The 1989–90 Australian region cyclone season was an above average tropical cyclone season. It was also an event in the ongoing cycle of tropical cyclone formation. It ran from 1 November 1989 to 30 April 1990. 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 1989 to 30 June 1990.
| 1989–90 Australian region cyclone season | |
|---|---|
 Season summary map | |
| Seasonal boundaries | |
| First system formed | July 14, 1989 |
| Last system dissipated | April 18, 1990 |
| Strongest storm | |
| Name | Alex |
| • Maximum winds | 220 km/h (140 mph) (10-minute sustained) |
| • Lowest pressure | 927 hPa (mbar) |
| Seasonal statistics | |
| Tropical lows | 14 |
| Tropical cyclones | 14 |
| Severe tropical cyclones | 5 |
| Total fatalities | Unknown |
| Total damage | Unknown |
| Related articles | |
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
Tropical Storm 02S
Tropical Storm 02S existed from July 14 to July 16.
Tropical Cyclone Pedro
At 0:00 UTC on November 6, the BOM detected an area of low pressure within a monsoonal trough near 7.8°S, 97.2°E., which gradually organized while drifting westward for the next couple of days. On November 8, the disturbance strengthened into a tropical cyclone and was named Pedro. The cyclone continued to intensify before reaching its peak intensity at 13:00 UTC on November 10 with 10-minute sustained winds of around 70 mph (110 km/h) and a minimum pressure of 982 mbar (29.0 inHg), with a short-lived eye visible on satellite imagery. As Pedro moved southward, strong vertical wind shear left the low-level center bare and displaced convection to the northwestern side of the storm. At 0:00 UTC on November 13, Pedro's winds weakened below gale-force and the system degenerated into a remnant system, which dissipated the following day.[1]
Pedro passed within 85 miles (137 km)[nb 1] of Cocos Island, where a peak wind gust of around 85 mph (137 km/h) was recorded. At least 7.9 inches (200 mm) of precipitation fell on the island within a 24-hour period, causing localized flooding. A palm plantation and loading wharf were damaged by the storm.[1]
Severe Tropical Cyclone Felicity
On 13 December, the BoM started to monitor a monsoon low, that had developed within the Arafura Sea to the northeast of Darwin.[2] Over the next day, the system moved southeastwards over the Northern Territory, before it re-curved slightly and entered the Gulf of Carpentaria.[2] Early on 15 December, the system was named Felicity by TCWC Brisbane, after it had become a category 1 tropical cyclone on the Australian Scale.[2] During that day the JTWC initiated advisories on the system and designated it as Tropical Cyclone 07P, with peak 1-minute sustained wind speeds of 110 km/h (68 mph).[3] TCWC Brisbane subsequently reported peak 10-minute sustained wind speeds of 110 km/h (68 mph), before the system made landfall over the Cape York Peninsula where it weakened below cyclone intensity.[2] The system subsequently moved into the Coral Sea during 16 December, where it started to rapidly deepen, but did not reattain the classical characteristics of a tropical cyclone.[2][4] As a result, both TCWC Nadi and TCWC Brisbane treated the system as a tropical depression over the next four days despite winds of between 110 and 115 km/h (68 and 71 mph) being observed in the southwest quadrant.[2][4] Felicity subsequently dissipated during 20 December as it was absorbed by a short-wave trough of low pressure to the north of New Zealand.[2][4] Some minor damage to vegetation was recorded on the Cape York Peninsula.[2][4]
Tropical Cyclone Rosita
Rosita was first noted as a low-pressure system at 18:00 UTC on January 4 while it located well south of Java. Moving swiftly westward, the disturbance gradually organized for two days until slightly weakening due to increasing vertical wind shear. The system remained quasi-stationary until January 9 when a developing ridge in the middle-latitudes forced the disturbance northwestward. The low was ill-defined with a weak and sheared structure on satellite imagery while moving equatorward. By 6:00 UTC the following day, convection began to redevelop and consolidate through January 12 as the disturbance strengthened.[5]
At 15:00 UTC on January 13, tropical storm-force winds formed around the center, prompting the BOM to upgrade the low into Tropical Cyclone Rosita. The nascent cyclone tracked south-southeastward, remaining under the influence of vertical wind shear causing majority of convection to be displaced west of the center. Rosita once again changed course late the next day, shifting northwestward as it lost gale-force winds. The remnants tracked around the periphery of the more intense Severe Tropical Cyclone Sam, before moving equatorward and dissipating on January 17.[5]
Severe Tropical Cyclone Sam
Sam, 11 to 21 January 1990, near Western Australia
Tropical Cyclone Tina
Tina, 24 to 29 January 1990, crossed Western Australia
Tropical Cyclone Nancy
In late January, a monsoon trough spawned a tropical depression on 26 January, over the Coral Sea. The depression developed good outflow, before gaining tropical cyclone characteristic on 31 January, and was designated as Tropical Cyclone Nancy. An upper-level trough forced the storm southward, before shifting southwestward. At 3:00 UTC on 1 February, Nancy reached its peak intensity with 10-minute sustained winds of around 60 mph (97 km/h) and a minimum pressure of 975 mbar. Between 1–2 February, the cyclone gradually moved just offshore the Brisbane area. Nancy then weakened while continuing to move southward, before transitioning into an extratropical low on 4 February. The remnants eventually dissipated to the west of New Zealand on 8 February.[6]
Nancy caused flash floods responsible for five fatalities.[7]
Severe Tropical Cyclone Vincent
Vincent, 25 February to 6 March 1990, near Western Australia
Tropical Cyclone Greg
Greg, 28 February to 5 March 1990, Gulf of Carpentaria
Tropical Cyclone Walter–Gregoara
Walter existed from 3 to 27 March 1990.
Tropical Cyclone Hilda
Cyclone Hilda had cloud tops estimated at 19,200 metres (63,000 ft) tall. The measured cloud top temperature was −100 °C (−148 °F) which is the coldest cloud-top temperature ever measured.[8][9] This record lasted until Typhoon Kammuri in 2019 with cloud tops of −109.35 °C (−164.83 °F).[10]
Severe Tropical Cyclone Alex
Alex was a fairly intense system. It existed from 14 to 26 March 1990. Despite the intensity, Alex never caused significant damage.
Severe Tropical Cyclone Ivor
Ivor, 14 to 26 March 1990, crossed Cape York, Queensland
Tropical Cyclone Bessi
Bessi, 11 to 18 April 1990, Indian Ocean
Season effects
| Name | Dates | Peak intensity | Areas affected | Damage (USD) |
Deaths | Refs | ||
|---|---|---|---|---|---|---|---|---|
| Category | Wind speed | Pressure | ||||||
| Rosita | 4 – 17 January 1990 | Category 1 tropical cyclone | 85 km/h (50 mph) | 988 hPa (29.18 inHg) | None | None | None | [11] |
| Tina | 25 – 28 January 1990 | Category 2 tropical cyclone | 95 km/h (60 mph) | 976 hPa (28.82 inHg) | Western Australia | Minor | None | [12] |
| Nancy | 28 January – 4 February 1990 | Category 2 tropical cyclone | 110 km/h (70 mph) | 976 hPa (28.82 inHg) | Queensland, New South Wales, New Zealand | Unknown | Unknown | [13] |
| Greg | 28 February – 5 March 1990 | Category 1 tropical cyclone | 75 km/h (45 mph) | 990 hPa (29.23 inHg) | None | None | None | [14][15] |
| Walter – Gregoara | 3 – 13 March 1990 | Category 2 tropical cyclone | 95 km/h (60 mph) | 985 hPa (29.09 inHg) | None | None | None | [16] |
| Hilda | 4 – 13 March 1990 | Category 2 tropical cyclone | 110 km/h (70 mph) | 970 hPa (28.64 inHg) | New Caledonia | Unknown | Unknown | [17] |
| Bessi | 15 – 18 April 1990 | Category 1 tropical cyclone | 85 km/h (50 mph) | 990 hPa (29.23 inHg) | None | None | None | [18] |
See also
Notes
- This calculation is rounded to the nearest tenth, which is why it may differ from others.
References
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