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Australian east coast lows (known locally as east coast lows, maritime lows, and east coast cyclones) are extratropical cyclones or low-pressure systems on the coast of southeastern Australia that may be caused by both mid-latitude and tropical influences over a variety of levels in the atmosphere. These storms should not be confused with Australian region tropical cyclones which typically affect the northern half of the continent.

The most intense of these systems have many of the characteristics of subtropical cyclones. They develop between 25˚ south and 40˚ south and within 5˚ of the eastern Australian coastline, mostly during autumn and early winter with a peak in June. Prior to the introduction of satellite imagery in the early 1960s, many east coast lows were classified as tropical cyclones. ECLs are responsible for more than half of all days with rainfall above 50 mm (2.0 in) in the southeastern seaboard.

Causes

Generally, the low occurs when there exists a temperature contrast between the warmer Tasman Sea and cooler continental landmass (including the cold air in the upper atmosphere), a setup similar to the lake-effect rain. The interaction of such airs create heavy moisture and heightened wind speed. Two thirds of the recorded low-pressure systems are fully cold core storms while the remaining third display hybrid features, which are defined by a warm core at lower levels and a cold core at upper levels. A smaller portion are fully warm core cyclones, where they somehow transition to a tropical cyclone, as well as in part warm seclusion cyclones. Furthermore, 46% of ECLs were hybrid cyclones.

Development

An east coast low can develop in a variety of other weather conditions, including:

• A blocking high in the Tasman Sea which prevents the ECL from leaving the coastline, therefore making the system lengthy and more impactful
• From extropical cyclones, typically in the warm season, which head south
• Sea surface temperature contrasting with the warm eddies that are found on the East Australian Current
• Rapid formation in the sea within a preexistent trough of low pressure
• Much rarely, in the wake of a cold front heading across from Victoria into the Tasman Sea (i.e. a cut-off low originally enclosed within the westerly wind band that flows around the Southern Ocean and is now displaced from the stream).
• A shallow warm core or warm separation at low levels and a cold core in the upper troposphere

Characterisation

Explosive cyclogenesis is seen on average just once per year, but these storms cause significant wind and flood damage when they occur. East Coast Lows by and large have shorter lifespans than Tropical Cyclones, lasting only a few days. Australian east coast cyclones vary in size from mesoscale, around 10–100 km (6–62 mi), to synoptic scale, approximately 100–1,000 km (62–621 mi). Cold core cyclones are more predominant in the southern parts of the ECL region during the cool season, while hybrid cyclones are more regular closer to the tropics, particularly in the warm season.

Australian east coast cyclones, although variable in size and intensity, are typically characterised by widespread heavy rainfall. Rain associated damages attributed to east coast cyclones are estimated in millions to tens of million dollars annually and are a major contributor to the total weather-associated insurance losses for all of Australia. Seven per cent of all major Australian disasters since 1967 can be directly attributed to east coast cyclones.

ECLs are the cause of more than 25% of yearly rainfall and more than 60% of days with mass coastal flooding or significant dam influxes. A Tasman Low is an offshore low that occurs around 200 km away from the coast which can cause light to moderate rainfall and gusty winds, although its effect is insignificant compared to that of an east coast low.

Regions

East coast lows usually occur along the subtropical east coast of Australia from Gladstone in Queensland to the Victoria/New South Wales border in the South Coast (near eastern Gippsland), and often affect large populated cities such as Sydney and Brisbane, between which over one-third of the Australian population resides. ECLs are generally more intense between Batemans Bay in the south to Coffs Harbour in the north, which include the Mid North Coast, Central Coast, Hunter Valley, Sydney CBD, the Illawarra, and as well as the Blue Mountains and Southern Highlands. South East Queensland, the far southern coast and Northern Rivers of New South Wales, and eastern Victoria are generally less impacted than the areas situated at the centre of the NSW coastline.

More powerful systems may percolate inland into the Central Tablelands, New England, the Central West, South Western Slopes, the Monaro and, albeit rarely, the Orana and the Riverina regions in NSW; also the Australian Capital Territory, the Hume region in Victoria; as well as Darling Downs and the Brigalow Belt in Queensland, although the rainfall in these interior areas will often be insignificant.

