ArticleslgStudy

earth science

Southerly buster

Southerly buster is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Southerly buster rather than just read about it. In short: A southerly buster is the colloquial name of an abrupt southerly wind change in the southern regions of New South Wales and Victoria, Australia, which approaches from the southeast, mainly on a hot day, bringing in cool, usually severe weather and a dramatic temperature drop, thus ultimately replacing and relieving the prior hot conditions. Marking the boundary between hot and cool air masses, a southerly buster is…

Southerly buster — main illustration
Southerly buster — illustration

Key takeaways

  • Southerly buster belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Southerly buster to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Southerly buster from memory before moving on to harder problems.

Reference excerpt

A southerly buster is the colloquial name of an abrupt southerly wind change in the southern regions of New South Wales and Victoria, Australia, which approaches from the southeast, mainly on a hot day, bringing in cool, usually severe weather and a dramatic temperature drop, thus ultimately replacing and relieving the prior hot conditions. Marking the boundary between hot and cool air masses, a southerly buster is sometimes represented by a roll cloud perpendicular 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. Southerly busters occur in the backside of a low pressure trough in the Tasman Sea, followed by the speedy advance of an anticyclone south of Western Australia and South Australia (around the Great Australian Bight). They are caused by the interaction of a shallow cold front with the blocking mountain range that aligns the coast, and frictional contrasts over the mainland and the ocean that disconnect the flow. 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 of Tasmania, New Zealand, and in Argentina and Chile. The name 'southerly buster' initiated as a slang term used by Sydneysiders, though it has since evolved into an official weather attribute in the Bureau of Meteorology terminology. Global warming has decreased their frequency, with falls of 20 °C (36 °F) in minutes being less recorded, where they can disrupt flights, create dangerous sea conditions, and intensify bushfire danger.

History

19th century

In 1819, Australian explorer William Wentworth describes 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 (about 17 to 22°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... From the early days of settlement at Sydney Cove, sudden southerly squalls had been a problem for boats in the harbour. In 1829, a brickfielder as these squalls as were then called, laid the boat carrying Governor Ralph Darling and his family on its beam ends. Later Port Jackson boatmen would call it, the "Sútherly Búster". During the early days of the European settlement, Sydney's summer storms were accompanied by rolling red dust from the colony's brickworks. 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. It would give boats in Port Jackson warning of approaching busters. The new signals were included in Gowland's amendments to the NSW Sailing Directory The signal was a diamond shape (see Day 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 flying on the masthead to show the location of the squall. The numbers were those already in use from 1842 for identifying ports, e.g. Jervis Bay was 46 and Wollongong, added in 1854, was 82. The signal masts were at South Head Signal Station and Fort 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." 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. 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.", was introduced in England 1861 by Robert Fitzroy, but this appears to be the first time it was used in Port Jackson. In 1879, George Herbert Gibson published a book called Southerly Busters, where a buster wreaks havoc near Hyde Park, Sydney. In November 1898, the Postmaster General, Varney Parkes, announced that a white flag with the letters E, J.B. or W would be flown from the flagstaff on the clock tower of the General Post Office, Sydney to signal the approach of a southerly buster. As the wind reached Eden, Jervis Bay or Wollongong the relevant flag would be hoisted. The J.B. flag was hoisted for the first time on 10 February 1899 but the wind did not travel beyond Kiama. 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. It was possibly later reduced to just two flags, JB and W.

20th century On the night of 16 December 1908 a new signal, also on the GPO clock tower, made its debut. For warnings at night a red light had been installed in the lantern - the glass enclosed room below the flagstaff. It continued until 1940. Capsizes still occurred, but fishing boats did heed the warnings. In 1931, with the addition of signals for southerly busters, the practice of displaying the Bureau of Meteorology weather forecast with flags was extended, with the cooperation of the Royal Australian Navy, to the signal staff on Garden Island. The weather flags had been flown since 1912 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 on Snapper Island (New South Wales).

… excerpt ends here. Continue reading the full article.

Illustrations

Southerly buster: Arrival of a southerly buster in Sydney, over the Royal National Park.
Arrival of a southerly buster in Sydney, over the Royal National Park.
Southerly buster: Warning signal showing southerly buster at Wollongong
Warning signal showing southerly buster at Wollongong
Southerly buster: Southerly buster warning signals displayed at Garden Island.
Southerly buster warning signals displayed at Garden Island.
Southerly buster: Navy League sea cadets at Schnapper Island with signal staff behind.
Navy League sea cadets at Schnapper Island with signal staff behind.
Southerly buster: A sailing skiff during an afternoon sea breeze in the Sydney Harbour
A sailing skiff during an afternoon sea breeze in the Sydney Harbour

Worked examples

Example 1 — a first encounter with Southerly buster

Start with the simplest possible case. Write down what Southerly buster claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Southerly buster before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Southerly buster ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Southerly buster

In research
Southerly buster appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Southerly buster in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Southerly buster is common in secondary-school and first-year university syllabi. It links to neighbouring topics Bass Strait, Climate of Australia, Climate of New Zealand, so understanding it makes those chapters shorter.
In everyday life
Look for Southerly buster outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Southerly buster” →

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Southerly buster in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Southerly buster means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Southerly buster out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Southerly buster in simple terms?

A southerly buster is the colloquial name of an abrupt southerly wind change in the southern regions of New South Wales and Victoria, Australia, which approaches from the southeast, mainly on a hot day, bringing in cool, usually severe weather and a dramatic temperature drop, thus ultimately replac…

Why does Southerly buster matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Southerly buster?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Southerly buster.

Tags

  • Bass Strait
  • Climate of Australia
  • Climate of New Zealand
  • Coastline of New South Wales
  • Coastline of Victoria (state)
  • Cold
  • Weather events in Australia
  • Weather fronts
  • Winds

Keep exploring