1991–92 Australian region cyclone season

none November 2024 Aus 1992 1991-1992 Australian region cyclone season summary.png 2 December 1991 13 April 1992 Graham 915 110 10 12 10 9 7 13.94 1989–90, 1990–91, 1991–92, 1992–93, 1993–94 1991–92 South-West Indian Ocean cyclone season 1991–92 South Pacific cyclone season The 1991–92 Australian region cyclone season saw several intense storms. It was also an event in the ongoing cycle of tropical cyclone formation. It ran from 1 November 1991 to 30 April 1992. The regional tropical cyclone operational plan also defines a tropical cyclone year separately from a tropical cyclone season, and the "tropical cyclone year" ran from 1 July 1991 to 30 June 1992. Tropical cyclones in this area were monitored by four Tropical Cyclone Warning Centres (TCWCs): the Australian Bureau of Meteorology in Perth, Darwin, and Brisbane; and TCWC Port Moresby in Papua New Guinea. Seasonal summary Systems Severe Tropical Cyclone Graham Aus Graham 1991 path.png Graham 1991-12-05 0852Z.jpg 2 December 12 December 110 120 915 On 2 December, a south-southwesterly moving low pressure system formed. Rapidly intensifying, Tropical cyclone Graham was classified the next day about 750 km mi on northwest of Cocos Island. Within 24 hours, an eye developed. Shortly thereafter, Graham turned towards the southeast due to influence of a deep-layer anticyclone to the east. Maximum intensity was reached at 1500 UTC 5 December as a Category 5 system. As the cyclone tracked away from Cocos Island, it encountered less favorable conditions. By 0000 UTC 8 December, the low-level circulation became fully exposed on the northwest side of the deep convection. Graham weakened below cyclone intensity at 1800 UTC 9 December and became devoid of convection the next day.Severe Tropical Cyclone Graham 15 August 2012 Australian: Bureau of Meteorology http://www.bom.gov.au/cyclone/history/graham91.shtml Tropical Cyclone Mark Aus Mark jan 9 1992 0519Z.jpg Mark 1992 path.png 7 January 10 January 55 55 980 Tropical cyclone Mark formed within the monsoon trough in the Timor Sea, west of Melville Island, on 6 January. The system tracked rapidly eastwards across northern Australia, entering the Gulf of Carpentaria at 1200 UTC 7 January. Once over water, satellite imagery indicated that the system slowly organized and by 0600 UTC 8 January, whilst approaching the central Gulf of Carpentaria, it was upgraded into a Category 1 cyclone. Upon naming, Mark slowed and adopted a slightly northeastward track in response to enhanced ridging to the south. This track was maintained for the next 40 hours and at 2100 UTC 9 January, Mark crossed the western coast of Cape York Peninsula just south of Weipa. Maximum sustained winds at landfall were estimated at 100 km/h mph on with a central pressure of 980 mbar inHg on. Mark soon weakened as it crossed the peninsula and was downgraded to a tropical depression at 1200 UTC 10 January. Mark dissipated later that day. Weipa sustained minor, but widespread damage with failing trees often being a consequence for damage to houses and power lines. High waves brought $3.5 million (AUD) damage to the Weipa port.Tropical Cyclone Mark 15 August 2012 Australian: Bureau of Meteorology http://www.bom.gov.au/cyclone/history/betsy.shtml Brisbane Tropical Cyclone Warning Center Severe Tropical Cyclone Betsy Aus Betsy 1992-01-10 2100Z.png Betsy 1992 path.png 10 January (entered basin) 14 January (exited basin) 85 90 950 Cyclone Betsy A deep depression formed from gale-force westerlies on 5 January. The depression continued to intensify as it drifted slowly west and became a Category 1 cyclone the next day. During the next 12 hours, Betsy rapidly intensified while moving south-southeast slowly. Mean winds associated with the cyclone reached storm-force late on 7 January and the system turned to the southwest and subsequently the cyclone approached the central Vanuatu Islands. By 1800 UTC 8 January, Besty developed hurricane-force winds. Six hours later, the core of the cyclone struck the islands of Ambrym and Malakula