# Southeast Australian foehn

The southeast Australian foehn is a westerly foehn wind and a rain shadow effect that usually occurs on the coastal plain of southern New South Wales, and as well as in southeastern Victoria and eastern Tasmania, on the leeward side of the Great Dividing Range.
Ranging from cool to hot (depending on the season), the effect occurs when westerly winds descend steeply from the Great Dividing Range onto the coastal slopes, thereby causing major adiabatic compression (the rate at which temperature decreases with altitude) and a substantial loss of moisture. The effect is known by other names, such as the Australian chinook, the Great Dividing wind, the Great Dividing foehn or simply westerly foehn.
Typically occurring from late autumn to spring, though not completely unheard of in the summer (particularly in eastern Tasmania), the foehn effect mainly occurs when a westerly or south-westerly frontal system (which brings rainy and windy weather to southern capitals like Melbourne, Perth and Adelaide) passes over the Great Dividing Range and thereby provides clear to partly cloudy, relatively warmer conditions on the lee.

## Origins

The foehn effect on the coastal plains of southeastern Australia is mostly linked with the passage of a deep low pressure system or westerly cold fronts across the Great Australian Bight and southeastern Australia that cause strong winds to reorient virtually perpendicular to some parts of the Great Dividing Range, predominantly between late autumn into winter and spring, particularly during a negative AAO phase. Their occurrence is owed to the incomplete orographic blocking of comparatively moist low-level air and the subsidence of drier upper-level air in the lee of the mountains.
Foehn occurrence on the southeast coastal plains can also occur when hot, northwesterly winds blow from the interior (even when there is little moisture on the windward side), because the air heats up faster as it descends into the plains than it cooled as it ascended the ranges.
Typically between 60 km/h (37 mph) to 70 km/h (43 mph), sometimes they may be brought on by a large polar air mass from the south-west of the continent in the Southern Ocean which moves east or north-eastward across Victoria towards the east coast. Moreover, temperatures on the lee of the Great Dividing Range tend to rise substantially (due to a katabatic effect) when cold fronts push warm and dry air from the desert across the country's eastern states and over the Range (this is generally followed by a southerly buster).
As such, the Great Dividing foehn is one the few reasons why Sydney, among other places on the coastal plain, registers high temperatures in the warm season but seldom attains cold maximum temperatures in the winter. Furthermore, when the warm season north-westerly winds strike (such as the Brickfielder), the hottest and driest areas of southeastern Australia will generally be located along the southern coastal region of NSW in the lee of the Great Dividing range and coastal escarpment due to the foehn effect. Much lower relative humidity figures would also observed in these leeward stations.

## Formation

The southeast Australian foehn is distinguished by three criteria; surface winds which blow from the mountains' direction, a sharp rise in air temperature in the leeward side of the mountains, and an accompanying diminution in atmospheric moisture.
As the moist air rises over the windward side of the ranges, it cools and it would condense, thereby creating precipitation on the upwind slopes. The precipitation then gets rid of the moisture from the air mass on the lee side of the ranges, and the condensation raises the air temperature as it descends the lee slopes towards the coastal plains because of the adiabatic compression.
During these conditions, an orographic cloud band, or the Föhn wall, builds up along the ridgelines of the southeastern highlands due to condensation of moisture as the air ascends the windward slopes. Meanwhile, the Föhn arch, with its broad layer of altostratus cloud, shapes downwind of the mountains in the ascending component of a standing lee mountain wave. In weather maps, a band of clear air called the Föhn gap, which is over the downwind of the Great Dividing region, can be seen between the wall and arched cloud cover. This foehn wind can be referred to as thermodynamically driven.
The existence of topographically induced atmospheric waves in connection with foehn occurrence has been indicated, which develop with the descent of upper-level air above of the ridgetop and pass into the lee of the ranges as broad-scale, vertically supporting gravity waves. The wind shears and the strength of the downslope motion manifested in the model examination also point that the onslaught of foehn conditions results in increased turbulence near the surface, evident in the gusty conditions observed at the lee stations. In addition to the foehn winds, the same westerly winds also ward off the cooling sea breezes that arrive from the northeast, thereby preventing them from developing in the eastern seaboard.
A vertically propagating gravity wave over the affected region exists. The descending motion over the coastal escarpment is stronger than that over the primary range and is connected with more powerful shear. The downslope winds tend to be strong, particularly near the lee's surface of the coastal escarpment. Smaller-scale, trapped lee waves over the affected region exist, and their incidence, together with the strong wind shears, signal significant turbulence throughout the boundary layer, which is concordant with the heavy gusty surface winds registered on the leeside. At nighttime, the foehn effect subsides due to a mountain breeze – This is when denser cool air flows down the mountain slopes to settle in the downwind side, thereby providing relatively cold conditions in the night and, consequently, a high diurnal range of temperature.

