Effects of the El Niño–Southern Oscillation in Australia

Effects of the El Niño–Southern Oscillation in Australia is present across most of Australia, particularly the north and the east, and is one of the main climate drivers of the country. Associated with seasonal abnormality in many areas in the world, Australia is one of the continents most affected and experiences extensive droughts alongside considerable wet periods that cause major floods. There exist three phases — El Niño, La Niña, and Neutral, which help to account for the different states of ENSO. Since 1900, there have been 27 El Niño and 18 La Niña events in Australia. The events usually last for 9 to 12 months, but some can persist for two years, though the ENSO cycle generally operates over a time period from one to eight years.

Through La Niña years the eastern seaboard of Australia records above-average rainfall usually creating damaging floods due to stronger easterly trade winds from the Pacific towards Australia, thus increasing moisture in the country. Conversely, El Niño events will be associated with a weakening, or even a setback, of the prevailing trade winds, and this, results in reduced atmospheric moisture in the country. Many of the worst bushfires in Australia accompany ENSO events, and can be exacerbated by a positive Indian Ocean Dipole, where they would tend to cause a warm, dry and windy climate. The Bureau of Meteorology features an alert system for the El Niño–Southern Oscillation.

Impacts

El Niño

El Niño episodes are defined as continuous warming of the central and eastern tropical Pacific Ocean, thus resulting in a decrease in the strength of the Pacific trade winds, and a reduction in rainfall over eastern and northern Australia, particularly in winter and spring. An El Niño event typically begins in autumn and fully forms during winter and spring, but would then would start to dissipate by summer, with the event usually concluding in the autumn of the next year. Snow depth during El Niño years is generally lower in Australia's alpine regions.

Furthermore, El Niño years generally experience warmer-than-average temperatures with hotter daily temperature extremes across the south, especially in spring and summer. Even though temperature maxima is occasionally warmer than average, reduced cloud cover frequently produces a cooler temperature minimum during winter-spring and a longer frost season.

El Niño's effect on Australian rainfall decreases after November, particularly in the southeast, and therefore a pronounced difference between the rainfall patterns of early and late summer would exist. Nonetheless, Cape York and northwest Tasmania would have moderately dry conditions. Some areas on the Queensland/New South Wales border exhibit a small inclination for wetter conditions. There is also a reasonably stronger propensity for wetter than average conditions in the southeast of Western Australia.

La Niña

La Niña episodes are defined as uninterrupted cooling of the central and eastern tropical Pacific Ocean, thus resulting in an increase in the strength of the Pacific trade winds, and the opposite effects in Australia when compared to El Niño. In the La Niña case, the convective cell over the western Pacific strengthens inordinately, resulting in colder than normal winters in North America and a more intense cyclone season in South-East Asia and Eastern Australia with above-average winter–spring rainfall. There is a strong correlation between the strength of La Niña and rainfall: the greater the sea surface temperature and Southern Oscillation difference from normal, the larger the rainfall change.

La Niña is characterised by increased rainfall and cloud cover, especially across the east and north that continue into the warm months (unlike El Niño events); the average December–March precipitation is 20% higher than the long-term average, particularly in the east coast. Snow depth and snow cover is increased in the southeast during winter. There are also cooler daytime temperatures south of the tropics (especially during the second half of the year) and fewer extreme highs, and warmer overnight temperatures in the tropics. There is less risk of frost, but increased risk of widespread flooding, tropical cyclones, and the monsoon season starts earlier. La Niña Modoki leads to a rainfall increase over northwestern Australia and northern Murray–Darling basin, rather than over the east as in a conventional La Niña.

SOI and IOD

The Southern Oscillation is the atmospheric component of El Niño. This component is an oscillation in surface air pressure between the tropical eastern and the western Pacific Ocean waters. The strength of the Southern Oscillation is measured by the ''Southern Oscillation Index (SOI)''. The SOI is computed from fluctuations in the surface air pressure difference between Tahiti (in the Pacific) and Darwin, Australia (on the Indian Ocean): El Niño episodes with negative SOI means there is lower pressure over Tahiti and higher pressure in Darwin; La Niña episodes with positive SOI means there is higher pressure in Tahiti and lower in Darwin.

In several recent studies, it is shown that the ''Indian Ocean Dipole (IOD)'' has a much more significant effect on the rainfall patterns in south-east Australia than the ''El Niño-Southern Oscillation (ENSO)'' in the Pacific Ocean. It is further demonstrated that IOD-ENSO interaction is a key for the generation of Super El Ninos. When an El Niño occurs with a positive IOD, the two events can strengthen their dry impact. Similarly, when La Niña coexists with a negative IOD, the chance of above-average winter–spring rainfall generally increases.

