Australian east coast low explained
Australian east coast lows (known locally as east coast lows, maritime lows, and east coast cyclones[1]) are extratropical cyclones or low-pressure systems on the coast of southeastern Australia thatmay be caused by both mid-latitude and tropical influences over a variety of levels in the atmosphere.[2] [3] These storms should not be confused with Australian region tropical cyclones which typically affect the northern half of the continent.[4]
The most intense of these systems have many of the characteristics of subtropical cyclones.[5] They develop between 25˚ south and 40˚ south and within 5˚ of the eastern Australian coastline,[1] mostly during autumn and early winter with a peak in June.[6] [7] [8] 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 50mm in the southeastern seaboard.[9]
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). 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
- 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).[10]
- A shallow warm core or warm separation at low levels and a cold core in the upper troposphere[11]
Characterisation
Explosive cyclogenesis is seen on average just once per year, but these storms cause significant wind and flood damage when they occur.[7] 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-, to synoptic scale, approximately 100-.[12] [13] 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.[11]
Australian east coast cyclones, although variable in size and intensity, are typically characterised by widespread heavy rainfall.[13] 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.[13] Seven per cent of all major Australian disasters since 1967 can be directly attributed to east coast cyclones.[13]
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.[9] 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.[14]
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.[13] 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.[15]
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.[9]
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.[16] Much recently, it was observed that around 22 east coast lows were recorded annually – around 2 to 3 causing daily rainfall above 100mm and 7–8 causing daily rain above 25mm.[3] 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.[17]
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.[4] 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.[4] 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.[13] A positive SAM is linked with a higher frequency of deep cyclones in August–October and of shallow upper cyclones in December–February.[9]
Examples
- 2015 Australian east coast lows
- 23–25 August, An unusual low formed late in the season bringing some flooding along the coast.[26] [27] of rainfall was recorded at Nowra in 48 hours.[28]
- 28 April–1 May[29] – 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.[30]
- 20–23 April[31] At least 4 people died in an event that was described as the worst since 2007. Severe flooding affected the areas of and, inundating homes and isolating entire communities. Power and water access was restricted for tens of thousands of homes across the wider Hunter Region.[32]
- 14 October 2014, New South Wales saw wind gusts up to 1610NaN0.[33] 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 at 940NaN0 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 80NaN0 were reported.[34] 30,000 homes in the region were left without power.[35]
- June 2013[36] [37]
- 21 May 2009, an east coast low caused massive coastal erosion and major flooding of the Clarence River.[38]
- June 2007[39] June 2007 Hunter Region and Central Coast storms the grounding of the bulk coal-carrying ship, 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.[12]
- 9 July 2005[40]
- 23 March 2005[41]
- 2 October 2004, off Sydney[42]
- 27–28 July 2001[42]
- 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 3000NaN0 of rain over four days.[42]
- 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 64kn at Wollongong and 53kn near Sydney Airport.[1]
- September 1995, A$8 million damage.[1]
- August 1990, two lows in early August cause A$12 million damage.[1]
- 5 August 1986, 24-hour rainfall totals: over 300mm in the Sydney area.[42] Sydney's Observatory Hill recorded 12.91inches of rain, an all-time daily record for the location.[43]
- 17–23 July 1984, A$53m insurance costs.[12]
- 26 May 1974, storm saw the shipwreck of the .[7]
- 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.[12]
- 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, 642.71NaN1.[12]
- 20 August 1857, the Dunbar sunk near Sydney, with only one survivor.[42]
See also
External links
Notes and References
- Leslie. Lance M.. Speer, Milton S.. Short-Range Ensemble Forecasting of Explosive Australian East Coast Cyclogenesis. Weather and Forecasting. 1998. 13. 3. 822–832. 10.1175/1520-0434(1998)013<0822:SREFOE>2.0.CO;2. 1998WtFor..13..822L . free.
- Dowdy. Andrew J.. Graham A. Mills. Bertrand Timbal. Yang Wang. Changes in the Risk of Extratropical Cyclones in Eastern Australia. Journal of Climate. February 2013. 26. 4. 1403–1417. 10.1175/JCLI-D-12-00192.1. 2013JCli...26.1403D. free.