Pattern

In a June 2007 observation by the Bureau of Meteorology, there were about ten significant maritime lows with an "explosive development" usually occurring once per year. Much recently, it was observed that around 22 east coast lows were recorded annually – around 2 to 3 causing daily rainfall above 100 mm (3.9 in) and 7–8 causing daily rain above 25 mm (0.98 in). A Black nor'easter, which occurs in the warm months in eastern New South Wales, can intensify as it heads south and turn into an east coast low.

The incidence of these types of storms can be seen to fluctuate quite widely from one year to the next, with none in some years and the highest incidence being twelve in 1978/79. Another feature of east coast low development is the tendency for clustering of events when conditions remain favourable. For example, near Brisbane, almost one third of events occur within 20 days of a preceding event. Areas south of the low can experience heavy rain, while those at the north of the rotating low would experience sunny skies. The movement of the low pressure system is generally difficult to predict for weather forecasters.

Correlations of east coast cyclones with the interannual differences of the Southern Oscillation Index (SOI) indicate a strong preference for these storms to form just after a large swing from negative to positive Southern Oscillation index values and especially between swings from negative SOI the year before and positive SOI the year after. This suggests a preference for formation of east coast cyclones between extreme events of the Southern Oscillation Index. A positive SAM is linked with a higher frequency of deep cyclones in August–October and of shallow upper cyclones in December–February.

Examples

• 2022 east coast lows

• 2–7 July 2022. Severe flooding in parts of Western Sydney and the Hunter Region, in addition to 1 death and thousands of evacuations. (See 2022 New South Wales floods)
• 7–8 March 2022. 22 deaths. (See 2022 eastern Australia floods)

• 9–13 June 2021. 2 deaths. Widespread flash flooding across Gippsland in Victoria. 160,000 properties blacked out. Traralgon in the Latrobe Valley was one of the hardest-hit towns with 200 homes evacuated. The rainfall event was actually caused by a cut-off low that "had similar characteristics to an East Coast low".
• 26–28 July 2020.
• 5–6 June 2016 An east coast low combined with a King tide brought severe coastal damage, notably to Collaroy and Coogee, New South Wales along with flooding along the east coast and later severe flooding to Tasmania.

• 2015 Australian east coast lows

• 23–25 August, An unusual low formed late in the season bringing some flooding along the coast. 390 millimetres (15 in) of rainfall was recorded at Nowra in 48 hours.
• 28 April–1 May – On 28 April the Bureau of Meteorology reported that an east coast low was forming off the coast of Fraser Island. Record breaking rainfall and strong winds were recorded in southeast Queensland and northern New South Wales causing 5 fatalities in the Caboolture area.
• 20–23 April At least 4 people died in an event that was described as the worst since 2007. Severe flooding affected the areas of Maitland and Dungog, inundating homes and isolating entire communities. Power and water access was restricted for tens of thousands of homes across the wider Hunter Region.

• 14 October 2014, New South Wales saw wind gusts up to 161 km/h (100 mph). A Bureau of Meteorology spokesman described the rainfall observed at Marrickville, Canterbury, and Sydney Airport as "probably what you'd expect to see in one location about once every 20 years", with rainfall totals in Strathfield at 94 mm (4 in) falling in three hours described as a one in 100 years recurrence. Sydney Airport saw disruption to flights as the airport closed for a time due to high winds. In Port Botany the strong winds caused the Hapag-Lloyd cargo ship Kiel Express to break free. Waves off Sydney over 8 m (26 ft) were reported. 30,000 homes in the region were left without power.
• June 2013
• 21 May 2009, an east coast low caused massive coastal erosion and major flooding of the Clarence River.

