| 1910s Australian region cyclone seasons | |
|---|---|
| Seasonal boundaries | |
| First system formed | 1910 |
| Last system dissipated | 1920 |
| Seasonal statistics | |
| Total fatalities | Unknown |
| Total damage | Unknown |
 |
| 1910s Australian region cyclone seasons | |
|---|---|
| Seasonal boundaries | |
| First system formed | 1910 |
| Last system dissipated | 1920 |
| Seasonal statistics | |
| Total fatalities | Unknown |
| Total damage | Unknown |
|
A cyclone hit Queensland, Australia near the city of Cairns. [1]
On 19 November 1910, a cyclone touched land in Western Australia when it had a minimum pressure of 965 hPa. [2] It passed directly over Broome, where there was much damage. Twenty six boats of the pearling fleet were sunk and 40 people died. [3]
A long-lived weak cyclone formed in the Gulf of Carpentaria on 3 January, and made landfall with a pressure of 996 hPa. [2] [1]
On 4 January 1911 a cyclone affected the Pilbara coast between Cossack and Onslow. The steel-hulled sailing ship Glenbank was wrecked off Legendre Island with the loss of all but one of its crew. The cyclone crossed near Mardie Station where nearly every outbuilding was levelled to the ground and 6000-gallon tanks were blown away. [4]
This cyclone affected Queensland. [2]
Cyclone 5 crossed the Cape York Peninsula.
This cyclone approached the Queensland coast near Townsville, Australia, but took a sharp turn away from the coast on 22 March.
The cyclone came ashore between Cape Upstart and Cape Bowling Green. The ship Yongala was completely destroyed, with the loss of all 120 people on board. [5]
This cyclone crossed the coast just west of Balla Balla near Port Hedland and claimed well over 150 lives. It is almost certainly Australia's worst weather-related maritime disaster since Federation with the loss of the coastal steamer Koombana.Trove – Archived webpage [4]
| Precipitation | Storm | Location | Ref. | ||
|---|---|---|---|---|---|
| Rank | mm | in | |||
| 1 | 1,947 | 76.65 | Peter 1979 | Mount Bellenden Ker | [6] |
| 2 | 1,870 | 73.62 | Rona 1999 | Mount Bellenden Ker | [6] |
| 3 | 1,318 | 51.89 | Wanda 1974 | Mount Glorious | [7] |
| 4 | 1,256.8 | 49.48 | Fletcher 2014 | Kowanyama | [8] [9] |
| 5 | 1,082 | 42.60 | Aivu 1989 | Dalrymple Heights | [10] |
| 6 | 1,065 | 41.93 | May 1998 | Burketown | [11] |
| 7 | 1,000 | 39.37 | Justin 1997 | Willis Island | [12] |
| 7 | 1,000 | 39.37 | Ellie 2009 | [13] | |
| 7 | 1,000 | 39.37 | Oswald 2013 | Tully | [14] |
| 8 | 986 | 38.82 | Debbie 2017 | Clarke Range | [15] |
The 1918 Mackay cyclone struck the city of Mackay, Queensland, Australia on 20–21 January 1918. [16] It remains one of the most destructive cyclones to strike a populated centre in Australia.
The eye of the storm passed to the north of the city just after sunrise on 21 January. During the height of the storm, barometric pressure was recorded at 932.6 hPa, one of the lowest recordings in Australia. However, the pressure was probably a lot lower, as the barometer would not go beyond 932.6 hPa, and the eye of the storm did not cross directly over Mackay where the measurement was taken. The meteorologist at the time stated that the barometer was at its maximum low reading for at least 30 minutes before the cyclone moved inland and away, allowing the pressure to finally rise. Few buildings in the centre of Mackay escaped without significant structural damage. The accompanying storm surge resulted in a sea-level-rise of 2.36 metres above the highest spring tide level, with one witness later recalling waves of 2–3 metres breaking in the main street.
Communication links into Mackay were destroyed. The outside world did not learn of the Mackay cyclone until five days after impact, leading to some speculation the city had been completely destroyed.
Record amounts of rainfall were recorded in Mackay, the totals to 9 a.m. are as follows:
The rainfall resulted in the Pioneer River's highest flood level at the time, which took 2 weeks to subside.
Damage wasn't limited to Mackay. In Rockhampton, over 350 km south of Mackay, houses lost their roofs and solid jacaranda trees were uprooted. Extensive structural damage was also reported in Yeppoon and Mount Morgan. Rainfall associated with the cyclonic system was responsible for the big Rockhampton Flood of 1918 in February.
A total of thirty people perished in the disaster, including two in Rockhampton and another in Yeppoon.
