Meteorological history | |
---|---|
Formed | 1 May 2017 |
Extratropical | 10 May |
Dissipated | 16 May 2017 |
Category 5 severe tropical cyclone | |
10-minute sustained (FMS) | |
Highest winds | 205 km/h (125 mph) |
Lowest pressure | 935 hPa (mbar);27.61 inHg |
Category 4-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 230 km/h (145 mph) |
Lowest pressure | 929 hPa (mbar);27.43 inHg |
Overall effects | |
Fatalities | 2 total |
Damage | $10 million (2017 USD) |
Areas affected | Solomon Islands,Vanuatu,New Caledonia,New Zealand |
IBTrACS | |
Part of the 2016–17 South Pacific cyclone season |
Severe Tropical Cyclone Donna was the strongest off-season tropical cyclone in the Southern Hemisphere at the time,since surpassed by Cyclone Lola in 2023. The twenty-first tropical disturbance,third named storm,and second severe tropical cyclone of the annual cyclone season,Donna formed from an area of disturbed weather that was first monitored west-northwest of Fiji on 1 May 2017. The disturbance drifted eastward amid an increasingly favourable environment,and it was designated Tropical Depression 21F late on 2 May. Twelve hours later,it intensified into a Category 1 on the Australian tropical cyclone scale and was designated Tropical Cyclone Donna as the storm's motion shifted west and then south. After reaching its initial peak as a Category 4 cyclone early on 6 May,the effects of wind shear and upwelling caused the storm to weaken. However,it reintensified into a Category 5 cyclone on 8 May. Soon after,Donna entered a region of strong westerly flow and began to rapidly weaken. Continuing to accelerate in a southerly direction,Donna eventually weakened into a tropical low on 10 May. By 16 May,Donna's remnants had fully dissipated.
Buffeting the island chain of Vanuatu,Donna has resulted in severe damage throughout the northern provinces,though the exact extent is unknown in the absence of good communication.
On 1 May, the day after the official end of the South Pacific cyclone season, the Joint Typhoon Warning Center (JTWC) began monitoring an area of disturbed weather about 1,455 km (905 mi) west-northwest of Nadi. Though it possessed an oblong area of low pressure partially exposed to the northeast of deep shower and thunderstorm activity, the system was embedded within an environment of moderate wind shear, good upper-level outflow, and warm ocean temperatures. [1] The official warning agency for the South Pacific, the Fiji Meteorological Service (FMS), began monitoring the disturbance a short while later. [2] As fragmented spiral bands began wrapping into the centre of circulation, the JTWC assessed that the potential for tropical cyclone formation was high, issuing a Tropical Cyclone Formation Alert accordingly at 21:00 UTC on 1 May. [3] The storm tracked slowly eastward through the northern islands of Vanuatu but consolidated rapidly as upper-level winds became light, prompting the FMS to upgrade the disturbance to Tropical Depression 21F at 18:00 UTC on 2 May. [4] This was followed by the JTWC's classification of Tropical Cyclone 18P three hours later. [5]
Following formation, the depression turned west in response to a developing subtropical ridge to its south. [6] A continued favourable environment allowed it to intensify into a Category 1 on the Australian tropical cyclone scale by 06:00 UTC on 3 May, at which point it was named "Donna" by the FMS, [7] and further to Category 2 intensity by 18:00 UTC. [8] The JTWC, meanwhile, upped the cyclone to the equivalent of a Category 1 hurricane on the Saffir–Simpson scale, citing consolidation of deep convection near the centre and satellite intensity estimates around 120 km/h (75 mph). [9] Despite some evidence of wind shear along the northern fringes of the storm, it began to clear an eye late on 4 May, prompting the JTWC to classify Donna as a Category 2 equivalent, [10] and the FMS to upgrade to Category 3 strength. [11] At 00:00 UTC on 6 May, after re-tracking through Vanuatu and beginning a southward track, Donna attained its initial peak as a Category 4 cyclone. [12] [13]
Shortly thereafter, the effects of increased northeasterly upper-level flow became more prevalent as the storm's cloud pattern changed to a central cold cover and then devolved into patchy areas of moderate convection. [14] Around 09:00 UTC on 6 May, the JTWC reduced the storm back to a Category 1 equivalent, [15] and by 18:00 UTC, the FMS indicated Donna had weakened to a Category 3 cyclone on the Australian scale. [16]