• June 2007 June 2007 Hunter Region and Central Coast storms the grounding of the bulk coal-carrying ship MV Pasha Bulker, ten deaths and insurance claims of around A$1.4 billion making it one of the most costly natural disasters in Australia's history. 2007 saw five east coast cyclones develop off Australia's east coast.
• 9 July 2005
• 23 March 2005
• 2 October 2004, off Sydney
• 27–28 July 2001
• 27–28 December 1998, a notorious case of explosive development in eastern Australia, the Sydney–Hobart yacht race cyclone resulted in the death of six race participants.
• 7–8 August 1998, parts of Sydney and the Illawarra region received in excess of 300 mm (12 in) of rain over four days.
• 30–31 August 1996, cost at least two lives and caused almost A$20 million in damage. Heavy rain and strong to gale-force winds with extreme gusts of 64 kn (119 km/h; 74 mph) at Wollongong and 53 kn (98 km/h; 61 mph) near Sydney Airport.
• September 1995, A$8 million damage.
• August 1990, two lows in early August cause A$12 million damage.
• 5 August 1986, 24-hour rainfall totals: over 300mm in the Sydney area. Sydney's Observatory Hill recorded 327.91 mm (12.91 in) of rain, an all-time daily record for the location.
• 17–23 July 1984, A$53m insurance costs.
• 26 May 1974, storm saw the shipwreck of the MV Sygna.
• 6 July 1973, the cargo ship Cherry Venture ran aground on Teewah Beach in South East Queensland during the storm.
• June 1967, a series of east coast cyclones had a major impact on the northern New South Wales and southern Queensland coasts.
• June 1950, a series of east coast cyclones develop off the New South Wales coast during which Sydney registered its highest monthly rainfall on record, 642.7 mm (25.3 in).
• 20 August 1857, the Dunbar sunk near Sydney, with only one survivor.

See also

• East Australian Current
• Southerly buster
• Severe storms in Australia
• Black nor'easter
• Severe storm events in Sydney
• Cold-core low