History

Paleoclimate record

During the Last Glacial Maximum, around 45,000 years ago, moisture variability in the Australian core shows dry periods related to frequent warm events (El Niño), correlated to DO events. Although no strong correlation was found with the Atlantic Ocean, it is suggested that the insolation influence probably affected both oceans, although the Pacific Ocean seems to have the most influence on teleconnection in annual, millennial and semi-precessional timescales.

1880s–1920s

1885 to 1898 were mostly La Niña years, being generally wet, though less so than in the period since 1968. The only noticeably dry years in this era were 1888 and 1897. Although some coral core data suggest that 1887 and 1890 were the wettest years across the continent since settlement. In New South Wales and Queensland, however, the years 1886–1887 and 1889–1894 were indeed exceptionally wet La Niña years, and February 1893 saw the disastrous 1893 Brisbane flood.

1903–04 were La Niña years, which followed the Federation drought, though two major El Niño events in 1902 and 1905 produced the two driest years across the whole continent, whilst 1919 was similarly dry in the eastern States apart from the Gippsland. 1906–07 were moderate La Niña years with above-average rainfalls. 1909 to early 1911 were strong La Niña years. The 1911–1915 period were El Niño years, where the country suffered a major drought. Drying of the climate took place from 1899 to 1921, though with some interruptions from wet El Niño years, especially between 1915 and 1916–18 and 1924–25, and 1928.

1920s–1960s

The period from 1922 to 1937 was particularly dry with most years having a positive El Niño phase, with only 1930 having Australia-wide rainfall above the long-term mean and the Australia-wide average rainfall for these seventeen years being 15 to 20 percent below that for other periods since 1885. This dry period is attributed in some sources to a weakening of the Southern Oscillation and in others to reduced sea surface temperatures. During World War II, eastern Australia suffered El Niño conditions which lasted from 1937 through to 1947 with little relief, despite a few weak and relatively dry La Niña years in between (1938–39 and 1942–43).

1949–51 were La Niña years, which had significant rain events in central New South Wales and most of Queensland: Dubbo's 1950 rainfall of can be estimated to have a return period of between 350 and 400 years, whilst Lake Eyre filled for the first time in thirty years. 1954–57 were also intense La Niña years. In contrast, 1951–52, 1961 and 1965 were very dry, with complete monsoon failure in 1951–52 and extreme drought in the interior during 1961 and 1965. 1964–69 were moderate La Niña years. Conditions had been dry over the centre of the continent since 1957 but spread elsewhere during the summer of 1964–65. The El Niño conditions from 1965–70 contributed to the 1967 Tasmanian fires.

1970s–1990s

The wettest periods in this century have been from 1973 to 1976, peaking in 1974, all La Niña years. The drought in 1979–83 is regarded as the worst of the twentieth century for short-term rainfall deficiencies of up to one year and their over-all impact. An El Niño event brought severe dust storms in north-western Victoria and severe bushfires in south-east Australia in February 1983. This El Niño-related drought ended in March, when a monsoon depression became an extratropical low and swept across Australia's interior and on to the south-east in mid-to late March. 1987–88 were weak El Niño years, with 1988–89 featuring a strong La Niña event affecting the southeast half of the country.

Most of the 1990's were characterised by El Niño events; Beginning in the second half of 1991, a very severe drought occurred throughout Queensland which intensified in 1994 and 1995 to become the worst on record.Collie, Gordon. ''Dry tears of despair''. The Courier-Mail. p. 29. 22 October 1994. From July to August 1995 the drought was further influenced by a strong El Niño weather pattern associated with high temperatures. Dry conditions began to emerge in south-eastern Australia during late 1996 and accentuated during the strong 1997 El Niño event. Despite the fact that the 1990s mostly consisted of El Niño years, a La Niña event formed from May 1998 where, in April 1999, it brought the notorious 1999 Sydney hailstorm.

2000s

The 35 months from May 1998 to March 2001 can be considered a long La Niña phase, although much of eastern Australia experienced a dry 2001. 2002 was one of Australia's driest and warmest years on record, with 'remarkably widespread' dry conditions, particularly in the eastern half of the country which was again affected by El Niño conditions. It was, at the time, Australia's fourth-driest year since 1900. The El Niño weather pattern broke down by 2004, but occasional strong rainfall in 2003 and 2004 failed to alleviate the cumulative effect of persistently low rainfall in south-eastern Australia.