## Occurrence

The Great Dividing foehn is primarily observed in the southeast of New South Wales, east of the Great Dividing Range, in places such as the Sydney metropolitan area (Cumberland Plain), the Illawarra, some areas of the Southern Highlands, parts of the Monaro region, and the South Coast. It can also occur in the Central Coast, Hunter Valley and the Mid North Coast to the north. In many instances, it is observed in the East Gippsland region in Victoria as well as the eastern portion of Tasmania to the south.
Foehn winds may also impact other parts of Australia, such as east of the Great Dividing Range in southeast Queensland and northern New South Wales. The Great Dividing foehn does not heavily impact areas northward from the Central Coast. The effect is gradient; being more common and efficacious towards the South Coast (due to the latter region being in the track of prevailing westerlies, which exponentially falters north of 35° S). With leeward areas, or areas that receive foehn winds, precipitation is predominantly derived from the Tasman Sea to the east, since the Great Dividing Range blocks frontal westerlies off the Southern Ocean (which are most frequent between May and October). Consequently, winters in leeward zones are drier with the summers being relatively wet, unlike those on the windward side which, conversely, have drier summers and damp winters.
Areas that lie to the west of the Great Dividing Range are windward and therefore never experience a foehn effect under a westerly stream, with persistent cloud cover. On the contrary, the Great Dividing Range also blocks frontal systems originating in the southern Tasman as well as the eastern Bass Strait. When south/southeasterly frontal systems lift over the coastal slopes, the western edge of the Range would, conversely, experience foehn-like winds.
In southeastern Queensland, foehn winds are associated with prefrontal/pre-trough gradient northwesterly winds, post-frontal west to southwesterly gradient winds linked with anticyclonic ridging over southern Australia, and as well as east coast lows in the southeast. They are most predominant in August and September in the transect between Toowoomba and Gatton – The Applethorpe to Archerfield Airport line of area recorded around 20 foehn events per year, followed by the Toowoomba to Archerfield Airport transect recorded 19 foehn events per year, becoming rarer towards Warwick.

### Leeward zones

* From north to south, the westerly foehn strongly affects areas that lie to the east of the Great Dividing Range (the southeast coastal plains or the eastern seaboard) such as, Newcastle, Gosford, Sydney, Wollongong, Nowra, Ulladulla, Moruya, Batemans Bay, Narooma, Bega, and Merimbula.
* The eastern portion of the Blue Mountains lies in the leeward zone, with places from Lawson to Springwood generally featuring a foehn effect.
* A strong foehn effect is observed in the Monaro region to the south, in places such as Bombala, Nimmitabel and particularly Cooma.
* When a vigorous cold front consumes the state of New South Wales, foehn winds would occur in the Hunter Valley in the mid-north coast in places such as Taree, Port Macquarie and Coffs Harbour.

#### Transitional zones

* The western portion of the Blue Mountains is transitional (Leura, Katoomba and westwards). Further inland in the state of New South Wales, Mount Boyce, Lithgow, Bathurst, Goulburn, Bowral, Taralga, Braidwood and Canberra in the Australian Capital Territory, occasionally receive foehn winds, though are at times exposed to south-westerly systems as isolated frontal rainbands pass over the ranges as they lie in a transitional zone. When these areas observe foehn winds, they are inclined to have more cloud cover (including wave clouds) than those on the coastal plain to the east.
* In the East Gippsland region of Victoria, transitional areas include Omeo, Bendoc, Bairnsdale, Orbost, Mallacoota and Sale, as these are highly susceptible to south-westerly systems and would even experience notable cloud cover from true westerlies in some instances. Due to their south-facing location and western longitude, cloud cover is significantly greater than in their New South Wales counterparts.
* In Tasmania, Hobart, New Norfolk, Scamander, Swansea and St Helens on the east coast; as well as Oatlands, Ouse and Bothwell in the Midlands, are downwind of the Central Highlands, thereby usually receiving foehn winds (particularly in the warm season, though sporadically throughout the year). However, due to their south-facing location, they are all susceptible to south-westerly systems and may occasionally experience some cloud cover from westerlies.

## Effects

The Great Dividing wind can be particularly damaging to homes and would affect flights, in addition to being uncomfortable, as the wind chill factor can paradoxically make the temperatures feel cooler than what they are. The Australian foehn has also impacted international sporting events and as well as recreational aviation, such as in 2007, when a light aircraft crashed in the Central Highlands due to severe winds on a region that is prone to mountain-wind waves. Much like the Santa Ana winds in California, they may elevate fire danger in the warmer months due to their dry, gusty nature.
Foehn winds in general have been linked to headaches, depression and as well as suicide contemplation, although this study has not been proven. Though recent studies regarding migraine attacks during Chinook winds suggest there may be some truth in it.

## Notable observations

* 28 May 2000 was a striking example of the 'divided' weather between the western and eastern faces of the range. On the western face, Hunters Hill in Victoria registered a maximum temperature of just −0.7 °C (30.7 °F), whereas Cooma Airport on the eastern face reached 7.3 °C (45.1 °F). These stations are at altitudes of 981 metres (3,219 ft) and 930 metres (3,050 ft) respectively. Furthermore, Thredbo Village reached a maximum of −0.5 °C (31.1 °F); this is warmer than that recorded at Hunters Hill, despite being over 400 metres (1,300 ft) higher in altitude; whereas Cabramurra at a more similar altitude only topped at −3.0 °C (26.6 °F).
* On 29 September 2000, a remarkable foehn event was recorded in the lee of the Blue Mountains region in Sydney, where maximum temperatures at Penrith, Badgerys Creek, Bankstown Airport, and Sydney Airport were around 10 °C (18 °F) above average. The elevated temperatures again coexisted with the inflow of significantly drier air. Simultaneously, the leeward stations in the southern New South Wales coast showed a sharp increase in temperature (9°C in 2 hours) and a decrease in relative humidity. Similar warming and drying were also observed further inland at Cooma, Braidwood, Canberra, and Bombala.
* On 29 May 2007, it was observed that the temperature at Sale (leeward side) was around 4–9 °C (7–16 °F) higher than the corresponding temperatures at Melbourne and Wangaratta (which lie on the upwind side). In this foehn event, Sale had a high above 24 °C (75 °F), whereas the latter cities struggled to reach higher than 12 °C (54 °F). Furthermore, the relative humidity was 31% at Sale and as high as 80%–90% at Melbourne and Wangaratta. Unusually warm and dry conditions were also registered at other stations in the downwind side of the ranges – Bairnsdale, Orbost, Latrobe Valley, and Nowa Nowa, which recorded temperatures of 24 °C (75 °F), 24.2 °C (76 °F), 22.9 °C (73 °F), and 22.6 °C (73 °F), respectively, making this location in the lee of the ranges consistent with the position of the foehn gap and foehn arch.
* On 2 April 2008, maximum temperatures on the Gippsland coast coexisted with peak wind speeds from the northwest that gusted to 75 km/h. Temperatures at Bairnsdale, Latrobe Valley, and Nowa Nowa were 2°–4°C higher than average, with reductions in relative humidity also being observed.
* On 28 April 2008, predominant winds were mainly westerly with the hottest and driest areas of southeastern Australia located along the coastal fringe of southern New South Wales, in the lee of the Great Dividing Range. Temperatures on the windward side of the mountains reached at about 8°C below average, while in the lee temperature peaked at only about 1°–2°C below average, therefore indicating a positive anomaly of about 6°–7°C.
* On the evening of 18 September 2008, temperatures at Mount Nowa Nowa and Bairnsdale rose after sunset, while relative humidity displayed complemental behavior during the course of the night. On 19 September, the relatively warm and dry conditions prevailed along the Gippsland coast, in contrast to upwind conditions.
* On 27 October 2008, foehn wind dynamics were observed over the Gippsland region to the southeast of the Australian Capital Territory on the lee of the ranges, associated with northwesterly winds over southern New South Wales. These downwind regions experienced lower humidity levels and higher than average temperatures. The temperature at Orbost reached 32 °C (90 °F); the temperature at Mount Nowa Nowa rose to 26 °C (79 °F); Bega reached 36 °C (97 °F), which is approximately 14 °C (25 °F) above the average maximum temperature for October–November. At Moruya, the temperature rose to a maximum of 35.4 °C (96 °F). Similar but less pronounced effects were also observed in Green Cape, Bombala, and Cooma. In contrast, Albury, which is on the windward side of the ranges, only reached a maximum of 27.7 °C (82 °F).
* On 23 August 2012, a foehn effect caused Sydney to record its 3rd warmest August day on record where it reached 29.0 °C (84 °F) at the CBD and 30.0 °C (86 °F) at Sydney Airport.
* On 18 July 2016, Mallacoota reached an unseasonable high of 23.5 °C (74 °F) due to the foehn effect, a record warm winter day for that region in Victoria.
* On 20 September 2023, during a heatwave in southeast Australia, Gabo Island, Ulladulla and Montague Island recorded highs of 32.1 °C (90 °F), 35.4 °C (96 °F) and 33.4 °C (92 °F), respectively, due to strong foehn winds on the leeward side of the mountains. Western Sydney surpassed 35.0 °C (95 °F), and Sydney Airport recorded its highest September temperature at 35.9 °C (97 °F).
* On 30 August 2024, hot foehn winds on the eastern seaboard caused Sydney Airport to reach a winter record of 31.5 °C (88.7 °F).
* On 27 November 2024, due to the foehn effect, Sydney Airport reached 38.1 °C (100.6 °F) at 12:15pm, which made it the hottest place in the world at that time.