References

1. ^ Leslie, Lance M.; Speer, Milton S. (1998). "Short-Range Ensemble Forecasting of Explosive Australian East Coast Cyclogenesis". Weather and Forecasting. 13 (3): 822–832. Bibcode:1998WtFor..13..822L. doi:10.1175/1520-0434(1998)013<0822:SREFOE>2.0.CO;2.
2. Dowdy, Andrew J.; Graham A. Mills; Bertrand Timbal; Yang Wang (February 2013). "Changes in the Risk of Extratropical Cyclones in Eastern Australia". Journal of Climate. 26 (4): 1403–1417. Bibcode:2013JCli...26.1403D. doi:10.1175/JCLI-D-12-00192.1.
3. ^ East coast lows and climate change in Australia The Earth Systems and Climate Change Hub
4. ^ Harper, Bruce; Ken Granger (2000). "Chapter 5: East coast low risks" (PDF). In K. Granger & M. Hayne (ed.). Natural hazards and the risks they pose to South-East Queensland. Australian Geological Survey Organisation in conjunction with Bureau of Meteorology. ISBN 0642467080. Retrieved 7 April 2013.
5. ^ Dowdy, Andrew J.; Mills, Graham A.; Timbal, Bertrand (2011). "Large-scale indicators of Australian East Coast Lows and associated extreme weather events" (PDF). In Day K. A. (ed.). CAWCR technical report; 37. CSIRO and the Bureau of Meteorology. ISBN 978-1-921826-36-8. Archived from the original (PDF) on 11 April 2013. Retrieved 7 April 2013.
6. East coast lows Bureau of Meteorology
7. ^ Holland, Greg J.; Lynch, Amanda H.; Leslie, Lance M. (1987). "Australian East-Coast Cyclones. Part I: Synoptic Overview and Case Study". Monthly Weather Review. 115 (12): 3024–3036. Bibcode:1987MWRv..115.3024H. doi:10.1175/1520-0493(1987)115<3024:AECCPI>2.0.CO;2.
8. ^ Lim, Eun-Pa; Simmonds, Ian (2002). "Explosive Cyclone Development in the Southern Hemisphere and a Comparison with Northern Hemisphere Events". Monthly Weather Review. 130 (9): 2188–2209. Bibcode:2002MWRv..130.2188L. doi:10.1175/1520-0493(2002)130<2188:ECDITS>2.0.CO;2.
9. ^ Intense east coast lows and associated rainfall in eastern Australia Journal of Southern Hemisphere Earth Systems Science, 2021, 71, 110–122. CSIRO PUBLISHING. Acacia Pepler and Andrew Dowdy
10. ^ Know your lows: East Coast Lows (and lookalikes) Bureau of Meteorology. 22 May 2019.
11. ^ Review of Australian east coast low pressure systems and associated extremes NESP climate.com.au
12. ^ "About East Coast Lows". Bureau of Meteorology. Retrieved 6 April 2013.
13. What is an east coast low? By Kate Doyle from ABC Weather. 7 February 2020. Retrieved 2 July 2022.
14. ^ "Australian East Coast Storm 2007: Impact of East Coast Lows". Guy Carpenter. October 2007. Retrieved 7 April 2013.
15. ^ Hopkins, Linda C.; Holland, Greg J. (1997). "Australian Heavy-Rain Days and Associated East Coast Cyclones: 1958–92". Journal of Climate. 10 (4): 621–635. Bibcode:1997JCli...10..621H. doi:10.1175/1520-0442(1997)010<0621:AHRDAA>2.0.CO;2.
16. Hunter Valley weather: Sydney evacuation orders as east coast low, flood warnings span Newcastle to Batemans Bay by Newcastle Herald. July 3 2022
17. BOM warns of more wet weather, dangerous conditions as east coast low looms off NSW By Kate Doyle, ABC Weather. 2 March 2022.
18. "Sydney floods: residents brace for another day of devastating weather as NSW coast battered by rain". The Guardian. 3 July 2022. Retrieved 4 July 2022.
19. "Severe thunderstorms expected and potential flooding for south-east Queensland". Bureau Of Meteorology. 2 March 2022. Retrieved 5 March 2022.
20. "Flood warnings and wild weather alert as east coast low hits Victoria". ABC News. 9 June 2021. Retrieved 9 June 2021.
21. "Clean-up begins in Victoria after homes destroyed, towns cut off during storm". Nine News. 11 June 2021. Retrieved 11 June 2021.
22. "Woman's body found in floodwater as Victoria's storm toll rises, further rain expected overnight". ABC News. Australian Broadcasting Corporation. 11 June 2021. Retrieved 11 June 2021.
23. Thomson, Stuart (28 July 2020). "Your pics of the east coast low hitting the Shoalhaven". South Coast Register. Retrieved 2 November 2021.
24. "Weather warning: Heavy rain brings flooding, strong winds and dangerous surf". ABC News. 5 June 2016. Retrieved 8 June 2016.
25. "Sydney homes evacuated as king tide combines with east coast low". ABC News. 5 June 2016. Retrieved 16 June 2016.
26. Higgins, Kate (25 August 2015). "NSW weather: Severe east coast low hitting late in season, meteorologist says". ABC. Retrieved 26 August 2015.
27. Hannam, Peter (24 August 2015). "Sydney weather: City to sit on 'edge' of unusual east coast low". Sydney Morning Herald. Retrieved 26 August 2015.
28. "Nowra daily temperature and rain summaries". Weatherzone. 2 September 2015. Retrieved 2 September 2015.
29. "Weather forecast for Sydney and NSW". News.com.au. 27 April 2015. Retrieved 2 May 2015.
30. "Queensland weather: Three people killed in car washed off flooded road; storm moves into northern NSW - ABC News (Australian Broadcasting Corporation)". ABC News. Abc.net.au. 30 April 2015. Retrieved 2 May 2015.
31. "NSW wild weather: Three killed, homes washed away in Dungog as 'cyclonic' winds batter Sydney, Hunter and Central Coast - ABC News (Australian Broadcasting Corporation)". Abc.net.au. 21 April 2015. Retrieved 2 May 2015.
32. "Three dead as severe storms hit New South Wales in Australia". BBC News. 20 April 2015. Retrieved 21 April 2015.
33. "East coast low cause of wild NSW weather". Sky News. 15 October 2014. Archived from the original on 18 October 2014. Retrieved 18 October 2014.
34. Hannam, Peter. "'Once every 100 years': what made the Sydney storm so ferocious". No. 15 October 2014. The Sydney Morning Herald. Retrieved 18 October 2014.
35. "Snow, winds and floods — chaos from city to mountains". news.com.au. 16 October 2014. Retrieved 18 October 2014.
36. Guerit, Charlie (2 July 2013). "East coast low caused the flooding rains". Milton Ulladulla Times. Archived from the original on 4 March 2016. Retrieved 7 July 2013.
37. "SES issues flash flooding warning for NSW coast". ABC News. 22 June 2013. Retrieved 7 July 2013.
38. Mills, Graham A.; Rob Webb; Noel E. Davidson; Jeffrey Kepert; Alan Seed; Deborah Abbs (2010). "The Pasha Bulker east coast low of 8 June 2007" (PDF). CAWCR Technical Report No. 023. The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology. ISBN 978-1-921605-77-2. Archived from the original (PDF) on 11 April 2013. Retrieved 8 April 2013.
39. "June 2007 East Coast Lows". Bureau of Meteorology. Retrieved 6 April 2013.
40. "Severe weather likely for south-east NSW and eastern Victoria at the weekend". Bureau of Meteorology. Retrieved 6 April 2013.
41. "broken link". Bureau of Meteorology. Retrieved 6 April 2013.
42. ^ "When were most recent major East Coast Lows?". Bureau of Meteorology. Retrieved 6 April 2013.
43. Erdman, Jon (22 April 2015). "Australia Storm Hammers Sydney, New South Wales; 3 Dead, Hundreds Evacuated as Flooding Washes Away Homes". The Weather Channel. Retrieved 26 April 2015.