South-east Australia experienced its second-driest year on record in 2006, an El Niño year, particularly affecting the major agricultural region of the Murray–Darling basin. In early 2007, forecasters believed that the El Niño effect that had been driving the drought since 2006 had ended, though the Murray–Darling Basin experienced their seventh consecutive year of below-average rain. Wildfires such as the 2003 Canberra bushfires in January and the worst bushfires in Australian history, which occurred on Black Saturday in February 2009, were intensified when combined with a positive Indian Ocean Dipole (IOD) event.

Although 2007 to early 2009 were moderate La Niña years, hot and dry conditions still prevailed in parts of south-eastern Australia, with occasional heavy rainfall failing to break the continuing drought. The effects of the drought were exacerbated by Australia's (then) second-hottest year on record in 2009, with record-breaking heatwaves in January, February, and the second half of the year, when El Niño conditions returned, which also brought a powerful dust storm in the east.

2010s

According to the Bureau of Meteorology's 2011 Australian Climate Statement, Australia had lower than average temperatures in 2011 as a consequence of a La Niña weather pattern. During the 2010–2012 La Niña event, Australia experienced its second- and third-wettest years, since a record of the rainfall started to kept during 1900. It caused Australia to experience its wettest September on record in 2010, and its second-wettest year on record in 2010. It also led to an unusual intensification of the Leeuwin Current.

El Niño conditions developed in mid-2013 through much of western Queensland. Although these began easing for western Queensland in early 2014, drought began to develop further east, along the coastal fringe and into the ranges of southeast Queensland and northeast New South Wales. Warm and dry conditions continued into 2015 in the east, particularly in Queensland where the monsoon rains were delayed. The 2013 New South Wales bushfires occurred in a neutral ENSO year, as not all major fires occur in El Niño years.

By the start of spring in 2015, the Indian Ocean had started to help the El Niño, which resulted in Australia's third-driest spring on record and limited growth at the end of cropping season. The combination of heat and low rainfall brought a very early start to the 2015–16 Australian bushfire season, with over 125 fires burning in Victoria and Tasmania during October. During the 2014–2016 El Niño event, the 2015–16 Australian region cyclone season was the least active since reliable records started during 1950s.

Mild La Niña conditions were present from April to November 2016. Moderate, albeit brief, La Niña conditions returned in the summer of 2017–18. Despite a few and short-lived La Niña outbursts, 2017–19 mostly consisted of El Niño conditions and had caused drier than average conditions for much of inland Queensland, most of New South Wales, eastern and central Victoria, and all of Tasmania. In 2018, rainfall for the year was very low over the southeastern quarter of the Australian mainland. Exacerbating the effects of diminished rainfall during the 2018 El Niño year were a record-breaking run of above-average monthly temperatures, with the first half of 2019 being on an El Niño alert.

2020s–present

Although the unusually powerful 2019–20 Australian bushfire season was one of the most destructive bushfire seasons on record, it occurred in a neutral ENSO period and was rather intensified by a strong positive IOD. La Niña conditions began to take effect in the 2020-21 summer, which resulted in the coolest summer in nine years and wettest in four years (with 29% more rainfall than average). The La Niña event, although weak, caused the floods in March in southeastern Australia, which led to above-average rainfall and flooding in the Hawkesbury-Nepean catchment and on the Mid North Coast of New South Wales.

November 2021 was one of the wettest on record across some areas in eastern and northern Australia, after a La Niña was officially declared for the 2021–22 summer, making it the first back-to-back La Niña event since 2010–12. Moreover, the summer of 2021–22 in Sydney was the wettest in 30 years due to the persisting La Niña conditions. From late February to early March 2022, southeastern Queensland and northeastern New South Wales experienced significant rainfalls and flooding, which marked the phase of two years of wet La Niña summers in eastern Australia. After the floods in July 2022 in New South Wales, La Niña was declared once again for spring as higher than above average rainfall was recorded in October in New South Wales, making it the third La Niña event in a row.How La Niña could wipe out stretches of Australia's beaches and dunes with wild weather
ABC News. October 8 2022.

See also

*Climate of Australia
*Climate change in Australia
*Drought in Australia
*Floods in Australia
* Bushfires in Australia

References

External links

ENSO Outlook
an alert system for the El Niño–Southern Oscillation by BOM
El Niño Southern Oscillation (ENSO)
by BOM

{{DEFAULTSORT:Effects of the El Nino-Southern Oscillation in Australia
Climate of Australia
Regional climate effects