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Southerly buster

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Arrival of a southerly buster inSydney,over theRoyal National Park.

Asoutherly busteris thecolloquialname[1]of an abrupt southerly wind change in the southern regions ofNew South WalesandVictoria,Australia,which approaches from the southeast, mainly on a hot day,bringing in cool,usuallysevere weatherand a dramatic temperature drop, thus ultimately replacing and relieving the prior hot conditions.[2]Marking the boundary between hot and cool air masses, a southerly buster is sometimes represented by aroll-up cloudperpendicular to the coast, which appears from the south and coexists with the wind change, though sometimes there is little visual signal of the southerly's arrival.[3]

Southerly busters occur in the backside of alow pressuretroughin theTasman Sea,followed by the speedy advance of ananticyclonesouth ofWestern AustraliaandSouth Australia(around theGreat Australian Bight). They are caused by the interaction of a shallowcold frontwith the blocking mountain range that aligns the coast, and frictional contrasts over the mainland and the ocean that disconnect the flow.[4]Southerly busters occur about 32 times each year on the coast of southeastern Australia, with variable strength, usually in spring and summer. Although southerly busters are often associated with NSW and Victoria, they also occur on the east coast ofTasmania,New Zealand,and inArgentinaandChile.[5][6]

History

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19th century

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Warning signal showing southerly buster atWollongong
Southerly buster warning signals displayed atGarden Island.
Navy League sea cadets atSchnapper Islandwith signal staff behind.

In 1819, Australian explorerWilliam Wentworthdescribes the southerly buster experienced in Sydney:

...They [hot northwesterly winds] seldom, however, continue for more than two days at a time, and are always superseded by a cold southerly gale, generally accompanied with rain. The thermometer then sinks sometimes as low as 60 °F (16 °C), and a variation of temperature of from 30 to 40 °F (−1 to 4 °C) takes place in half an hour. These southerly gales usually last at this season from twelve to twenty-four hours, and then give way to the regular sea and land breezes...[7]

From the early days of settlement at Sydney Cove, sudden southerly squalls had been a problem for boats in the harbour.[8]In 1829, abrickfielderas these squalls as were then called, laid the boat carrying GovernorRalph Darlingand his family on its beam ends.[9]Later Port Jackson boatmen would call it, the "Sútherly Búster".[10]During the early days of the European settlement, Sydney's summer storms were accompanied by rolling red dust from the colony'sbrickworks.[11]

In 1869, following the connection of lighthouses and signal stations on the east coast of NSW to the electric telegraph network, a system was instituted to give shipping warning of approaching gales.[12]It would give boats in Port Jackson warning of approaching busters. The new signals were included in Gowland's[13]amendments to the NSW Sailing Directory[14]The signal was a diamond shape (seeDay shapes) on the southern yard-arm of the signal mast to indicate a squall approaching from the south, and numeral pendants per John Nicholson's Code of Signals[15]flying on the masthead to show the location of the squall. The numbers were those already in use from 1842 for identifying ports,[16]e.g.Jervis Baywas 46 and Wollongong, added in 1854,[17]was 82. The signal masts were at South Head Signal Station[18]andFort Phillip.These masts had two yard-arms at right angles aligned north–south and east–west. The success of the system was seen in 1870 when a newspaper reported, "About 9 o'clock, however, intelligence of a southerly burster was telegraphed from Eden, and by half-past 12 the expected 'brickfielder' blew over the city."[19]

From 1876 signals would be displayed at two additional places - the new flagstaff at Bradley's Head and the Floating Light Vessel at the entrance to the Harbour.[20]This direction specified that a cone signal on the flagstaff would indicate the approach of a southerly squall. This signal, "A cone, with the point downwards, shows that a gale is probable; at first from the southward.",[21]was introduced in England 1861[22]byRobert Fitzroy,but this appears to be the first time it was used in Port Jackson. In 1879,George Herbert Gibsonpublished a book calledSoutherly Busters,where a buster wreaks havoc nearHyde Park, Sydney.