External links

• #AskBOM, What is an East Coast Low?
• East-coast lows
• NSW Climatedogs: Eastie, East Coast Low
• ARCHIVE: Known Impacts of East Coast Lows, 1846 – 2009, detailed list of events by Jeff Callaghan for Green Cross Australia.

v t e Extratropical cyclones
Concepts	Anticyclonic storm Storm Cyclone Post-tropical cyclone Low-pressure area Weather bomb Sting jet List Rainband
Northern Hemisphere	North America Continental Lee Cyclone Alberta clipper Colorado low Great basin low Bighorn Low Other Panhandle hook November gale Oceanic Aleutian Low Hatteras low Nor'easter Gulf low Pacific Northwest windstorm Europe v t e European windstorms 14th-18th century Grote Mandrenke Burchardi flood Great Storm of 1703 Christmas Flood of 1717 19th century Great Storm of 1824 Night of the Big Wind Moray Firth fishing disaster Tay Bridge disaster Eyemouth disaster 20th century Ulysses 1903 Iberia 1941 North Sea flood of 1953 Debbie 1961 Great Sheffield Gale of 1962 1968 Scotland storm Quimburga 1972 Gale of January 1976 December 1981 windstorm Charley 1986 Great storm of 1987 Burns' Day storm 1990 1992 New Year's Day Storm Braer Storm 1993 Lili 1996 Christmas Eve storm 1997 Boxing Day Storm of 1998 Anatol 1999 Lothar 1999 Martin 1999 21st century Oratia 2000 Jeanett 2002 Gudrun 2005 Per 2007 Kyrill 2007 Emma 2008 Klaus 2009 Xynthia 2010 Berit 2011 Friedhelm/Bawbag 2011 Joachim 2011 Dagmar 2011 Andrea 2012 St Jude 2013 Xaver 2013 Dirk 2013 Anne 2014 Christina 2014 Tini 2014 Niklas 2015 Egon 2017 Thomas (Doris) 2017 Zeus 2017 Xavier 2017 Ophelia 2017 Herwart 2017 Eleanor (Burglind) 2018 Friederike (David) 2018 Adrian 2018 Ciara 2020 Dennis 2020 Aurore 2021 Malik 2022 Eunice 2022 Larisa 2023 Babet 2023 Ciarán 2023 Darragh 2024 See also List of European windstorms List of atmospheric pressure records in Europe Other Black Sea storms Icelandic Low Genoa low Asia Asiatic Low Western Disturbance Continental North Asian storms East Asian-northwest Pacific storms Other areas Arctic Kona storm
Southern Hemisphere	Australia Australian east coast low Black nor'easter Other areas Southern Ocean cyclone Sudestada