- https://nespclimate.com.au/wp-content/uploads/2019/11/A4_4pp_brochure_NESP_ESCC_East_Coast_Lows_Nov11_2019_WEB.pdf East coast lows and climate change in Australia
- Book: Harper, Bruce. Natural hazards and the risks they pose to South-East Queensland. 2000. Australian Geological Survey Organisation in conjunction with Bureau of Meteorology. 0642467080. http://www.ga.gov.au/image_cache/GA4206.pdf. Ken Granger. K. Granger & M. Hayne. 7 April 2013. Chapter 5: East coast low risks.
- Book: Dowdy. Andrew J.. CAWCR technical report; 37. 2011. CSIRO and the Bureau of Meteorology. 978-1-921826-36-8. http://www.cawcr.gov.au/publications/technicalreports/CTR_037.pdf. Graham A.. Mills. Bertrand. Timbal. Day K. A.. 7 April 2013. Large-scale indicators of Australian East Coast Lows and associated extreme weather events. https://web.archive.org/web/20130411044703/http://cawcr.gov.au/publications/technicalreports/CTR_037.pdf. 11 April 2013. dead.
- http://www.bom.gov.au/weather-services/severe-weather-knowledge-centre/eastcoastlows.shtml#:~:text=East%20Coast%20Lows%20(ECL)%20are,Queensland%2C%20NSW%20and%20eastern%20Victoria. East coast lows
- Holland. Greg J.. Lynch, Amanda H.. Leslie, Lance M.. Australian East-Coast Cyclones. Part I: Synoptic Overview and Case Study. Monthly Weather Review. 1987. 115. 12. 3024–3036. 10.1175/1520-0493(1987)115<3024:AECCPI>2.0.CO;2. 1987MWRv..115.3024H . free.
- Lim . Eun-Pa . Simmonds, Ian . Explosive Cyclone Development in the Southern Hemisphere and a Comparison with Northern Hemisphere Events . Monthly Weather Review . 2002 . 130 . 9 . 2188–2209 . 10.1175/1520-0493(2002)130<2188:ECDITS>2.0.CO;2 . 2002MWRv..130.2188L . free .
- https://www.publish.csiro.au/es/pdf/ES20013 Intense east coast lows and associated rainfall in eastern Australia
- https://www.abc.net.au/news/2020-02-07/what-is-an-east-coast-low-wild-weekend-weather/11936190 What is an east coast low?
- https://nespclimate.com.au/wp-content/uploads/2019/05/2.2-Review-of-Australian-east-coast-low-pressure-systems-pre-print.pdf Review of Australian east coast low pressure systems and associated extremes
- Web site: Australian East Coast Storm 2007: Impact of East Coast Lows. Guy Carpenter. 7 April 2013. October 2007.
- Hopkins. Linda C.. Holland, Greg J.. Australian Heavy-Rain Days and Associated East Coast Cyclones: 1958–92. Journal of Climate. 1997. 10. 4. 621–635. 10.1175/1520-0442(1997)010<0621:AHRDAA>2.0.CO;2. 1997JCli...10..621H . free.
- https://media.bom.gov.au/social/blog/2140/know-your-lows-east-coast-lows-and-lookalikes/ Know your lows: East Coast Lows (and lookalikes)
- https://www.newcastleherald.com.au/story/7804678/sydney-evacuation-orders-as-warning-spans-newcastle-to-batemans-bay/ Hunter Valley weather: Sydney evacuation orders as east coast low, flood warnings span Newcastle to Batemans Bay
- Web site: About East Coast Lows. Bureau of Meteorology. 6 April 2013.
- https://www.abc.net.au/news/2022-03-02/more-wet-weather-to-come-as-east-coast-low-forms-off-nsw/100873942 BOM warns of more wet weather, dangerous conditions as east coast low looms off NSW
- Web site: Sydney floods: residents brace for another day of devastating weather as NSW coast battered by rain . 3 July 2022 . The Guardian . 4 July 2022.