In November 1898, the Postmaster General,Varney Parkes,[23]announced that a white flag with the letters E, J.B. or W would be flown from the flagstaff on the clock tower of theGeneral Post Office, Sydneyto signal the approach of a southerly buster. As the wind reachedEden,Jervis Bay or Wollongong the relevant flag would be hoisted.[24]The J.B. flag was hoisted for the first time on 10 February 1899 but the wind did not travel beyondKiama.[25]The day had been hot and oppressive and the much anticipated cool change did not eventuate. The original intention was to change the flags as the change moved north but this did not always happen.[26]It was possibly later reduced to just two flags, JB and W.[27]

20th century

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On the night of 16 December 1908 a new signal, also on the GPO clock tower, made its debut.[28]For warnings at night a red light had been installed in the lantern - the glass enclosed room below the flagstaff. It continued until 1940.[29]Capsizes still occurred,[30][31]but fishing boats did heed the warnings.[32]

In 1931, with the addition of signals for southerly busters, the practice of displaying theBureau of Meteorologyweather forecast with flags was extended, with the cooperation of theRoyal Australian Navy,to the signal staff on Garden Island.[33]The weather flags had been flown since 1912[34]from the flagstaffs on prominent buildings but as well, at Garden Island, a diamond shape would be hoisted for warnings during the day and a red light at night when a southerly buster was expected. In 1932 Navy League sea cadets flew the same signals as at Garden Island at their station onSnapper Island (New South Wales).[35]

A sailingskiffduring an afternoon sea breeze in theSydney Harbour

TheWeather beaconon the top ofMLC Building, North Sydney,built in 1957, could also warn of 'southerly busters'. Generally, the forecasts displayed by the lights were updated three times a day but could be changed at anytime if a sudden change was imminent. If a 'buster' was expected the red lights at the bottom of the beacon would flash at half second intervals.[36]This signal, indicating strong winds and rain, was not specific to 'southerly busters', but as the jingle advised:[37]

Flashes short, prepare for gales, Gather the washing, furl the sails. "

AuthorRuth Parkmakes a reference to the southerly buster in her novelPoor Man's Orange(1949):[11]

After an unbearably hot day, the old men on the balconies were sniffing the air and saying, 'Here she comes!' The Southerly Buster, thegenieof Sydney, flapped its coarse wing over the city... The women undid the fronts of their frocks and the little children lifted up their shirts and let it blow on their sweaty bottoms.

Formation

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For a southerly buster to occur, acold frontapproaching the southeast of Australia should lie between twohigh pressure systems;one in theTasman Seaandthe otherin theGreat Australian Bight.[38]

On a hot day, a strong offseagaledevelops from the south usually in the late afternoon and early evening, causing a rapid fall in temperature as it arrives, and sometimes a short rain and/orthunderstormmay accompany, especially if it is affiliated with acold frontcoming from the south and atrough,with the strongest winds being at the leading edge of the buster. The southerly buster, which usually trails a thick layer of lowstratus cloudsbringing episodic drizzle, banks up against theGreat Dividing Range,thus resulting in the transmission of the cool maritime air near the southeastern part of the ranges and the blocking of the airflow on the mountains' west side. The Buster progresses into a strongly stableboundary layerwith warm, prefrontal landmass air that is between 100 and 200 metres deep transporting over the cooler waters.[39][40]

In some occasions, a cold front in theSouthern Oceanmay interact with the Great Dividing Range and develop into a Southerly Buster. It is worth noting that some Southerly Busters are not southern ocean fronts, as they have developed on the pre-frontal trough south of Australia or have possibly originated on the southern NSW coast in affiliation with a shallowmesoscalelow development. As the Southerly Buster advances to the north, its force would decrease, though in rare occasions it can fortify north of theHunter Valleydue to upslope motion on the valley's north, which allows the flow to produceanticyclonicvorticityakin to the original obstruction and arrangement of the Southerly Buster in Victoria.[41]

