating on the Australian scale. It made landfall on Espiritu Santo on April 6 and the next day, strengthening to its peak intensity, attaining Category 5-equivalent intensity on the Saffir–Simpson scale before making landfall on Pentecost Island. Moving east, it weakened below Category 5 intensity on both scales over subsequent days. It regained Category 5 severe tropical cyclone status while passing south of Fiji, before weakening and becoming extratropical on April 9.