Cyclone Ian

Last updated
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

During January 2, 2014 the Fiji Meteorological Service's Regional Specialized Meteorological Center in Nadi, Fiji (RSMC Nadi) reported that Tropical Disturbance 07F had developed to the southeast of Futuna Island. [1] Over the next day the system gradually developed further underneath an upper level ridge of high pressure, within an area of moderate vertical wind shear, as it slowly moved towards the southwest. [1] [2] RSMC Nadi subsequently classified the disturbance as a tropical depression early on January 4, as the systems low level circulation center consolidated. [3] [4] Over the next day the system continued to move towards the southwest, before the United States Joint Typhoon Warning Center designated the system as Tropical Cyclone 07P late on January 5. [5] At around this time RSMC Nadi named the system Ian, after it had become a category 1 tropical cyclone on the Australian tropical cyclone intensity scale. [6]

Early on January 8, RSMC Nadi reported that Ian had become a category two tropical cyclone. [7] During that day the systems organization significantly improved with RSMC Nadi reporting at 1800 UTC that Ian had become a category three severe tropical cyclone. [8] Over the next day the system developed a cloud filled eye and intensified into a category 4 severe tropical cyclone. On January 12, as Ian started to weaken RSMC Nadi handed the primary warning responsibility, for issuing warnings over to the Wellington Tropical Cyclone Warning Center.[ citation needed ]

Preparations and impact

Cyclone Ian intensifying off Tonga on January 6 Ian Jan 06 2014 0125Z.jpg
Cyclone Ian intensifying off Tonga on January 6

Late on January 10, a state of emergency was declared by Tongan Prime Minister Lord Tu'ivakano, after Ian intensified into a category five severe tropical cyclone [9] with 287 km/h winds. It struck the Ha'apai islands the next day between Tongatapu and Vava'u, according to the Director of Emergencies Leveni Aho. He also said that 23 islands that are a part of Ha'apai were unreachable by telephone and that patrol boats were traveling from island-to-island to get information. As a result of the cyclone, homes were flattened and at least one person was dead. Ha'apai governor Tu'i Ha'angana said that he was able to see from one side of the island to the other and "that's how devastated it is." [10] By 13 January, contact with the islands was restored. [11]

The electrical grid on Ha'apai sustained tremendous damage, with 90 percent of power lines being lost or severely damaged. Approximately 1,000 customers lost power during the storm. Estimates placed the cost to repair the system at NZ$4 million (US$3.5 million). By January 23, only 100 residences had power back and Tonga Power Limited (TPL) stated it could take a further two months to fully restore the system. [12] In addition to the severe disruption to power, 80–90 percent of the region's water supply was lost. Most residents in Ha'apai rely on rain water collection, and the collection tanks were largely destroyed by the storm. [13] The nation's tourism industry also experienced moderate to severe losses, with damage to facilities amounting to T$1.6 million (US$861,000). [14] Throughout the archipelago, 1,130 buildings were affected, half of which were completely destroyed. Of those structures not destroyed, 34 percent sustained major damage, including 13 schools. Approximately 2,300 people were left homeless by the storm. [15]

Total damage from the storm amounted to an estimated T$90.2 million (US$48 million). [16]

Aftermath

This church on Lifuka Island had its roof torn off by Cyclone Ian. A church on Lifuka Island in Tonga had its roof torn off by Cyclone Ian (12041227283).jpg
This church on Lifuka Island had its roof torn off by Cyclone Ian.