However, the southerly buster does not always create precipitation, aside from lightdrizzleand light rain, which tend to occur a day after the southerly buster's arrival as its effects may still persist for 24 hours, in addition to creating aweather patternsimilar to that of aJune Gloomexperienced inSouthern California.[42]It is proposed that the southerly buster is basically a coastalgravity currentthat is held against the mountains by theCoriolis forceand in transversegeostrophicbalance, and is generated when a cold front is obstructed, experiencinganticyclonicdistortion near theGreat Dividing Range,spreading northward as a coastal trapped orographic jet.[43]

The southerly buster is caused by its interaction with the Great Dividing Range, as the cool air becomes trapped against the ranges, oftentimes in theGippslandarea of Victoria, where the mountains create achannelling effectas the southerly winds move across the New South Wales coast. When the inland portion of the cold front is held against the mountains, the part over the sea proceeds to move along the shore, twisting the front into an 'S' shape. This activity continues on thesouthern New South Wales coast,while areas leading the front are still experiencing hot northwesterly winds.[44]Other phenomena that lead to the temperature gradient between the warm air mass and the cold density current include; hot north-westerly or warmdry foehn windthat precede the squall. Furthermore, severe thunderstorms may come from the forced elevation of warm, humid air.[4]

Characteristics

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The main distinguishing feature of a southerly buster is the sudden, squally southerly change in wind direction which replace the continental northwesterly winds.[45]This is accompanied by a marked temperature drop andsea level pressurerise. Wind gusts in excess of 40 knots (74 km/h) near ground level averages about three per year, which usually come about after very hot days and would tremendously ease within 30 to 60 minutes after the Buster's arrival, becoming rather light within a few hours. A regular southerly buster is between 20 and 60nautical mileswide, with the heavier winds concentrated on the seaward strip, with its depth being around 1000m, restricted by the height of the mountains to west.[46]

Anorographicjet, the southerly buster is clearly amesoscalephenomenon, developing on about one day. Because busters seldom keep a staunch speed while advancing along the coast, its arrival has always been difficult to foretell, though meteorologists nowadays have the gain ofsatellite imageryandweather radarto foresee it, with wind warning issued by the Bureau of Meteorology. Temperature changes can be dramatic, with falls of 10 to 15 °C (18 to 27 °F) often occurring in a few minutes.[47]In extreme conditions, a southerly buster may lower the temperatures from 40 °C (104 °F) to 19 °C (66 °F).[48][46]To note, some southerly busters can be mild and not very pronounced, where they would arrive on lukewarm days and even during sultry thunderstorm events, bringing in light, though still noticeably cooler winds in the evening, with its affects still remaining in the following few days as well in some cases.[49]

Regions

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  • In New South Wales, southerly busters generally reach their maximum intensity betweenNowrain theSouth CoastandNewcastle,rarely passing beyond theMid North CoastorPort Macquarie– When they do they are usually strengthened by the presence of atropical cycloneoff the north coast of the state. Sydney receives an average of about five Southerly Busters a year, mostly in late spring and early summer, with the stronger ones generally reaching the city in the late afternoon or early evening on a hot day, though at times it would arrive after several days of hot weather. It is a crucial weather feature in the Sydney area, particularly for yachtsmen.[44][50]
  • In Victoria, most notably inMelbourne,southerly busters occur during the afternoons where the domineering heat, brought on by north-westerly winds fromcentral Australia,suddenly gives way to a rapid drop in temperature, followed by rain, thunderstorms and a relatively cool night. They would reach as far inland asSwan Hillin the north andOmeoto the east, but would be less pronounced more inland to the north. Temperature drops in these parts of Victoria are more dramatic than those in the east coast of New South Wales, where a 10 °C (50 °F) drop can occur within half an hour (part of the easily changeable weather).[51]Southerly busters most emerge in spring, as the landmass northbound of Melbourne starts to warm up. Meanwhile, though, theSouthern Ocean,which provides cool breezes to Victoria from the west, does not warm up as swiftly as themainland.As such, the temperature difference between hot air from the north and cold from the ocean would be very great, thus providing good conditions for the formation of thunderstorms.[52]
  • InSouth Australia,Mount Gambierwould the most affected by southerly busters in the state due to its southeasterly location. The buster may also reachAdelaideandWhyallain some occasions.[53]
  • InWestern Australia,the Buster occasionally reachesEucladue to its location near the Southern Ocean in the warm months, where it can experience dramatic temperature drops.[54]
  • InWellington,New Zealand these storms are normally short and frequently have winds gusting between 120 km/h and 160 km/h though higher speeds are known.
  • In South America, these southerly fronts frequently encroach on the southern coast of Chile and Argentina and would then advance northwards on both sides of theAndes.[55]