in central Vanuatu while developing a large ragged eye. Betsy continued to intensify after existing Vanuatu, and reached maximum intensity very early on 10 January while located 200 km mi on north of New Caledonia. By 11 January, Besty had become less organized. Meanwhile, the eye shrunk and became ragged. was losing organisation, with the large eye (diameter of 165 km) rapidly shrinking and becoming elongated and ragged. Midday 11 January, Betsy recurved sharply to the south and by 13 January Betsy had dissipated. However, the extratropical remnants passed close to the northern coast of New Zealand on 17 January. On Malakula, sustained winds of 118 km/h mph on were recorded between 0400 and 0500 UTC 9 January and the pressure dropped to 959 mbar inHg on. Tropical cyclone Betsy was blamed for significant damage in Vanuatu and was responsible for the deaths of two people. The worst impact was felt on Efate, where there was a 3 m ft on storm surge.Tropical Cyclone Besty 15 August 2012 Australian: Bureau of Meteorology http://www.bom.gov.au/cyclone/history/betsy.shtml Brisbane Tropical Cyclone Warning Center Severe Tropical Cyclone Daman SPac Daman 1992-02-18 0000Z.png Daman 1992 path.png 17 February (Crossed 160°E) 19 February 75 65 965 A tropical depression formed in the south Pacific on 11 February. The system steadily developed, and was named Daman on 15 February. Twelve hours later, the cyclone skirted Vanua Lava before passing northwest of Espiritu Santo. After emerging into Coral Sea, Cyclone Daman began curving to the southwest, and then south-southwest. On 17 February, it peaked in intensity as a Category 3 cyclone. The system began weakening shortly thereafter as environmental shear increased, and by Daman was no longer a tropical cyclone. Soon afterwards, the extratropical remnants turned rapidly eastwards, bringing gale-force winds to parts of the North Island of New Zealand. At Manukau Heads, a wind gust of 205 km/h mph on was recorded. Significant tree damage and downed power lines were reported in Auckland.Tropical Cyclone Daman 18 March 2012 Australian: Bureau of Meteorology https://web.archive.org/web/20120318210907/http://www.bom.gov.au/cyclone/history/daman.shtml 18 March 2012 live http://www.bom.gov.au/cyclone/history/daman.shtml Brisbane Tropical Cyclone Warning Center Severe Tropical Cyclone Harriet-Heather Aus Harriet-Heather 1992-03-01 0800Z.png Harriet-Heather 1992 path.png 24 February 8 March 95 120 930 A low formed on 24 February 550 km mi on east of Cocos Island. The low rapidly intensified under favorable conditions, and at 0600 UTC 25 February, the system was named. Initially, Harriet moved towards the islands, passing just south of North Keeling Island early on 27 February. The storm gradually became better organized, and early on 1 March, Cyclone Harriet attained peak intensity over estimated to have sustained winds of 115 km/h mph on and a central pressure of 930 mbar inHg on.Severe Tropical Cyclone Harriet http://www.bom.gov.au/cyclone/history/harriet92.shtml Australian Bureau of Meteorology 14 August 2012 The tropical cyclone weakened somewhat during the following next three days while continuing west. An approaching frontal system from the west resulted in Harriet re-curving to the south on 4 March. The storm continued to weakening due to strong wind shear. Harriet started to accelerate to the southeast on 6 March. The cyclone passed 700 km mi on to the southwest of Cape Leeuwin in southwest Western Australia during the evening of 8 March. Shortly after that, Harriet lost tropical features. A peak gust of 162 km/h mph on was recorded on Cocos Island, the second strongest on record on the island in the past 40 years. Harriet brought minor property damage on the island, but significant horticultural losses. Overall, damage was assessed at $600,000 (1992 AUD). Severe Tropical Cyclone Ian Aus Ian 1992-03-01 0649Z.jpg Ian 1992 path.png 27 February 4 March 105 115 930 Another depression developed in the monsoon trough, further east of Harriet-Heather, roughly 300 km mi on due south of Java. Unlike Harriet, this cyclone initially tracked east in response to a high amplitude upper trough located to the west. Under a favorable environment, the system was named Ian later that day. After re-curving to the south, Ian continued to intensify and on 0900 UTC 1 March, Ian bottomed out in intensity with 215 km/h mph on winds. Although Ian began weakening as it approached the Western Australian coast, it was still a severe cyclone as it tracked directly over the Monte Bellos Islands and Barrow Island. Ian subsequently crossed a sparsely populated stretch of coastline approximately 75 km mi on east of Onslow at 2145 UTC 2 March and weakened over land. Ian dissipated the next day.Severe Tropical Cyclone Ian http://www.bom.gov.au/cyclone/history/ian.shtml Australian Bureau of Meteorology 14 August 2012 Upon passing over the Monte Bellos Islands and Barrow Island, gusts to 205 km/h mph on were recorded. Effects from the system were mostly limited to the islands offshore. In the Monte Bellos, a mine was extensively damaged. Due to a 1.6 m ft on storm surge, a landing stage on Barrow Island sustained minor damage. On the Australian mainland, damage from the storm was minimal.http://archive.greenpeace.org/climate/database/records/zgpz0001.html Massive Cycline Threatens Northwest Australia 15 August 2012 GREENPEACE Climate Impacts Database https://web.archive.org/web/20120312061518/http://archive.greenpeace.org/climate/database/records/zgpz0001.html 12 March 2012 dead Severe Tropical Cyclone Esau SPac Esau 1992-02-28 2300Z.png Esau 1992 path.png 28 February (Entered basin) 1 March (Exited basin) 130 100 925 Cyclone Esau Esau moved into the Australian region and brought gale-force winds to the Solomon Islands during 29 February.Gill, Jonathan P The South Pacific and Southeast Indian Ocean Tropical Cyclone Season 1991–1992 Australian Meteorological Magazine 43 189 Australian Bureau of Meteorology 18 February 2015 http://www.bom.gov.au/amm/docs/1994/gill.pdf https://web.archive.org/web/20120321171916/http://www.bom.gov.au/amm/docs/1994/gill.pdf 21 March 2012 live In the same time, the JTWC also reported that Esau had peaked with 1-minute sustained wind speeds of 240 km/h mph 5 on, which made it equivalent to a category 4 hurricane on the Saffir-Simpson hurricane wind scale.United States Navy, United States Air Force http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1992/1992s-bsh/bsh211992.txt https://web.archive.org/web/20120917033345/http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1992/1992s-bsh/bsh211992.txt dead 17 September 2012 Tropical Cyclone 21P (Esau) best track analysis Naval Pacific Meteorology and Oceanography Center Joint Typhoon Warning Center 10 May 2013 However, Esau moved back into the South Pacific basin and started to weaken the next day.Tropical Cyclone Esau, February 24 - March 7 Fiji Meteorological Service Tropical Cyclone Report http://webapp1.dlib.indiana.edu/cgi-bin/virtcdlib/index.cgi/4274123/FID1/DATA/TROPIC/SWP_NAR/1992_6.NAR%3B1 Nadi Tropical Cyclone Warning Center 22 April 2013 26 June 2013 https://archive.today/20130626182255/http://webapp1.dlib.indiana.edu/cgi-bin/virtcdlib/index.cgi/4274123/FID1/DATA/TROPIC/SWP_NAR/1992_6.NAR;1 live Gill, Jonathan P The South Pacific and Southeast Indian Ocean Tropical Cyclone Season 1991–1992 Australian Meteorological Magazine 43 181 – 192 Australian Bureau of Meteorology http://www.bom.gov.au/amm/docs/1994/gill.pdf https://web.archive.org/web/20120321171916/http://www.bom.gov.au/amm/docs/1994/gill.pdf 21 March 2012 live 6 July 2014 Severe Tropical Cyclone Fran Aus Fran 1992-03-12 0000Z.png Fran 1992 path.png 11 March (Entered basin) 17 March 95 75 950 Cyclone Fran Fran moved into the region during 11 March as a Category 3 severe tropical cyclone, and peaked with 10-minute sustained winds of 145 km/h (90 mph).1992064S10184 1992 Tropical Cyclone FRAN (1992064S10184) International Best Track Archive for Climate Stewardship 15 April 2019 The cyclone had slowed by this stage and it subsequently assumed a somewhat erratic southwest track towards the coast. Over the subsequent next three days, Fran weakened as it became less organized. The cyclone finally crossed the Queensland coast near The Town of 1770 at 1700 UTC 15 March. Fran subsequently moved inland and weakened to a tropical depression before re-curving to the southeast and moving back over water. The remnants of Fran tracked over Norfolk Island before ultimately being merged by a trough north of New Zealand. In preparation of the storm, officials closed beaches along the Sunshine and Gold Coasts. In addition, train services from Brisbane were cancelled.Cyclone batters Queensland https://news.google.com/newspapers?id=BsFUAAAAIBAJ&pg=5045,1997891&dq=cyclone+fran&hl=en August 14, 2012 New Straits Times March 16, 1992 14 March 4, 2023 https://web.archive.org/web/20230304083619/https://news.google.com/newspapers?id=BsFUAAAAIBAJ&pg=5045,1997891&dq=cyclone+fran&hl=en live Across Queensland, coastal towns were flooded, uprooting trees and knocking out power.Australian cyclone floods coastal towns https://news.google.com/newspapers?id=eFpPAAAAIBAJ&pg=5039,4387592&dq=cyclone+fran&hl=en August 15, 2012 Toledo Blade March 16, 1992 2 Several roofs were torn off of homesCyclone slams Australian coast https://news.google.com/newspapers?id=40JWAAAAIBAJ&pg=1822,3579651&dq=cyclone+fran&hl=en August 15, 2012 Eugene Register-Guard March 16, 1992 2 and some flooding was reported.Tropical Storms https://news.google.com/newspapers?id=UKAaAAAAIBAJ&pg=4001,4557240&dq=cyclone+fran&hl=en August 15, 2012 The Milwaukee Journal March 22, 1992 51August 2026 InternetArchiveBot Winds and flooding caused minor property damage, but considerable crop losses along were reported the coast, with the worst effects in Bundaberg. A total of 40 houses were uproofed throughout Bundaberg. In Burnett Heads, 3 yachts were damaged. Heavy swells caused damage on Heron Island and severe erosion on the Gold and Sunshine Coasts. Overall, 2,624 insurance claims were made because of property damage. Total damage from the system was 8–10 million (1992 AUD),TROPICAL CYCLONE IMPACTS ALONG THE AUSTRALIAN EAST COAST FROM NOVEMBER TO APRIL 1858 TO 2000 http://www.australiasevereweather.com/cyclones/impacts-eastcoast.pdf Australia Severe Weather August 14, 2012 May 9, 2012 https://web.archive.org/web/20120509233225/http://australiasevereweather.com/cyclones/impacts-eastcoast.pdf live while insurance losses were estimated at $2.5 million (1992 AUD).Tropical Cyclone Fran http://www.bom.gov.au/cyclone/history/fran.shtml Australian Bureau of Meteorology August 14, 2012 November 29, 2014 https://web.archive.org/web/20141129040251/http://www.bom.gov.au/cyclone/history/fran.shtml live Severe Tropical Cyclone Neville Aus Neville Apr 8 1992 2311Z.png Neville 1992 path.png 7 April 13 April 110 120 945 A major surge of the Madden–Julian oscillation in early April resulting in the development of a tropical depression on 4 April near the Tanimbar Islands. At first, the depression drifted slowly southeast in an environment of low shear. By 0600 UTC 6 April, the circulation was well-defined and south to come under the influence of a deep easterly steering current generated by the subtropical ridge over inland Australia; at 0200 UTC 7 April, the depression re-curved to the southwest and was classified as a tropical cyclone. Despite its close proximity to land, Neville intensified rapidly due to its small size. Roughly 24 hours after being named, the storm attained hurricane-force winds. The cyclone continued deepening as it tracked into the central Timor Sea, reaching its peak intensity of 200 km/h (125 mph) around 1800 UTC 8 April. Shortly after its peak, Cyclone Neville slowed down response to the passage of a trough. After undergoing a small counterclockwise loop, the system resumed its track to the southwest. It weakened slowly. By 10 April, the eye of the cyclone had collapsed and increased winds shear caused the storm to become less organized. At 0800 UTC 11 April, sustained winds associated with Neville went below hurricane force and the cyclone stalled. Due to a combination of wind shear and cold water, and by 0200 UTC 13 April, Neville had dissipated, though the remnant low-level circulation was apparent for two more days as it drifted away to the southwest. In preparation of the cyclone on the Tiwi Islands, shipping was delayed and travel by air was cancelled. An oil rig supply boat was forced up on the beach by the winds, and 14 people were airlifted from the BHP rig Challis Venture. When Neville struck the islands only minor damage was reported. A few homes lost their roofs, trees were uprooted and power was knocked out. In addition, 14 people were airlifted when an oil rig was forced up the beach by high winds.EMA disaster database http://www.ema.gov.au/ema/emadisasters.nsf/0/ee3a4a5995bea718ca256d3300058019 14 August 2012 Tiwi Islands, NT: Cyclone dead https://web.archive.org/web/20071026084121/http://www.ema.gov.au/ema/emadisasters.nsf/0/ee3a4a5995bea718ca256d3300058019 26 October 2007 Damage on Australia associated with Serve Tropical Cyclone Neville was restricted to the northwestern portion the Northern Territory though widespread tree damage occurred and a camp was destroyed on Melville Island.Severe Tropical Cyclone Neville http://www.bom.gov.au/cyclone/history/neville.shtml Australian Bureau of Meteorology 14 August 2012 Severe Tropical Cyclone Jane-Irna Aus Jane Apr 13 1992 2115Z.png Jane-Irna 1992 path.png 8 April 17 April 100 95 930 On 7 April, TCWC Perth started to monitor a tropical low that had developed, within the monsoon trough about 600 km mi on 5 to the northeast of the Cocos Island. Over the next few days the low moved towards the southeast and gradually developed further, before TCWC Perth named it Jane as the low had developed into a category 1 tropical cyclone. Midday on 10 April Jane made its closest point of approach to Cocos Island, passing 200 km mi on away from the island. As the storm continued to track south, it came under the influence of a deep-layer easterly steering flow caused by the presence of a ridge to the south. Jane turned onto a westward track which it maintained for nearly five days. Cyclone Jane continued to intensify under an ideal environment. On 13 April, a well-defined eye appeared on satellite imagery. A day later, the storm reached its peak intensity of 230 km/h mph on, making the storm one of the strongest of the year. Over the ensuing 24 hours, tropical cyclone Jane began to weaken in response to increased vertical wind shear in association with a mid-latitude trough. By 15 April, the eye had become cloud-filled, and at 0000 UTC 16 April, the cyclone began to re-curve to the southeast and subsequently rapidly deteriorated. By 0100 UTC 17 April, Jane was no longer a tropical cyclone. Due to the storm's small size, winds of just 126 km mi on were reported Cocos Island. Therefore, there were no reports of damage or deaths.Severe Tropical Cyclone Jane http://www.bom.gov.au/cyclone/history/jane.shtml Australian Bureau of Meteorology 14 August 2012 Other system During 19 February, TCWC Brisbane and the JTWC started to monitor a tropical low that had developed within the Coral Sea about 670 km mi 5 on to the northeast of Rockhampton in Queensland Australia.http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1992/1992s-bsh/bsh181992.txt https://web.archive.org/web/20120917022914/http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1992/1992s-bsh/bsh181992.txt dead 17 September 2012 Tropical Cyclone 18P best track analysis Joint Typhoon Warning Center United States Navy, United States Air Force Naval Pacific Meteorology and Oceanography Center 6 January 2013Darwin Regional Specialised Meteorological Centre 1992 February 1992 Darwin Tropical Diagnostic Statement 2–3 1321-4233 Australian Bureau of Meteorology 11 3 6 January 2013 http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199202.pdf During that day, the low gradually developed further as it moved towards the southeast and an anticyclonically curved upper level jet stream, before during the JTWC reported that the low had become equivalent to a tropical storm and assigned it the designation 18P.South East Queensland Floods February 1992 1992 Australian Bureau of Meteorology http://www.bom.gov.au/qld/flood/fld_reports/South_East_Queensland_Floods_February_1992.pdf Queensland Regional Office 29 October 2013 https://web.archive.org/web/20140213093333/http://www.bom.gov.au/qld/flood/fld_reports/South_East_Queensland_Floods_February_1992.pdf 13 February 2014 live 1992 Annual Tropical Cyclone Report United States Navy, United States Airforce http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1992atcr.pdf Joint Typhoon Warning Center 15 September 2012 Naval Western Oceanography Center dead 6 January 2013 240–247 https://web.archive.org/web/20120915165323/http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1992atcr.pdf 1993 However, during the next day despite gale-force winds persisting in the systems southern quadrants, the system moved onto the central Queensland coast, before it could become a tropical cyclone. As a result of the low moving inland, the JTWC issued their final advisory on the system later that day, however, the system continued to be monitored until it was absorbed into the Australian inland heat trough. Season effects |- | Graham || 2–10 December || bgcolor=#A5|Category 5 Severe tropical cyclone || bgcolor=#A5|235 km/h (145 mph) || bgcolor=#A5|915 hPa (27.02 inHg) || None || None || None || None || |- | Mark || 7–10 January || bgcolor=#A2|Category 2 tropical cyclone || bgcolor=#A2|100 km/h (60 mph) || bgcolor=#A2|980 hPa (28.94 inHg) || Northern Territory, Queensland || 3.50 || 3.60 || None || |- | Betsy || 10–14 January || bgcolor=#A3|Category 3 Severe tropical cyclone || bgcolor=#A3|165 km/h (100 mph) || bgcolor=#A3|950 hPa (28.05 inHg) || Vanuatu || Unknown || Unknown || 2 || |- | 16S || 13–13 January || bgcolor=#TD|Tropical depression || bgcolor=#TD|45 km/h (30 mph) || bgcolor=#TD|1004 hPa (29.65 inHg) || None || None|| None || None || |- | Daman || 17–19 February || bgcolor=#A3|Category 3 Severe tropical cyclone || bgcolor=#A3|165 km/h (100 mph) || bgcolor=#A3|965 hPa (28.50 inHg) || New South Wales || Unknown || Unknown || None || |- | 18P || 19–20 February || bgcolor=#TD|Tropical low || bgcolor=#TD|65 km/h (40 mph) || bgcolor=#TD|997 hPa (29.44 inHg) || Queensland || Unknown || Unknown || None || |- | Harriet-Heather || 24 February – 8 March || bgcolor=#A4|Category 4 Severe Tropical Cyclone || bgcolor=#A4|210 km/h (130 mph) || bgcolor=#A4|930 hPa (27.46 inHg) || Western Australia || 0.06 || 0.06 || None || |- | Ian || 27 February – 4 March || bgcolor=#A5|Category 5 Severe tropical cyclone || bgcolor=#A5|210 km/h (130 mph) || bgcolor=#A5|930 hPa (27.46 inHg) || Western Australia || Minimal || Minimal || None || |- | Esau || 29 February – 1 March || bgcolor=#A4|Category 4 Severe tropical cyclone || bgcolor=#A4|185 km/h (115 mph) || bgcolor=#A4|925 hPa (27.32 inHg) || Solomon Islands || Unknown || Unknown || None || |- | Fran || 11–17 March || bgcolor=#A3|Category 3 Severe tropical cyclone || bgcolor=#A3|150 km/h (90 mph) || bgcolor=#A3|950 hPa (28.05 inHg) || Queensland || 10.00 || 10.28 || 5 || |- | Neville || 7–13 April || bgcolor=#A5|Category 5 Severe tropical cyclone || bgcolor=#A5|205 km/h (130 mph) || bgcolor=#A5|945 hPa (27.91 inHg) || Northern Territory, Western Australia|| Minor || Minor || None || |- | Jane-Irna || 8–13 April || bgcolor=#A4|Category 4 Severe tropical cyclone || bgcolor=#A4|210 km/h (130 mph) || bgcolor=#A4|930 hPa (27.46 inHg) || None || None || None || None || |- 12 2 December – 13 April 235 km/h (145 mph) 915 hPa (27.02 inHg) 13.56 million 13.94 million 7 See also Tropical cyclones Tropical cyclones in 1991 and 1992 1991–92 South-West Indian Ocean cyclone season 1991–92 South Pacific cyclone season Atlantic hurricane seasons: 1991, 1992 Pacific hurricane seasons: 1991, 1992 Pacific typhoon seasons: 1991, 1992 North Indian Ocean cyclone seasons: 1991, 1992 References 2 1990 Australian region cyclone yes 1991 y Category:Australian region cyclone seasons Category:Articles which contain graphical timelines