v t e Cyclones and anticyclones of the world (Centers of action)
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Cyclone	Synoptic scale Surface-based Polar North Polar low South Polar low v t e Extratropical cyclones Concepts Anticyclonic storm Storm Cyclone Post-tropical cyclone Low-pressure area Weather bomb Sting jet List Rainband Northern Hemisphere North America Continental Lee Cyclone Alberta clipper Colorado low Great basin low Bighorn Low Other Panhandle hook November gale Oceanic Aleutian Low Hatteras low Nor'easter Gulf low Pacific Northwest windstorm Europe v t e European windstorms 14th-18th century Grote Mandrenke Burchardi flood Great Storm of 1703 Christmas Flood of 1717 19th century Great Storm of 1824 Night of the Big Wind Moray Firth fishing disaster Tay Bridge disaster Eyemouth disaster 20th century Ulysses 1903 Iberia 1941 North Sea flood of 1953 Debbie 1961 Great Sheffield Gale of 1962 1968 Scotland storm Quimburga 1972 Gale of January 1976 December 1981 windstorm Charley 1986 Great storm of 1987 Burns' Day storm 1990 1992 New Year's Day Storm Braer Storm 1993 Lili 1996 Christmas Eve storm 1997 Boxing Day Storm of 1998 Anatol 1999 Lothar 1999 Martin 1999 21st century Oratia 2000 Jeanett 2002 Gudrun 2005 Per 2007 Kyrill 2007 Emma 2008 Klaus 2009 Xynthia 2010 Berit 2011 Friedhelm/Bawbag 2011 Joachim 2011 Dagmar 2011 Andrea 2012 St Jude 2013 Xaver 2013 Dirk 2013 Anne 2014 Christina 2014 Tini 2014 Niklas 2015 Egon 2017 Thomas (Doris) 2017 Zeus 2017 Xavier 2017 Ophelia 2017 Herwart 2017 Eleanor (Burglind) 2018 Friederike (David) 2018 Adrian 2018 Ciara 2020 Dennis 2020 Aurore 2021 Malik 2022 Eunice 2022 Larisa 2023 Babet 2023 Ciarán 2023 Darragh 2024 See also List of European windstorms List of atmospheric pressure records in Europe Other Black Sea storms Icelandic Low Genoa low Asia Asiatic Low Western Disturbance Continental North Asian storms East Asian-northwest Pacific storms Other areas Arctic Kona storm Southern Hemisphere Australia Australian east coast low Black nor'easter Other areas Southern Ocean cyclone Sudestada Subtropical Kona storm Australian east coast Low Lake Huron cyclone Mediterranean tropical-like cyclone Thermal Tropical (Outline) Northern Hemisphere Atlantic hurricane Cape Verde hurricane Pacific hurricane Typhoon North Indian Ocean tropical cyclone Mediterranean tropical-like cyclone Black Sea tropical-like cyclone Southern Hemisphere South-West Indian Ocean tropical cyclone Australian region tropical cyclone South Pacific tropical cyclone South Atlantic tropical cyclone Upper level Cold-core low Cut-off low Polar vortex Upper tropospheric cyclonic vortex Mesoscale Mesoscale ocean eddies Catalina eddy Haida Eddies Mesoscale convective system Wake Low Mesohigh Mesoscale convective vortex Line echo wave pattern Whirlwind Major Mesocyclone Supercell Low-topped supercell Wall cloud Funnel cloud Tornado Multiple-vortex tornado Satellite tornado Anticyclonic tornado Landspout Waterspout Minor Gustnado Dust devil Steam devil Fire whirl
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