Records

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The strongest recorded Southerly Buster fell around 4:30 pm on 12 March 2010 inWellington, New Zealand,with a maximum gust recorded of 72 knots (133 km/h; 83 mph).[56]

Artist's impression ofDandenong(right) sinking in Jervis Bay in 1876

Henry Ambrose Huntin "An Essay on Southerly Bursters" included the Dandenong Gale in his list of bursters and wrote "the wind attained, locally, to the abnormal velocity of one hundred and fifty-three miles per hour (246 km/h) in a gust, the rate of one hundred and twelve miles for ten minutes and fifty seven miles per hour for nine hours."[57]The sail-steamerDandenongfoundered off Jervis Bay during the gale with the loss of forty lives.[58]- hence the name of the gale.

This velocity is no longer officially recognised but the 'Kurnell Tornado' in December 2015[59]shows gusts in excess of 200 km/h (120 mph) are possible in the area, and the day before the tornado the possibility of a southerly buster on the following day had been proposed.[60]

Incidents

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On 21 November 2016, at around 6pm, a powerful southerly change occurred in Melbourne, which resulted in the death of 10 people, who wereasthmaticand succumbed torespiratory failure.[61]Thousands of others across the city experiencedallergic reactionsand asthma-like symptomstriggered by the storm.[62]This was due to a stark southerly wind (60 km/hour) that distributedryegrasspolleninto the moist air, rupturing them into very fine specks, small enough particles to enter people's lungs, as they were sucked up into the warm updraft of air forming thestorm cells,before they returned to earth in the storm's cool down-draft, spreading across the land in the storm's efflux area.[63]Hospitals and medical centres in the city had to arduously manage 8,500 emergency calls in the space of just five hours, and the hospitalisation of 1,400 people.[64]

