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Tropical cyclones in Fiji

This list has 42 members. See also Natural disasters in Fiji, Tropical cyclones by country, Tropical cyclones in Oceania by country
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  • Cyclone Kina
    Cyclone Kina South Pacific tropical cyclone in 1992–93
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    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.
  • Cyclone Susan
    Cyclone Susan Category 5 South Pacific cyclone in 1997 and 1998
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    Severe Tropical Cyclone Susan was a powerful tropical cyclone that is one of the most intense on record within the South Pacific basin. It was first noted on December 20, 1997, as a weak tropical disturbance located to the north of American Samoa. Over the next 12 days, the disturbance remained weak while it gradually moved towards the southwest before it started to rapidly develop on January 2, 1998 while it was located near the Fijian dependency of Rotuma. The disturbance was declared a tropical cyclone later that day, but was not named Susan until the next day, after it had intensified into a category 2 tropical cyclone on the Australian Scale. Over the next few days, Susan moved towards the southwest and continued to intensify before it reached its peak intensity as a category five tropical cyclone during January 5 while it was located about 400 km (250 mi) to the northwest of Vanuatu's capital city Port Vila.
  • Cyclone Ami
    Cyclone Ami Category 3 South Pacific cyclone in 2003
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    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.
  • Cyclone Zoe
    Cyclone Zoe 2002 tropical cyclone
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    Severe Tropical Cyclone Zoe was the second-most intense tropical cyclone on record within the Southern Hemisphere and was the strongest tropical cyclone worldwide in 2002. The system was first noted on December 23, 2002, as a tropical depression that had developed, within the South Pacific Convergence Zone to the east of Tuvalu. Over the next couple of days, the system moved southwestwards and crossed the International Dateline early on December 25. After this, the system became better organized and was declared to be a tropical cyclone and named Zoe later that day. Zoe subsequently rapidly intensified in very favorable conditions as it continued to move west-southwest towards the Solomon Islands. The system subsequently became a Category 5 tropical cyclone on both the Australian tropical cyclone intensity scale and the Saffir-Simpson hurricane wind scale on December 27. The system subsequently affected the Solomon Islands Temotu Province during that day, before it peaked with 10-minute sustained wind speeds of 240 km/h (150 mph). As the system peaked, it performed a small clockwise cyclonic loop within the vicinity of Tikopia island, as a result of the steering flow over the cyclone becoming weak and variable. The system subsequently started to move towards the southeast during December 29, in response to a strengthening steering flow, provided by an upper level trough of low pressure and a baroclinic system near New Caledonia. Over the next few days the system weakened and degenerated into a tropical depression during January 1, 2003. The system was subsequently last noted during January 4, while it was located to the southeast of New Caledonia.
  • Cyclones Judy and Kevin
    Cyclones Judy and Kevin two tropical cyclones brought impacts in Vanuatu and other regions
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    Severe Tropical Cyclones Judy and Kevin were a pair of intense tropical cyclones that made landfall on the Pacific island nation of Vanuatu within 48 hours of each other in March 2023. They were the fourth and fifth named storms of the 2022–23 South Pacific cyclone season respectively, as well as the second and third severe tropical cyclones of the season. By the end of February, Judy had affected the Solomon Islands, and shortly after, Kevin began to affect the country.
  • Cyclone Tino
    Cyclone Tino 2020 South Pacific cyclone
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    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.
  • January 2009 Fiji floods
    January 2009 Fiji floods South Pacific tropical depression in 2009
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    During January 2009, Fiji was impacted by a series of consecutive weather events, that caused severe flooding in various parts of the island nation. The floods were caused by a number of intense synoptic-scale weather features, which included an active monsoonal trough, the South Pacific Convergence Zone, Tropical Depression's 04F and 05F as well as Tropical Cyclone Hettie. These weather features combined to cause strong winds, considerable rainfall, as well as severe flooding across the island nation throughout the month.
  • Cyclone Cody
    Cyclone Cody category 3 tropical cyclone in 2022
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    Severe Tropical Cyclone Cody was a strong tropical cyclone in the South Pacific which caused widespread damage in Fiji. The second tropical cyclone and first severe tropical cyclone of the 2021–22 South Pacific cyclone season, Cody was first noted by the Fiji Meteorological Service (FMS) on 5 January as Tropical Disturbance 03F. The tropical depression killed one person, and over 4,500 people were evacuated. On 10 January, the system was upgraded to a Category 1 tropical cyclone by the FMS, receiving the name Cody. While the FMS recorded a peak intensity of 130 km/h (80 mph), the Joint Typhoon Warning Center (JTWC) only recorded a peak intensity of 95 km/h (60 mph). Cody was the first tropical cyclone in 2022.
  • Cyclone Harold
    Cyclone Harold Category 5 tropical cyclone in 2020, affecting Vanuatu and several other Oceanic countries
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    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 (on the Australian scale only) while passing south of Fiji, before weakening and becoming extratropical on April 9.
  • Cyclone Nigel
    Cyclone Nigel Category 3 tropical cyclone in 1985
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    Severe Tropical Cyclone Nigel was the second of two tropical cyclones to affect Northern Vanuatu and the Fijian islands during January 1985. The system was first noted as an ill-defined low-pressure area ("low") located within the Intertropical Convergence Zone near the Cape York Peninsula. Over the next few days the low moved eastwards and increased in strength; it was named Nigel on January 16 as it developed into a tropical cyclone.
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