The 1918 Innisfail cyclone made landfall in the area around Innisfail, Queensland, Australia on 10 March 1918. It was more severe than the earlier Mackay storm. Only 12 houses survived being unroofed or totally destroyed. Damage was also sustained in Cairns, 100 km to the north, and inland to the Atherton Tableland. A 3.6m storm surge was experienced to the south at Mission Beach. 37 people were killed in Innisfail, and an estimated 40 to 60 more in outlying areas. The lowest pressure recorded was 926hPa, but again, damage to recording equipment meant that no accurate minimum for the storm's center survived. Estimates place the figure below 910hPa. [17]
Following this destruction, the area experienced a period of prosperity in the local agricultural industries. This led to the construction of many buildings in a grand art-deco style.
Innisfail is a regional town and locality in the Cassowary Coast Region, Queensland, Australia. The town was originally called Geraldton until 1910. In the 2016 census, the town of Innisfail had a population of 7,236 people, while the locality of Innisfail had a population of 1,145 people.
Severe storms in Australia refers to the storms, including cyclones, which have caused severe damage in Australia. For comparison, a comprehensive list of all damaging storms can be found on the Australian Bureau of Meteorology website.
Severe Tropical Cyclone Larry was a tropical cyclone that made landfall in Australia during the 2005–06 Southern Hemisphere tropical cyclone season. Larry originated as a low pressure system over the eastern Coral Sea on 16 March 2006, and was monitored by the Australian Bureau of Meteorology in Brisbane, Australia. The low-pressure area organized into a tropical cyclone two days later and quickly strengthened into a Category 4 storm on the Australian tropical cyclone scale. Larry made landfall in Far North Queensland close to Innisfail, on 20 March 2006, as a Category 5 tropical cyclone on the Australian scale, with wind gusts reaching 240 kilometres per hour (150 mph), before dissipating over land several days later.
The 1999–2000 Australian region cyclone season was a slightly above average tropical cyclone season. It ran from 1 November 1999 to 30 April 2000. The regional tropical cyclone operational plan also defines a "tropical cyclone year" separately from a "tropical cyclone season", with the "tropical cyclone year" for this season lasting from 1 July 1999 to 30 June 2000.
The 2003–04 Australian region cyclone season was a slightly below average tropical cyclone season. It began on 1 November 2003 and ended on 30 April 2004. The regional tropical cyclone operational plan also defines a tropical cyclone year separately from a tropical cyclone season, which runs from 1 July 2003 to 30 June 2004.
The 1996–97 Australian region cyclone season was an above average tropical cyclone season. It ran from 1 November 1996 to 30 April 1996. 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 1996 to 30 June 1997.
The 2010–11 Australian region cyclone season was a near average tropical cyclone season, with eleven tropical cyclones forming compared to an average of 12. The season was also the costliest recorded in the Australian region basin, with a total of $3.62 billion in damages, mostly from the destructive Cyclone Yasi. The season began on 1 November 2010 and ended on 30 April 2011, although the first tropical cyclone formed on 28 October. The Australian region is defined as being to the south of the equator, between the 90th meridian east and 160th meridian east. Tropical cyclones in this area are monitored by five Tropical Cyclone Warning Centres (TCWC's): Jakarta, Port Moresby, Perth, Darwin, and Brisbane, each of which have the power to name a tropical cyclone. The TCWC's in Perth, Darwin, and Brisbane are run by the Bureau of Meteorology, who designate significant tropical lows with a number and the U suffix. The Joint Typhoon Warning Center also issues unofficial warnings for the region, designating significant tropical cyclones with the "S" suffix when they form west of 135°E, and the "P" suffix when they form east of 135°E.
Severe Tropical Cyclone Rona and Severe Tropical Cyclone Frank were a pair of tropical cyclones that affected Queensland and New Caledonia during the 1998–99 Australian region cyclone season and the 1998–99 South Pacific cyclone season. Rona originated from a low that developed on 9 February about 225 km (140 mi) to the northeast of Cairns. Over the next couple of days, the low slowly developed further before it was upgraded into a Category 1 cyclone on the Australian intensity scale by the Australian Bureau of Meteorology on 10 February as it started to move towards the southwest. Subsequently, Rona rapidly intensified just before making landfall near the Cape York Peninsula. While the low-level circulation became difficult to locate on 12 February, the upper-level circulation eventually emerged into the Coral Sea and later regenerated into Tropical Cyclone Frank. The system rapidly intensified before making landfall on New Caledonia as a Category 2 cyclone on the Saffir-Simpson Hurricane Scale in the early morning hours of 20 February. Frank was re-classified as an extratropical cyclone the next day.
The 1983–84 Australian region cyclone season was the most active season on record. It officially started on 1 November 1983, and officially ended on 30 April 1984.
Severe Tropical Cyclone Aivu was a powerful late-season tropical cyclone that caused extensive damage across parts of Queensland, Australia in April 1989.