Drifting south-southwest and then south, Donna continued to struggle under the combined effects of upper-level winds and ocean upwelling. [17] By early on 7 May, however, convection within the eyewall began to increase in intensity, [18] and the FMS upgraded Donna to a Category 4 cyclone for a second time accordingly. [19] Three hours later, the JTWC estimated that it had intensified to a Category 4 equivalent, completely skipping Category 3 status. [20] With a solid ring of deep convection surrounding a well-defined 55 km (35 mi) eye, [21] the FMS upgraded Donna to a Category 5 cyclone at 00:00 UTC on 8 May, estimating that the storm possessed 10-minute sustained winds of 205 km/h (125 mph). [22] As a result, Donna became the strongest off-season tropical cyclone on record during the month of May in the South Pacific basin. [23] Weakening began shortly following peak intensity as Donna's eye became partially obscured and the eastern eyewall was eroded; [24] the storm weakened back to Category 4 intensity by 18:00 UTC on 8 May, [25] Category 1 intensity by 21:00 UTC on 9 May, [26] and ultimately degenerated into a tropical low by 06:00 UTC on 10 May as it dodged New Caledonia. [27]
According to Aon Benfield Inc. in January 2018, Donna was responsible for two deaths and a total of US$10 million in damage. [28]
As Donna buffeted Vanuatu, entire villages across the Torres Islands of Torba Province were forced to seek refuge in caves. Throughout the province, buildings were destroyed and others had their roofs ripped off. Heavy rainfall led to flooding of low-lying areas of Efate. In Port Vila, rushing water carved out large chunks of land that resulted in structural collapse. [29] Across the entire northern half of the island chain, crops sustained significant damage and water sources were contaminated, though the full extent of the damage was unknown as a result of severed communications. [30] [31]
In the Temotu Province, Donna caused two fatalities; an adult who was struck by a fallen branch and a primary school student of Tarano School who drowned on an out-board motorboat when crossing from one-side to the other side of a lake. [32]
Moisture from the remnants of Donna combined with a weakening Tasman Sea low to produce heavy rains over much of the North Island and the west coast of the South Island. In expectation of more than 100 mm (3.9 in) of rain, heavy rain warnings were issued for Nelson and the Bay of Plenty regions, while severe weather warnings were issued for much of the North Island. [33] [34]
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.
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 2007–08 South Pacific cyclone season was a below-average season with only four tropical cyclones, forming within the South Pacific to the east of 160°E. The season officially ran from November 1, 2007, to April 30, 2008, although the first cyclone, Tropical Depression 01F, formed on October 17.
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.
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 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.
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.
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).
Severe Tropical Cyclone Pat was a small but strong tropical cyclone that passed directly over Aitutaki, Cook Islands, in southern Pacific Ocean on February 10, 2010. Part of a series of storms to impact the group of islands early that year, Pat was first identified as a tropical depression on February 6 well to the northeast of the Samoan Islands. The storm steadily organized as it moved generally southeast, becoming a tropical cyclone on February 8. Turning to the south, intensification began in earnest and the system acquired hurricane-force winds within 48 hours of being named. The 445 km (275 mi) wide system displayed annular characteristics and a 19 km (12 mi) wide eye. Pat reached its peak strength early on February 10 as a severe tropical cyclone with winds of 140 km/h (85 mph) and a barometric pressure of 960 mbar. Hours later it struck Aitutaki, producing gusts in excess of 185 km/h (115 mph) on the island. Hostile wind shear then prompted rapid weakening of the cyclone. The system degraded below gale-intensity on February 11, just 24 hours after it peaked, and was last noted early on February 12.
