Drought in Australia is defined by the Australian Bureau of Meteorology as rainfall over period greater than three-months being in the lowest decile of what has been recorded for that region in the past. [1] This definition takes into account that drought is a relative term and rainfall deficiencies need to be compared to typical rainfall patterns including seasonal variations. Specifically, drought in Australia is defined in relation to a rainfall deficiency of pastoral leases and is determined by decile analysis applied to a certain area. [2] Note that this definition uses rainfall only because long-term records are widely available across most of Australia. However, it does not take into account other variables that might be important for establishing surface water balance, such as evaporation and condensation.
Historical climatic records are now sufficiently reliable to profile climate variability taking into account expectations for regions. [3] Bureau of Meteorology records since the 1860s show that a 'severe' drought has occurred in Australia, on average, once every 18 years. [4] State Governments are responsible for declaring a region drought affected and the declaration will take into account factors other than rainfall. [1]
Australia has experienced a marked decrease in precipitation levels since 1994. [5] Deficiencies in northern Australia increased in 2013–14, leading to an extended drought period in certain parts of Queensland. Between 2017 and 2019, severe drought developed once more across much of eastern and inland Australia including Queensland, New South Wales and Victoria, also extending into parts of South and Western Australia.
Since 1860, when adequate meteorological recording commenced, the most severe droughts have occurred commonly at intervals of 11 to 14 years. Major droughts that were recorded later in the 19th century include:
At the time of Federation, Australia suffered a major drought. There had been a number of years of below average rainfall across most of Australia before the drought. During the drought, the wheat crop was "all but lost", and the Darling River was dry at Bourke, New South Wales, for over a year, from April 1902 to May 1903. There was concern about Sydney's water supply. [10] By 1902, Australia's sheep population dropped from its 1891 level of 106 million to fewer than 54 million. Cattle numbers fell by more than 40 per cent. Sheep numbers did not return to 100 million until 1925.
In the 1911–1915 period, Australia suffered a major drought, which failed the 1914 wheat crop. [11] From 1918 to 1920, a severe drought was experienced by Queensland, New South Wales, South Australia, Northern Territory (Darwin-Daly Waters area and central Australia), Western Australia (Fortescue area), Victoria, and Tasmania.
During World War II frequent dry spells from 1937 to 1945 extended over New South Wales, Victoria, much of Queensland and parts of Western Australia, with more breaks than the Federation and Millennium droughts, but more periods of intense dryness. Parts of New South Wales, notably the central west, had record-low rainfall and in 1938 severe dry conditions intensified there and in Victoria, eastern South Australia and in southwest Australian grain-growing areas. An extremely dry six-month spell in Victorian forests contributed to the disastrous Black Friday bushfires of January 1939, before heavy rain came in late February 1939 over Victoria, South Australia and New South Wales. [12]
The rains were only a brief respite, and 1940 was one of the driest years of the century over most of southern Australia, emptying the Nepean Dam in New South Wales and imposing water restrictions in Brisbane. Perth had its driest year of the 20th century. Heavy rain in the southeastern States in November 1940 and January 1941 slightly eased the situation and 1942 was a year of good general rain, but an even worse 1944 resulted when dearth of winter–spring rains led to failure of the wheat crop and required populations in northern Victoria to cart water. Into 1945, large rivers virtually dried up, with most of the Hunter River ceasing flow and the Hawkesbury drying up at North Richmond. There was no flow in the Murray above Echuca. Adelaide faced water shortages while main Victorian water storages were empty in April 1945 and water restrictions were imposed as far north as Townsville. Dust storms blanketed South Australia, northern Victoria and southern New South Wales through the summer of 1944–45. [13]
Artist Russell Drysdale undertook 3-week 5000km tour, at the height of WW2, of wind-eroded drought-stricken areas on commission from The Sydney Morning Herald . The articles written by Keith Newman and variously headed "The country in which there are no Bushfires. There is nothing to burn;" "Worst Drought in Australia's History;" and "An Artist's Journey Into Australia's Lost World," were generously illustrated with stark line drawings by Drysdale and appeared on subsequent days 16-19 December 1944. [14]
The drought broke in the southern States in winter 1945, with a good wheat harvest that year, but in some regions of southern Queensland and northern New South Wales 1946 was the worst year of all, and only in 1947 did significant general rains end the long drought.
In 1952 large regions across the North were affected by a failed wet season declared to be the "driest season for 50 years." [15] Its effect on agriculture was profound, with millions of cattle dying, many because the stock routes south were too dry to sustain their journey. [16] Artist Sidney Nolan, on commission from the Brisbane Courier-Mail, produced a series of photographs of their dried carcasses, [17] but the results were judged by editors to be too confronting and the article carried his drawings from the pictures instead. [18]
From 1965–1968, eastern Australia was again greatly affected by drought. Conditions had been dry over the centre of the continent since 1957 but spread elsewhere during the summer of 1964/1965. This drought contributed to the 1967 Tasmanian fires in which 62 people died in one day and 1,400 homes were lost. [19]
The drought in 1982–83 is regarded as the worst of the twentieth century for short-term rainfall deficiencies of up to one year and their over-all impact. There were severe dust storms in north-western Victoria and severe bushfires in south-east Australia in February 1983 with 75 people killed. [20] 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.
An extremely severe drought occurred in the later year of 1991, [21] which intensified in 1994 and 1995 to become the worst on record in Queensland. [22] This drought was influenced by a strong El Niño weather pattern and associated with high temperatures in July and August 1995, the fifth continuous year of drought in parts of Queensland. According to Primary Industries Minister, Ed Casey, "the drought affected region stretched in a 200 km to 300 km wide strip from Stanthorpe to Charters Towers". [23] So few wheat and barley crops survived, about half the usual for that year, that grains had to be imported from other states. [24]
In June 1994, more than ten towns had lost irrigation systems; and some areas had gone five years without decent rainfall. [23]
A part of the upper Darling River system collapsed during this drought. By October 1994, the Condamine River was exhausted, reverting to a series of ponds. Across the state, in more than 13,000 properties, totaling 40% of Queensland, was drought declared. [25] The flow past Goondiwindi was the lowest since 1940. Cotton farms near Moree and Narrabri had been allocated no water for irrigation, which resulted in a major loss of production. [25] The town of Warwick was particularly affected.
From 1996 to 2010, south-eastern Australia experienced prolonged dry conditions with rainfall persistently well below average, particularly during the cooler months from April to October. The most acute period of the so-called 'Millennium drought' was between 2001 and 2009. The drought finished with the arrival of wet La Niña conditions during 2010 and 2011, with particularly heavy summer rainfall. [26]
Dry conditions began to emerge in south-eastern Australia during late 1996 and intensified during the strong 1997 El Niño event. [27] Rainfall in 1998, 1999 and 2000 was closer to average, with isolated areas affected by rainfall well below average.
According to the Bureau of Meteorology, much of eastern Australia experienced a dry 2001. [28] 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. [29]
The El Niño weather pattern broke down during 2003, but occasional strong rainfall in 2003 and 2004 failed to alleviate the cumulative effect of persistently low rainfall in south-eastern Australia, with some measurement stations having recorded below average rainfall for eight consecutive years. [30] Rainfall in early 2005 remained below average, and better rainfall in the second half of the year again failed to break continuing drought conditions in the south-east. [31]
South-east Australia experienced its second driest year on record in 2006, particularly affecting the major agricultural region of the Murray–Darling basin. [32] 2007 saw record temperatures across the south of Australia, and only patchy rain; promising early year rains contrasted with a very dry July–October period, meaning that drought conditions persisted across much of the south-east. At this point, the Bureau of Meteorology estimated that south-eastern Australia had missed the equivalent of a full year's rain in the previous 11 years. [33]
2008 and 2009 saw continuing hot and dry conditions in 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. [34]