- Web site: Severe thunderstorms expected and potential flooding for south-east Queensland . 2 March 2022 . Bureau Of Meteorology . 5 March 2022.
- Web site: Flood warnings and wild weather alert as east coast low hits Victoria . 9 June 2021 . . 9 June 2021.
- Web site: Clean-up begins in Victoria after homes destroyed, towns cut off during storm . . 11 June 2021.
- News: Woman's body found in floodwater as Victoria's storm toll rises, further rain expected overnight . 11 June 2021 . ABC News . Australian Broadcasting Corporation . 11 June 2021 . en-AU.
- Web site: Thomson. Stuart. 2020-07-28. Your pics of the east coast low hitting the Shoalhaven. 2021-11-02. South Coast Register. en-AU.
- Web site: Weather warning: Heavy rain brings flooding, strong winds and dangerous surf . 5 June 2016 . . 8 June 2016.
- News: Sydney homes evacuated as king tide combines with east coast low. 16 June 2016. ABC News. 5 June 2016. en-AU.
- News: Higgins. Kate. NSW weather: Severe east coast low hitting late in season, meteorologist says. 26 August 2015. ABC. 25 August 2015.
- News: Hannam. Peter. Sydney weather: City to sit on 'edge' of unusual east coast low. 26 August 2015. Sydney Morning Herald. 24 August 2015.
- Web site: Nowra daily temperature and rain summaries. Weatherzone. 2 September 2015. 2 September 2015.
- Web site: Weather forecast for Sydney and NSW. News.com.au. 27 April 2015. 2 May 2015.
- News: Queensland weather: Three people killed in car washed off flooded road; storm moves into northern NSW - ABC News (Australian Broadcasting Corporation). ABC News . 30 April 2015 . Abc.net.au. 2 May 2015.
- Web site: 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. 2 May 2015.
- News: Three dead as severe storms hit New South Wales in Australia. BBC News. 20 April 2015 . 21 April 2015.
- News: East coast low cause of wild NSW weather . 18 October 2014 . Sky News . 15 October 2014 . dead . https://web.archive.org/web/20141018112958/http://www.skynews.com.au/news/top-stories/2014/10/15/east-coast-low-cause-of-wild-nsw-weather.html . 18 October 2014 .
- News: Hannam. Peter. 'Once every 100 years': what made the Sydney storm so ferocious. 18 October 2014. 15 October 2014. The Sydney Morning Herald.
- News: Snow, winds and floods — chaos from city to mountains. 18 October 2014. news.com.au. 16 October 2014.
- News: Guerit. Charlie. East coast low caused the flooding rains. 7 July 2013. Milton Ulladulla Times. 2 July 2013. dead. https://web.archive.org/web/20160304065509/http://www.ulladullatimes.com.au/story/1611180/east-coast-low-caused-the-flooding-rains/?cs=1480. 4 March 2016.
- News: SES issues flash flooding warning for NSW coast. 7 July 2013. ABC News. 22 June 2013.
- Book: Mills, Graham A.. CAWCR Technical Report No. 023. 2010. The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology. 978-1-921605-77-2. http://www.cawcr.gov.au/publications/technicalreports/CTR_023.pdf. Rob Webb. Noel E. Davidson. Jeffrey Kepert. Alan Seed. Deborah Abbs. 8 April 2013. The Pasha Bulker east coast low of 8 June 2007. https://web.archive.org/web/20130411045307/http://cawcr.gov.au/publications/technicalreports/CTR_023.pdf#. 11 April 2013. dead.
- Web site: June 2007 East Coast Lows. Bureau of Meteorology. 6 April 2013.
- Web site: Severe weather likely for south-east NSW and eastern Victoria at the weekend. Bureau of Meteorology. 6 April 2013.
- Web site: broken link . Bureau of Meteorology . 6 April 2013 .
- Web site: When were most recent major East Coast Lows?. Bureau of Meteorology. 6 April 2013.
- News: Erdman. Jon. Australia Storm Hammers Sydney, New South Wales; 3 Dead, Hundreds Evacuated as Flooding Washes Away Homes. 26 April 2015. The Weather Channel. 22 April 2015.