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).
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.
The 2016–17 South Pacific cyclone season was the least active South Pacific cyclone season since the 2011–12 season, with only four tropical cyclones occurring within the South Pacific Ocean to the east of 160°E. Two of the four systems developed into severe tropical cyclones on the Australian tropical cyclone intensity scale. The season officially ran from November 1, 2016 until April 30, 2017. However, May featured two post-season systems: Donna and Ella, of which the former was the strongest post-season South Pacific tropical cyclone ever recorded in that month. Overall, 22 tropical disturbances were monitored by a combination of the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BoM) and New Zealand's MetService.
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).
The 2019–20 South Pacific cyclone season was a slightly above-average season in which tropical cyclones formed within the South Pacific Ocean to the east of 160°E. The season officially ran from November 1, 2019, to April 30, 2020, however a tropical cyclone could form at any time between July 1, 2019, and June 30, 2020, and would count towards the season total. The season began on November 22 with the formation of Tropical Cyclone Rita, which would later become a severe tropical cyclone. The season has been near-average in terms of activity, with 8 tropical cyclones and 4 severe tropical cyclones forming during the season. The season featured Cyclone Harold, the first Category 5 severe tropical cyclone in the basin since Cyclone Gita, and one of the strongest since Cyclone Winston. During the season, tropical cyclones are officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BOM) and New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) also monitors the basin and issue unofficial warnings for American interests. The FMS attaches a number and an F suffix to tropical disturbances that form in or move into the basin while the JTWC designates significant tropical cyclones with a number and a P suffix. The FMS, BoM and MetService all use the Australian Tropical Cyclone Intensity Scale and estimate wind speeds over a period of ten minutes, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHWS).
The 2020–21 South Pacific cyclone season was an average season where most tropical cyclones formed within the South Pacific Ocean to the east of 160°E. The season officially started on November 1, 2020, and officially ended on April 30, 2021, however a tropical cyclone could form at any time between July 1, 2020, and June 30, 2021, and would count towards the season total. During the season, tropical cyclones will be officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BoM), New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) will also monitor the basin and issue 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).
Severe Tropical Cyclone Gavin was the most intense tropical cyclone to affect Fiji, since Cyclone Oscar of the 1982–83 cyclone season and was the first of three tropical cyclones to affect the island nations of Tuvalu and Wallis and Futuna during the 1996–97 season. The system that was to become Gavin was first identified during March 2, as a weak tropical depression that had developed within the monsoon trough of low pressure. Over the next two days the depression gradually developed further, before it was named Gavin by RSMC Nadi early on March 4 as it had developed into a tropical cyclone.
The 2021–22 South Pacific cyclone season was a near average tropical cyclone season within the South Pacific Ocean to the east of 160°E. The season officially started from November 1, 2021, and officially ended on April 30, 2022, however a tropical cyclone could form at any time between July 1, 2021, and June 30, 2022, and would count towards the season total. During the season, tropical cyclones will be officially monitored by the Fiji Meteorological Service, Australian Bureau of Meteorology and New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) will also monitor the basin and issue unofficial warnings for American interests. The FMS attaches a number and an F suffix to tropical disturbances that form in or move into the basin while the JTWC designates significant tropical cyclones with a number and a P suffix. The BoM, FMS and MetService 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).
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.
The 2023–24 South Pacific cyclone season was a below-average season within the South Pacific Ocean to the east of 160°E. The season officially started on November 1, 2023, and ended on April 30, 2024, however a tropical cyclone could form between July 1, 2023, and June 30, 2024, and still be included in the season, as shown by Cyclone Lola which formed in October. During the season, tropical cyclones will be officially monitored by the Fiji Meteorological Service, Australian Bureau of Meteorology and New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) will also monitor the basin and issue unofficial warnings for American interests. The FMS attaches a number and an F suffix to systems that are active in 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 winds with a 10-minute period, while the JTWC estimates winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHWS).