Top Qs
Timeline
Chat
Perspective
1984–85 South Pacific cyclone season
Tropical cyclone season From Wikipedia, the free encyclopedia
Remove ads
The 1984–85 South Pacific cyclone season was an above-average tropical cyclone season, with nine tropical cyclones occurring within the basin between 160°E and 120°W. The season ran from November 1, 1984, to April 30, 1985, with tropical cyclones 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 was nine tropical cyclones occurring within the basin, including three that moved into the basin from the Australian region. The BoM, MetService and RSMC Nadi all estimated sustained wind speeds over a period of 10-minutes, which are subsequently compared to 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 (SSHWS).
Remove ads
Seasonal summary
During November and December no significant tropical cyclones developed in or moved into the basin in the region,
The remnants of Tropical Cyclone Pierre were last noted during 24 February, as they moved into the basin from the Australian region.[1][2]
Systems
Summarize
Perspective
Unnamed tropical cyclone
An unnamed tropical cyclone existed from December 26 to December 28.
Tropical Cyclone Monica
Tropical Cyclone Monica existed from December 29 to December 30.
Tropical Cyclone Drena
Tropical Cyclone Drena existed from January 9 to January 16.
Severe Tropical Cyclone Eric
On January 13, TCWC Nadi started to monitor a shallow depression that had developed within the monsoon trough about 725 km (450 mi) to the west of Espiritu Santo, Vanuatu.[3] Over the next day the system moved eastwards and developed further as gale-force winds developed near the systems centre before the JTWC initiated advisories on the system and designated it as Tropical Cyclone 11P during January 14.[3][4] The system was subsequently named Eric by TCWC Nadi as it moved closer to Espiritu Santo and became equivalent to a category 1 tropical cyclone.[3][5] During January 15, Eric passed near or over Espiritu Santo, as it continued to intensify before it turned and accelerated south-eastwards.[3] Eric subsequently became equivalent to a category 3 severe tropical cyclone early the next day, before an Air Pacific flight from Fiji to the Solomon Islands located the systems eye on radar.[3]
During January 17, Eric's well defined eye came into the range of Nadi airports surveillance radar, before TCWC Nadi estimated that Eric had peaked with 10-minute sustained wind-speeds of 150 km/h (90 mph).[3][5] During that day Eric's eye seemed to contract to around 15 km (10 mi) as it made passed through Fiji's Western Division and made landfall on the Fijian main island of Viti Levu about 10 km (5 mi) to the south of Nadi.[3] After the system had made landfall, the JTWC estimated that Eric had peaked with 1-minute sustained wind speeds of 185 km/h (115 mph), which made it equivalent to a category 3 hurricane on the SSHWS.[5]The system subsequently passed near or over Fiji's capital: Suva before emerging into the Korro Sea and weakening. Eric subsequently passed through the Tonga's Ha'apai islands just to the south of Nomuka during January 18, before it gradually weakened and was last noted during January 20, over 1,800 km (1,120 mi) to the south of Papeete, French Polynesia.[5]
Severe Tropical Cyclone Nigel
Late on January 16, Tropical Cyclone Nigel moved into the South Pacific basin from the Australian region. During the next day the system continued to move eastwards and developed an eye, before it became equivalent to a modern-day category 3 severe tropical cyclone.
Severe Tropical Cyclone Odette
At around 1300 UTC on January 19, Severe Tropical Cyclone Odette moved into the South Pacific Basin from the Australian Region.
Severe Tropical Cyclone Freda
During January 26, the FMS reported that a depression was located within the vicinity of the Southern Cook Islands about 150 km (95 mi) to the west-northwest of the island of Aitutaki.
Tropical Cyclone Gavin
During March 2, the Fiji Meteorological Service reported that a tropical depression had developed within a monsoon trough, in between Espiritu Santo and Rotuma about 450 km (280 mi) to the northwest of Fiji.[6][7] Over the next couple of days, the system gradually developed further as it moved southwards, while moderate to strong winds were recorded in Vanuatu's southern islands of Aneityum and Tanna.[6][7] During March 4, the United States Joint Typhoon Warning Center initiated advisories on the depression and designated it as Tropical Cyclone 27P, while the system was located about 300 km (185 mi) to the northeast of Port Vila in Vanuatu.[8] Later that day the FMS named the system Gavin, after it had become equivalent to a category 1 tropical cyclone on the modern day Australian tropical cyclone intensity scale.[6][8] At this time, Gavin was estimated to have an unusually large area of gale-force winds, with winds extending out to about 550 km (340 mi) in its northern semicircle and 280 km (175 mi) in its southern semicircle.[6] During March 5, the system intensified slightly and attained storm-force winds as it moved south-eastwards, before the FMS reported that Gavin had peaked as a category 2 tropical cyclone with 10-minute sustained winds of 95 km/h (60 mph).[6][8] Over the next couple of days, as the system moved south-eastwards brushed Fiji, there were no significant changes in Gavin's intensity, however, the wider area of gales moved into the system's semicircle.[6] During March 7, the JTWC reported that the system had peaked with 1-minute sustained wind speeds of 100 km/h (65 mph), before Gavin started to weaken and lose its tropical characteristics, as it accelerated south-eastwards towards higher latitudes.[6][8] Later that day, the FMS handed the primary warning responsibility for the system to the New Zealand Meteorological Service (NZMS), after Gavin had moved out of their area of responsibility.[6][8] During March 8, the NZMS reported that the system had become an extratropical depression after it had lost most of its tropical characteristics, before it was last noted during the following day, while it was located about 2,100 km (1,305 mi) to the southeast of Wellington in New Zealand.[6][8]
Severe Tropical Cyclone Hina
Hina was one of the most intense tropical cyclones ever recorded in the South Pacific basin. Having a distinct rainband and well defined outflow with low wind shear and warm water temperature, Hina underwent a period of Explosive Deepening (rapid intensification) The storm continued southward. Due to unfavorable conditions and an approaching Eyewall Replacement Cycle, the storm weakened into a tropical storm. As its center became ill-defined, the storm lost winds of tropical storm force and weakened into a tropical depression. The remnants dissipated some time later.
Other system
According to the JTWC, Tropical Depression 08P formed on 26 December. On 28 December, 08P reached tropical storm status, and would later dissipate south of Fiji.
Remove ads
Season effects
Summarize
Perspective
This table lists all the storms that developed in the South Pacific basin during the 1984–85 season. It includes their intensity on the Australian Tropical cyclone intensity scale, duration, name, areas affected, deaths, and damages.
Remove ads
See also
- Weather of 1985
- Atlantic hurricane seasons: 1984, 1985
- Pacific hurricane seasons: 1984, 1985
- Pacific typhoon seasons: 1984, 1985
- North Indian Ocean cyclone seasons: 1984, 1985
- 1984–85 South-West Indian Ocean cyclone season
- 1984–85 Australian region cyclone season
References
External links
Wikiwand - on
Seamless Wikipedia browsing. On steroids.
Remove ads