In the wake of Ian, the ANZ bank donated T$15,000 (US$8,000) to the Tonga Red Cross Society. [14] New Zealand provided NZ$2.27 million (US$1.87 million) in assistance to the TPL. In addition, six electricians, a front end loader, and a tractor were sent to assist in restoration and debris removal efforts. [17] Australia provided A$50,000 in emergency supplies including blankets, water containers, tarpaulins, kitchen sets and hygiene kits. [18] On January 22, the director of Tonga's National Emergency Office, Leveni Aho, announced that the scale of damage was beyond Tonga's ability to handle on its own and made a formal request for internal aid. Following this, China sent 400 tents to house displaced persons while France provided a cargo plane for supply transport. [13] In accordance with the FRANZ agreement, enacted in 1992, the Government of France established an air route from Nuku'alofa to Ha'apai and deployed an aircraft carrier from New Caledonia. The carrier, loaded with supplies from the French Red Cross, arrived in Tonga on January 17. [19] The Government of Turkey made a contribution of US$50,000 to assist Tonga with relief operations. [20] The Japanese Government provided 600  jerrycans and 30 water tanks (3,700 litre capacity), collectively worth ¥13 million (US$127,000). [21] Recovery from the cyclone was slow with over 80 families still living in tents over a year after the system had affected the islands. [22]

See also

Related Research Articles

<span class="mw-page-title-main">2007–08 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">2006–07 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">2003–04 South Pacific cyclone season</span> Tropical cyclone season

The 2003–04 South Pacific cyclone season was a below-average season with only three tropical cyclones occurring within the South Pacific to the east of 160°E. The season officially ran from November 1, 2003 to April 30, 2004 with the first disturbance of the season forming on December 4 and the last disturbance dissipating on April 23. This is the period of the year when most tropical cyclones form within the South Pacific Ocean.

<span class="mw-page-title-main">2002–03 South Pacific cyclone season</span> Tropical 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).

<span class="mw-page-title-main">2008–09 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">Timeline of the 2008–09 South Pacific cyclone season</span>

The 2008–09 South Pacific cyclone season was a below-average season with only six tropical cyclones occurring within the South Pacific between 160°E and 120°W. The season officially ran from November 1, 2008 to April 30, 2009 with the first disturbance of the season forming on December 1 and the last disturbance moving out of the region on April 11.

<span class="mw-page-title-main">2009–10 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">1996–97 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">Cyclone Cilla</span> Category 1 South Pacific cyclone in 2003

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.

<span class="mw-page-title-main">Timeline of the 2009–10 South Pacific cyclone season</span>

This timeline documents all of the events of the 2009–10 South Pacific cyclone season which is the period that tropical cyclones formed in the southern Pacific Ocean. Within the Southern Pacific Ocean, most tropical cyclones form within the cyclone season which began on November 1 and will end on April 30, though occasionally cyclones form outside these times. The scope of this article is limited to tropical cyclones that form in the Indian Ocean 160°E and 120°W to the south of the equator. Should a tropical cyclone form to the west of 160°E then it will be monitored within the Australian region by the Australian Bureau of Meteorology, should a tropical cyclone form to the east of 120°W, it is unclear how it will be handled as no tropical cyclone has ever been observed in the South Pacific Ocean east of 120°W.

<span class="mw-page-title-main">2010–11 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">2011–12 South Pacific cyclone season</span> Tropical cyclone season

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.

<span class="mw-page-title-main">2012–13 South Pacific cyclone season</span> Tropical cyclone season

The 2012–13 South Pacific cyclone season was a below average tropical cyclone season, with five tropical cyclones occurring within the basin between 160°E and 120°W. The season officially ran from November 1, 2012, to April 30, 2013, however the last tropical disturbance was last noted on May 1, as it moved into the subtropics. During the season, tropical cyclones were officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BoM) and New Zealand's MetService. The United States Joint Typhoon Warning Center (JTWC) and other national meteorological services including Météo-France and NOAA also monitored the basin during the season. During the season there were 22 significant tropical disturbances assigned a number and a F suffix by the FMS's Regional Specialized Meteorological Center in Nadi, Fiji (RSMC Nadi), including Severe Tropical Cyclone Sandra which moved into the basin from the Australian region on March 9. The BoM, MetService and RSMC Nadi all estimated sustained wind speeds over a period of 10-minutes and used the Australian tropical cyclone intensity scale, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHS).

<span class="mw-page-title-main">Cyclone Wilma</span>

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.

<span class="mw-page-title-main">2013–14 South Pacific cyclone season</span> Tropical cyclone season

The 2013–14 South Pacific cyclone season was a slightly below average tropical cyclone season, with six tropical cyclones occurring within the basin between 160°E and 120°W. The season ran from November 1, 2013, to April 30, 2014, however, the first four tropical disturbances occurred during October 2013 and were included as a part of the season. During the season, tropical cyclones were officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BoM) and New Zealand's MetService. The United States Joint Typhoon Warning Center (JTWC) and other national meteorological services including Météo-France and NOAA also monitored the basin during the season. During the season there were 21 significant tropical disturbances were assigned a number and an "F" suffix by the FMS's Regional Specialized Meteorological Center in Nadi, Fiji (RSMC Nadi), including the remnants of Tropical Cyclone Hadi from the Australian region. The BoM, MetService and RSMC Nadi all estimated sustained wind speeds over a period of 10-minutes and used the Australian tropical cyclone intensity scale, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHS).

<span class="mw-page-title-main">2014–15 South Pacific cyclone season</span> Tropical cyclone season

The 2014–15 South Pacific cyclone season was a slightly-below average tropical cyclone season, with five tropical cyclones occurring within the basin between 160°E and 120°W. The season officially ran from November 1, 2014, to April 30, 2015. During the season, tropical cyclones were officially monitored by the Regional Specialized Meteorological Center (RSMC) in Nadi, Fiji and the Tropical Cyclone Warning Centers 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 form in or move into 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 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).

<span class="mw-page-title-main">Cyclone Evan</span> Category 4 cyclone in the South Pacific in 2012

Severe Tropical Cyclone Evan was considered to be the worst tropical cyclone to affect the island nation of Samoa since Cyclone Val in 1991 and was the strongest storm to impact the main South Pacific islands until Winston in 2016. The system was first noted on December 9, 2012, as a weak tropical depression about 700 km (435 mi) to the northeast of Suva, Fiji. Over the next couple of days, the depression gradually developed further before it was named Evan on December 12, as it had fully developed into a tropical cyclone. During that day the system moved toward the Samoan Islands and gradually intensified, before the system slowed and severely affected the Samoan Islands during the next day with wind gusts of up to 210 km/h (130 mph).

<span class="mw-page-title-main">2015–16 South Pacific cyclone season</span> Tropical cyclone season

The 2015–16 South Pacific cyclone season was one of the most disastrous South Pacific tropical cyclone seasons on record, with a total of 50 deaths and $1.405 billion in damage. Throughout the season, 8 systems attained tropical cyclone status, whilst 5 became severe tropical cyclones. The most notable cyclone of the season by far was Winston, which attained a minimum pressure of 884 hPa, and maximum ten-minute sustained winds of 175 mph (280 km/h), making it the most intense tropical cyclone on record in the Southern Hemisphere. Winston went on to devastate Fiji, causing $1.4 billion in damage and 44 deaths across the country.

<span class="mw-page-title-main">2017–18 South Pacific cyclone season</span> Tropical cyclone season

The 2017–18 South Pacific cyclone season was a slightly below-average season that produced 6 tropical cyclones, 3 of which became severe tropical cyclones. The season officially began on November 1, 2017, and ended on April 30, 2018; however, a tropical cyclone could form at any time between July 1, 2017, and June 30, 2018, and would count towards the season total. During the season, tropical cyclones were officially monitored by the Fiji Meteorological Service, MetService and the Australian Bureau of Meteorology, while the United States Joint Typhoon Warning Center (JTWC) also monitored the basin and issued warnings for American interests. The FMS attaches a number and an F suffix to significant 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 BoM, FMS and MetService all use the Australian Tropical Cyclone Intensity Scale and estimate wind speeds over a period of ten minutes, while the JTWC estimates sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHWS).

<span class="mw-page-title-main">Cyclone Lusi</span>

Severe Tropical Cyclone Lusi was the second severe tropical cyclone of the 2013–14 season and affected Fiji, Vanuatu and New Zealand.

References

  1. 1 2 RSMC Nadi — Tropical Cyclone Centre (January 2, 2014). "Tropical Disturbance Summary January 2, 2014 21z". Fiji Meteorological Service. Archived from the original on January 3, 2014. Retrieved January 9, 2014.
  2. RSMC Nadi — Tropical Cyclone Centre (January 3, 2014). "Tropical Disturbance Summary January 3, 2014 21z". Fiji Meteorological Service. Archived from the original on January 3, 2014. Retrieved January 10, 2014.
  3. RSMC Nadi — Tropical Cyclone Centre (January 4, 2014). "Tropical Disturbance Summary January 4, 2014 06z". Fiji Meteorological Service. Archived from the original on January 4, 2014. Retrieved January 10, 2014.
  4. Joint Typhoon Warning Center (January 4, 2014). "Significant Tropical Weather Advisory for the Western and South Pacific Oceans January 4, 2014 12z". United States Navy, United States Air Force. Archived from the original on January 3, 2013. Retrieved January 10, 2014.
  5. Joint Typhoon Warning Center (January 5, 2014). "Tropical Cyclone 07P Tropical Cyclone Advisory January 5, 2014 21z". United States Navy, United States Air Force. Archived from the original on January 6, 2014. Retrieved January 10, 2014.
  6. RSMC Nadi — Tropical Cyclone Centre (January 5, 2014). "Tropical Disturbance Advisory January 5, 2014 21z". Fiji Meteorological Service. Archived from the original on January 6, 2014. Retrieved January 10, 2014.
  7. RSMC Nadi — Tropical Cyclone Centre (January 8, 2014). "Tropical Disturbance Advisory January 8, 2014 00z". Fiji Meteorological Service. Archived from the original on January 8, 2014. Retrieved January 12, 2014.
  8. RSMC Nadi — Tropical Cyclone Centre (January 8, 2014). "Tropical Disturbance Advisory January 8, 2014 18z". Fiji Meteorological Service. Archived from the original on January 9, 2014. Retrieved January 12, 2014.
  9. "State of Emergency declared for Vava'u and Ha'apai". Matangi Tonga. 11 January 2014. Retrieved 3 September 2022.
  10. "Cyclone rips through Tonga".
  11. "Extensive cyclone damage across Tonga". Australian Broadcasting Corporation . 13 January 2014.
  12. "US$3.5 million and two months to restore Ha'apai's power". Dateline Pacific. Radio New Zealand International. January 23, 2014. Archived from the original on September 24, 2015. Retrieved January 26, 2014.
  13. 1 2 "Cyclone Ian: Tonga appeals for international help in relief efforts". Australian Broadcasting Corporation. January 22, 2014. Archived from the original on January 26, 2014. Retrieved January 26, 2014.
  14. 1 2 "Tonga's Tourism Ministry estimates $1.6m damage to Ha'apai tourism facilities". Matangi Tonga. Islands Business. January 20, 2014. Archived from the original on February 1, 2014. Retrieved January 26, 2014.
  15. "Tonga asks for more NZ help in Cyclone Ian aftermath". ONE News. Television New Zealand Limited. January 17, 2014. Archived from the original on February 2, 2014. Retrieved January 26, 2014.
  16. January 2014 Global Catastrophe Recap (PDF) (Report). AON Benfield. 2014. Retrieved December 23, 2014.
  17. "NZ linesmen to help restore Tongan power". Australian Associated Press. MSN New Zealand. January 25, 2014. Archived from the original on February 1, 2014. Retrieved January 26, 2014.
  18. "Australia responds to Cyclone Ian in Tonga". Australian Government. January 14, 2014.
  19. "Aide française au profit des populations sinistrées des Ha'apai après le passage du cyclone Ian (Tonga, 11-12 janvier 2014)". Government of France (in French). ReliefWeb. January 23, 2014. Retrieved January 26, 2014.
  20. "Relations between Turkey and Tonga". Republic of Turkey Ministry of Foreign Affairs. Retrieved 4 January 2021.
  21. "Japan Handed Over Emergency Assistance for Cyclone Disaster". Government of Japan. ReliefWeb. January 24, 2014. Retrieved January 26, 2014.
  22. "New houses for Tongan cyclone victims". 17 February 2015.
Severe Tropical Cyclone Ian
Ian Jan 11 2014 0140Z.jpg
Cyclone Ian on January 11