Australia's weather pattern transitioned rapidly to a wet La Niña pattern during autumn, resulting in record-breaking rains in the Murray-Darling Basin and well above average rainfall across the south-east. For many locations this was the first year of above-average rainfall since 1996. The rainfall dramatically increased surface water storage and soil moisture, effectively ending the drought in the south-east. [35] Very wet conditions continued through 2011, resulting in floods in Queensland and northern Victoria. [36]
Dairy producers were hit particularly hard by the drought. 2004 was a particularly bleak year in the sector, with revenue in the industry falling by 5.6%. [37]
Agricultural production was affected. Water use by the industry fell by 37% between 2000/01 and 2004/05, due mainly to drought. [38] Around 20 cotton communities and 10,000 people directly employed by the cotton industry were impacted by the drought. The main areas affected were in New South Wales: Menindee, where the area under production was reduced by 100%, Bourke, area reduced by 99%, Walgett by 95%, the Macquarie River by 74% and Gwydir River by 60%. In Queensland, the worst-affected areas were Biloela, which reduced the area under production by 100%, Dirranbandi, by 91%, Central Highlandsby 82% and Darling Downs by 78%. Bourke has only had adequate water for one cotton crop in the last five years. [39]
Dry conditions again began to develop and be sustained in mid-2013 through much of western Queensland. [40] 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. [41]
Dry conditions continued into 2015 in the east, particularly in Queensland where the monsoon rains were delayed. Queensland had experienced poor wet season rains for three consecutive seasons. [42] Wetter conditions in 2016 eased the effects of drought in eastern Australia, but pockets of south-east Queensland and north-east New South Wales remained drier than average. [43]
Stock feed becomes scarce and farmers find it difficult to feed cattle and sheep. [44]
2017 was a drier than average year for much of inland Queensland, most of New South Wales, eastern and central Victoria, and all of Tasmania. [45] In 2018, rainfall for the year was very low over the southeastern quarter of the Australian mainland, with much of the region experiencing totals in the lowest 10% of historical observations, and was particularly low over the mainland southeast from April onwards. [46] The state of New South Wales was declared to be 100% in drought by August 2018, remaining at 98.6% into May 2019; [47] [48] by May 2019 65.2% of Queensland was also declared to be in drought. [49] Two southern parts of Western Australia were declared "water deficient" by May 2019 after months of drought, [50] with other drought affected areas including central and east Gippsland in Victoria, and parts of eastern South Australia. On one-to-two-year timeframes to the end of March 2019, rainfall deficiencies in the Murray–Darling Basin, Australia's most extensive river system, were the third lowest on record, behind similar length timeframes between 1901 and 1903, and between 1918 and 1920. [51] In July 2019, climatologist David Jones from the Australian Bureau of Meteorology stated that the present drought was now officially the worst on record in the Murray–Darling Basin, and "had now exceeded the Federation Drought, the WWII drought and the Millennium drought in terms of its severity through the MDB". [52] In October 2019, Australia's Bureau of Meteorology stated that drier and warmer and drier than average conditions were expected to persist at least until the end of the year with no relief in sight for most of the drought affected areas, influenced at least in part by a positive Indian Ocean Dipole and a prolonged period of negative SAM (Southern Annular Mode) during October and November. [53] Exacerbating the effects of diminished rainfall in this drought has been a record breaking run of above average monthly temperatures, lasting 36 months to October 2019. [54]
As of December 2019 [update] the drought was continuing – including the driest November across Australia on record [55] – but the Bureau of Meteorology reported that the positive Indian Ocean Dipole had weakened to around 50% of its peak seen in mid October, possibly indicating a future improvement in conditions later in the Australian summer. [56]
From 7-10 February 2020, many areas on the east coast of New South Wales received heavy and continuous rain, the heaviest falls for thirty years. 391.6 millimetres (15.42 in) of rain fell over the four days in Sydney, more than three times the February average. [57] Flooding was extensive, including areas such as Lake Conjola, that had been devastated by bushfires about 6 weeks earlier. [58] About 28500 people were affected by this drought.