See also

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References

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  1. ^1850, B. C. Peck,Recollections of Sydney,quoted in 1978, G. A. Wilkes,A Dictionary of Australian Colloquialisms,ISBN0-424-00034-2
  2. ^"SOUTHERLY BUSTER".Wellington Times.National Library of Australia. 23 December 1901. p. 2.Retrieved27 March2015.
  3. ^Southerly Busters Explained.The Australian Government Bureau of Meteorology. Accessed 21 February 2012.
  4. ^abSoutherly busterMarine Glossary
  5. ^Naranjo, Ralph (1 December 1994), "Forecasts and false steps. (includes related information on June 1994 Pacific storm)(Safety at Sea)",Cruising World,20(12), Bonnier Corporation: 42,ISSN0098-3519
  6. ^Cassiily, M. 1945. The frontology of sub-tropical Australia.RAAFMet. Services Weather Development and Res. Bulletin. 1. 5–28.
  7. ^Statistical, Historical, and Political Description of NSWby William Charles Wentworth, 1819
  8. ^"SYDNEY".The Sydney Gazette and New South Wales Advertiser.22 December 1805. p. 2.Retrieved26 June2020– via Trove.
  9. ^"INQUESTS".The Australian.9 October 1829. p. 3.Retrieved26 June2020– via Trove.
  10. ^Mundy, Godfrey Charles. Our Antipodes, or, Residence and Rambles in the Australasian Colonies: with a Glimpse of the Gold Fields / by Godfrey Charles Mundy. Richard Bentley, 1852. page 83
  11. ^abArthur Phillip Chapter of Fellowship of First Fleeters – WEATHER SECRETS OF THE FIRST FLEET VOYAGE
  12. ^"TELEGRAPHIC COAST DANGER SIGNALS".New South Wales Government Gazette.16 July 1869. p. 1797.Retrieved3 June2020– via Trove.
  13. ^"Commander Gowlland".Australian Town and Country Journal.22 August 1874. p. 13.Retrieved15 June2020– via Trove.
  14. ^Additions and Corrections to the present Admiralty Sailing Directory for the Coast of New South Wales, Navigating Lieut. J.T.Gowlland R.N., Sydney, Thomas Richards Govt. Printer 1870
  15. ^"Code of Signals for the Colony of New South Wales, 1 January 1832".
  16. ^"SIGNALS AT FORT PHILLIP, FOR VESSELS ARRIVING IN PORT JACKSON".New South Wales Government Gazette.7 January 1842. p. 12.Retrieved3 June2020– via Trove.
  17. ^"LIGHTHOUSE ON MOUILLE POINT".The Sydney Morning Herald.14 September 1854. p. 4.Retrieved11 June2020– via Trove.
  18. ^"South Head Signal Station | the Dictionary of Sydney".
  19. ^Evening News (Sydney, NSW: 1869 - 1931), Friday 14 January 1870, page 2, The Weather
  20. ^"NOTICE TO MARINERS".New South Wales Government Gazette.5 September 1876. p. 3510.Retrieved4 June2020– via Trove.
  21. ^The Weather Book: A Manual of Practical Meteorology, Rear Admiral FITZROY. - London: Longman, Green, Longman, Roberts, & Green. 1 8 6 3.- p. 347
  22. ^Jim Burton. “Robert FitzRoy and the Early History of the Meteorological Office.” The British Journal for the History of Science, vol. 19, no. 2, 1986, p 161. JSTOR, jstor.org/stable/4026590. Accessed 11 June 2020
  23. ^"Parkes, Varney (1859–1935)".Australian Dictionary of Biography.National Centre of Biography, Australian National University.
  24. ^"WINDS THAT BLOW FROM THE SOUTH".The Sydney Morning Herald.22 November 1898. p. 4 Col 6.Retrieved6 June2020– via Trove.
  25. ^"THE WEATHER".The Sydney Morning Herald.11 February 1899. p. 9.Retrieved6 June2020– via Trove.
  26. ^"THE CRITIC".Truth.25 June 1899. p. 1.Retrieved7 June2020– via Trove.
  27. ^H.O Publication No. 169, Australia Pilot, Volume III, 2nd Edition 1930, United States Govt Printing Office
  28. ^"THE RED LIGHT".The Sydney Morning Herald.17 December 1908. p. 7.Retrieved7 June2020– via Trove.
  29. ^"Mrs. ENDACOTT (of Parramatta) wants to know".The Daily Telegraph.27 July 1941. p. 7 (Sunday Telegraph News-Review Section).Retrieved7 June2020– via Trove.
  30. ^"STRONG SOUTHERLY".Sunday Times.8 November 1908. p. 11.Retrieved8 June2020– via Trove.
  31. ^"SAILING".The Sydney Morning Herald.9 February 1921. p. 13.Retrieved8 June2020– via Trove.