Severe Tropical Cyclone Rewa affected six countries and caused 22 deaths on its 28-day journey across the South Pacific Ocean in December 1993 and January 1994. Cyclone Rewa developed from a tropical disturbance on 28 December south of Nauru. After forming, Rewa moved southwest through the Solomon Islands, crossing the 160th meridian east from the South Pacific basin into the Australian region. The cyclone began to strengthen steadily and turned southward, paralleling the eastern Australian coast through 31 December. Rewa reached its initial peak intensity as a Category 4 tropical cyclone on 2 January. It maintained this intensity for about 12 hours before an increase in wind shear induced its weakening by 3 January. The cyclone turned southeastward and moved back into the South Pacific basin on 4 January, before it passed over New Caledonia between 5–6 January. After affecting New Caledonia, Rewa weakened to a tropical depression and turned northwestward before re-entering the Australian basin on 10 January.
The 2013–14 Australian region cyclone season was a slightly below-average tropical cyclone season, with 10 tropical cyclones occurring within the Australian region. It officially started on 1 November 2013, and ended on 30 April 2014. The regional tropical cyclone operational plan defines a "tropical cyclone year" separately from a "tropical cyclone season"; the "tropical cyclone year" began on 1 July 2013 and ended on 30 June 2014.
Severe Tropical Cyclone Joy struck Australia in late 1990, causing the third highest floods on record in Rockhampton, Queensland. This cyclone began as a weak tropical low near the Solomon Islands, and initially moved westward. On 18 December, it was named Joy, becoming the 2nd named storm of the 1990–91 Australian region cyclone season. After turning southwest, Joy developed a well-defined eye and strengthened to maximum sustained winds of 165 km/h (103 mph) while approaching Cairns in Far North Queensland. Brushing the city with strong winds, the cyclone soon weakened and turned southeast. Joy later curved back southwest, making landfall near Townsville, Queensland on 26 December. It dissipated the next day; remnant moisture continued as torrential rainfall over Queensland for two weeks.
Severe Tropical Cyclone Winifred was the worst tropical cyclone to make landfall in northern Queensland and the first since Althea in 1971 to inflict significant damage on the northeastern coast of Australia. The sixth named storm of the 1985–86 Australian region cyclone season, Winifred originated as a tropical low north of Cairns, Queensland on 27 January 1986. Slowly organizing, the system was recognized as a tropical cyclone after gaining tropical characteristics on 30 January, christened with the name Winifred the same day. Meandering southward, the cyclone began to curve southeastward that evening before suddenly turning toward the coast, southwestward, on 31 January, steadily intensifying in that time. By the time it came ashore near Silkwood, Queensland at 0445 UTC on 1 February, it was producing Category 3-force winds on the Australian tropical cyclone intensity scale and a minimum atmospheric pressure of 957 mbar (28.38 inHg). Weakening as it drifted inland, Winifred persisted as a tropical depression for another five days after landfall before finally dissipating on 5 February.
Severe Tropical Cyclone Marcia was a powerful tropical cyclone that made landfall at its peak strength over central Queensland, near Shoalwater Bay on 20 February 2015. The cyclone went on to affect various areas including Yeppoon and Rockhampton. It passed just to the west of Yeppoon as a Category 4 system, then traversed over the regional city of Rockhampton as a Category 2 system on the same day. Eventually, the cyclone weakened, moved southeast out to sea, before dissipating. Marcia caused at least A$750 million (US$587 million) worth of damage.
Cyclone Peter was the wettest tropical cyclone on record in Australia. The third system and first severe tropical cyclone of the 1978–79 season, Peter developed on 29 December from a weak low pressure area over the Gulf of Carpentaria. Peter moved southeastward and deepened while brushing Arnhem Land. Initially a tropical low, it strengthened into a Category 1 cyclone by 12:00 UTC on 29 December. Peter intensified further on 30 December and became a Category 2 cyclone. On the following day, the cyclone peaked with maximum sustained winds of 110 km/h (70 mph). Peter weakened to a Category 1 cyclone before making landfall near the mouth of the Edward River in Queensland. While crossing the Cape York Peninsula, the storm weakened slowly. After reaching Pacific Ocean near Cooktown, the storm decelerated and meandered offshore, but dissipated just offshore on 4 January.
Severe Tropical Cyclone Debbie in 2017 was the strongest tropical cyclone to strike Queensland since Marcia in 2015, and was the costliest tropical cyclone in Australia since Yasi in 2011. Forming as a tropical low on 23 March, the low gradually intensified into a named tropical cyclone on 25 March. After steadily strengthening offshore to a Category 4 system, Debbie eventually made landfall near Airlie Beach, at 12:40 AEST on 28 March. Afterwards, Debbie rapidly weakened into a tropical low by late 28 March, but continued to travel south, causing significant damage and flooding in the populous areas of South East Queensland and Northern Rivers. In total, the storm caused A$3.5 billion (US$2.67 billion) in damage and fourteen deaths across Australia, primarily as a result of extreme flooding. This makes Debbie the deadliest cyclone to hit Australia since Fifi in 1991.
The following is a list of all reported tropical cyclones within the Australian region between 90°E and 160°E, after the start of World War II in September 1939 and before the start of the satellite era during the 1969–70 Season.
The following is a list of Australian region tropical cyclones from 1900 to 1910.