In March 2021, above average rainfall led to serious and destructive flooding in the Hawkesbury-Nepean catchment and on the Mid North Coast of New South Wales. [59]
In November 2013 the Australian Government released a $500 million drought stimulus package, including an additional $2 million in loans under the Regional Investment Corporation under a reconfigured payment schedule, an extension to the existing Drought Communities Program which provides money to regional Councils, and supplementary payments under the Roads to Recovery program to assist with job creation in drought-affected areas. [60] The plan also provided $100 million for South Australia to turn on its Adelaide Desalination Plant to significantly ramp up production of water to supply the Adelaide metropolitan area, to allow farmers affected by drought to access more water from the Murray River upstream. [61] This followed the release of a $170 million Drought Stimulus Package by the New South Wales State Government in June. [62]
Dry conditions in September 2019 contributed to several small to mid-range fires in north eastern New South Wales. By November of that year, continuing heat and lack of rain had desiccated the forests and agricultural land along the Great Dividing range in New South Wales and Queensland. Sydney received less than 2 millimetres (0.079 in) of rain in December 2019, with temperatures reaching 40°C (104°F). Numerous intense bushfires occurred [63] , some of which burnt Gondwanan rainforest remnants that had not experienced fires for millennia.[ citation needed ] This included Mount Nothofagus National Park and Nightcap National Park.
Australia's national science research agency, the Commonwealth Scientific and Industrial Research Organisation (CSIRO), states that on account of projected future climate change, hot days will become more frequent and hotter (very high confidence), extreme rainfall events will become more intense (high confidence), and the time in drought is projected to increase over southern Australia (high confidence). Seasonal-average rainfall changes will vary across Australia: in southern mainland Australia, winter and spring rainfall is projected to decrease (high confidence), but increases are projected for Tasmania in winter (medium confidence), while in eastern and northern Australia in the near future (to 2030), natural variability is anticipated to predominate over trends due to greenhouse gas emissions. [64] However even if climate change does not result in decreased rainfall in eastern and northern Australia over the period to 2030, the perceived severity of drought (in terms of low soil moisture) would increase on account of the higher evaporative demand resulting from the projected overall rise in average temperatures.
New South Wales is Australia's most populous state, located in the east coast of the continent. It is in the southern hemisphere between latitudes 28 and 38 degrees south of the equator and longitudes 141 and 154 degrees east of the Universal Prime Meridian. The state is in the warm temperate climatic zone.
The following lists events that happened during 1902 in Australia.
The climate of Sydney, Australia is humid subtropical, shifting from mild and cool in winter to warm and occasionally hot in the summer, with no extreme seasonal differences as the weather is moderated by proximity to the ocean, although more contrasting temperatures are recorded in the inland western suburbs. Despite the fact that there is no distinct dry or wet season, rainfall peaks during summer and autumn months, and is at its lowest just around the middle of the year, though precipitation can be erratic throughout the year. Precipitation varies across the region, with areas adjacent to the coast being the wettest. According to the Bureau of Meteorology, Sydney falls in the temperate climate zone which has warm to hot summers and no dry season. Sydney's plant hardiness zone ranges from zone 11a to 9b throughout the metropolitan area. Under the Holdridge Life Zones classification, eastern Sydney falls in the Subtropical Moist Forest zone and the western suburbs in the Subtropical Dry Forest zone.
Australia's climate is governed mostly by its size and by the hot, sinking air of the subtropical high pressure belt. This moves north-west and north-east with the seasons. The climate is variable, with frequent droughts lasting several seasons, thought to be caused in part by the El Niño-Southern Oscillation. Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert. Australia holds many heat-related records: the continent has the hottest extended region year-round, the areas with the hottest summer climate, and the highest sunshine duration.
Climate change has been a critical issue in Australia since the beginning of the 21st century. Australia is becoming hotter and more prone to extreme heat, bushfires, droughts, floods, and longer fire seasons because of climate change. Climate issues include wildfires, heatwaves, cyclones, rising sea levels, and erosion.
In Australia, the Federation Drought is the name given to a prolonged period of drought that occurred around the time of Federation in 1901.
The 1950 rainfall records for the Australian states of New South Wales and Queensland reported probably the most remarkable record high rainfall totals ever recorded anywhere in the continent. Averaged over both of these states, 1950 is clearly the wettest year since adequate records became available circa 1885. Queensland recorded a statewide average rainfall of around 1,125 millimetres (44.3 in) as against a mean since 1885 of around 640 millimetres (25.2 in), whilst New South Wales recorded around 930 millimetres (36.6 in) as against an instrumental mean around 520 millimetres (20.5 in). Australia's wettest town, Tully also recorded its highest annual rainfall total in 1950 with 7,925 millimetres (312.0 in).