  32. ^"IN THE SIGNAL STATION".Evening News.11 October 1906. p. 6.Retrieved8 June2020– via Trove.
  33. ^"WEATHER SIGNALS".The Sydney Morning Herald.7 October 1931. p. 11.Retrieved27 June2020– via Trove.
  34. ^"FLAG-SIGNALLING FORECASTS".The Sydney Morning Herald.17 April 1912. p. 20.Retrieved27 June2020– via Trove.
  35. ^"WEATHER SIGNALS".The Sydney Morning Herald.27 February 1932. p. 17.Retrieved27 June2020– via Trove.
  36. ^"WEATHER BEACON".The Canberra Times.13 March 1957. p. 1.Retrieved9 July2020– via Trove.,
  37. ^"Federation and Meteorology, Weather News, page 1340".
  38. ^Helen J. Reid and Lance M. Leslie School of Mathematics,University of New South Wales,Sydney, Australia
  39. ^Shallow Cold Fronts - Cloud Structure In Satellite Imagesby EUMeTrain
  40. ^Reid, H.J. 2000, "Regeneration of the Southerly Buster of Southeast Australia". Weather and Forecasting Vol.15, pp432-446
  41. ^McInnes K. L., 1993: Australian southerly busters. Part III: The physical mechanism and synoptic conditions contributing to development. Mon. Wea. Rev., 121, 3261 - 3281
  42. ^"Journal of Meteorology".Artetech International. 1995. p. 213.
  43. ^""Southerly Buster" Relieves City ".The Sydney Morning Herald.National Library of Australia. 17 December 1953. p. 1.Retrieved27 March2015.
  44. ^abThe Big Bust - Southerly Busters Explained!- TheBureau of Meteorology
  45. ^1997, Peter Baines, Kathy McInnes, 24. The southerly buster, Eric Kenneth Webb (editor), Windows on Meteorology: Australian Perspective,
  46. ^abBerson, F.A., bid, D.G. and Troup, A.J. 1957. The summer cool change at southeastern Australia. I. General behaviour. Tech. Pap. No. 8. CSIRO Div. of Met. Phys.
  47. ^THE DYNAMICS OF THE SOUTHERLY BUSTER P.G. Baines CSIRO Division of Atmospheric physics, Aspendale, June 1980
  48. ^Storms and showers hit Sydney after a hot week of weatherby Louise Starkey,The Sunday Telegraph
  49. ^Climate Change in the Sydney Metropolitan Catchments
  50. ^Victoria. Ports and Harbors Division (1970),Sailing directions: Victoria including Bass Strait,Government Printer,retrieved27 March2015– page 25 lines 15 – 29... regarding the prevalence of theSoutherly Busterin a widespread area of south-east Australia, and not confined to Sydney.
  51. ^Melbourne weather: Quick change sees temperature slip from sticky to chillyby Emily Woods, Ebony Bowden. 27 March 2017. The Age
  52. ^Melbourne weather: How winds from the north and west create 'change days'by Belinda Smith, Tuesday 13 November 2018
  53. ^Southerly Buster cools southern AustraliabyAl Jazeera,Richard Angwin, 20 November 2012
  54. ^The Register News Pictorial, 1930
  55. ^meteorological reports. 1949. Aviation meteorology of south America. Met. Office Reports, VoI.,1, 1–50.
  56. ^"March 2010 Wellington and Marlborough Storm ( 2010-03-12 )".hwe.niwa.co.nz.Retrieved22 March2020.
  57. ^Three Essays on Australian Weather, Hon Ralph Abercromby, Printer: Frederick W. White, Sydney, 1896.https://archive.org/details/threeessaysonaus00aberuoft
  58. ^"'Dandenong' Gale Took 40 Lives ".Newcastle Morning Herald and Miners' Advocate.6 September 1952. p. 5.Retrieved30 June2020– via Trove.
  59. ^"Media Release - Bureau of Meteorology Newsroom".
  60. ^The Use of Convective Parameters by the Australian Extreme Weather Desk in Forecasting the 16 December 2015 Tornadic Supercell, James TAYLOR, Dean SGARBOSSA, Harald RICHTER, Bureau of Meteorology, Australia
  61. ^Melbourne thunderstorm asthma victims left waiting for ambulances which had not been despatchedby Karen Percy (ABC News)
  62. ^Coronial investigation uncovers tenth thunderstorm asthma deathby Aisha Dow (The Age)
  63. ^Thunderstorm asthma deaths: ambulance dispatch 'unlikely' factor – coronerby Melissa Davey (The Guardian)
  64. ^Inquest into deaths of 10 Victorians from thunderstorm asthma hears common themeby Rohan Smith (News.au)
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