Between 1979 and 1983 almost all of eastern Australia was affected by a major drought.
The 1911–16 Australian drought consisted of a series of droughts that affected various regions of Australia between the years of 1911 and 1916. Most of the dry spells during this period can be related to three El Niño events in 1911, 1913 and 1914, though rainfall deficiencies actually began in northern Australia before the first of these El Niños set in and did not ease in coastal districts of New South Wales until well after the last El Niño had firmly dissipated and trends toward very heavy rainfall developed in other areas of the continent.
Droughts are a relatively common feature of the weather in the United Kingdom, with one around every 5–10 years on average. These droughts are usually during the summer, when a blocking high causes hot, dry weather for an extended period. However this means that droughts can vary in their characteristics. All types of drought cause issues across all sectors, with impacts extending to the ecosystem, agriculture and the economy of the whole country in severe cases of drought. The south east of the country usually suffers most, as it has the highest population and the lowest average precipitation per year, which is even lower in a drought. Even in these areas in severe droughts, the definition, impacts, effects and management are all minimal in comparison to drought prone areas such as Australia and parts of the United States. In recent years however, the summers of 2007, 2008, 2009, August 2010 and 2012 were wetter than normal, 2007 being wettest on record. Droughts have continued to occur in recent times, with spring 2011, July 2013, summer 2018, spring 2020, spring and summer 2022 and May and June 2023 all featuring excessively dry periods for part or all of the UK, and will likely become more severe due to climate change over the 21st century.
The 2000s drought in Australia, also known as the millennium drought, is said by some to be the worst drought recorded since European settlement.
The geography of Queensland in the north-east of Australia, is varied. It includes tropical islands, sandy beaches, flat river plains that flood after monsoon rains, tracts of rough, elevated terrain, dry deserts, rich agricultural belts and densely populated urban areas.
The 2010 Gascoyne River flood was regarded as the most severe flood to take place along the Gascoyne River in Western Australia on record. Triggered by record-breaking rainfall, amounting to over 6,000 percent of the monthly mean, 313.6 mm (12.35 in) and 5 mm (0.20 in) respectively, in just four days, the floods caused widespread damage in the region. By 17 December, the river began to rise in response to the heavy rains, eventually exceeding its banks within two days. Water levels reached record values at three stations along the river, cresting at 15.53 m (51.0 ft) near Fishy Pool. Evacuation orders were issued for several towns affected by rising waters. The most substantial impact was felt in Carnarvon where entire homes were washed away. Following the disaster, emergency supplies and funds were distributed to affected residents to aid them in restoring their livelihoods. Though no people died in the event, an estimated two thousand head of cattle perished and damage was estimated at A$100 million.
The Australian summer of 2012–2013, known as the Angry Summer or Extreme Summer, resulted in 123 weather records being broken over a 90-day period, including the hottest day ever recorded for January on record, the hottest summer average on record, and a record seven days in a row when the whole country averaged above 39 °C (102 °F). Single-day temperature records were broken in dozens of towns and cities, as well as single-day rainfall records, and several rivers flooded to new record highs.
Australian east coast lows are extratropical cyclones or low-pressure systems on the coast of southeastern Australia that may be caused by both mid-latitude and tropical influences over a variety of levels in the atmosphere. These storms should not be confused with Australian region tropical cyclones which typically affect the northern half of the continent.
The 2014–2016 El Niño was the strongest El Niño event on record, with unusually warm waters developing between the coast of South America and the International Date Line. These unusually warm waters influenced the world's weather in a number of ways, which in turn significantly affected various parts of the world. These included drought conditions in Venezuela, Australia and a number of Pacific islands while significant flooding was also recorded. During the event, more tropical cyclones than normal occurred within the Pacific Ocean, while fewer than normal occurred in the Atlantic Ocean.
Brisbane has a humid subtropical climate with year-round period with warm to hot temperatures. Brisbane generally experiences 3 months of mild cool winter from June to August.
Severe weather events or extreme weather events in Sydney, Australia, include hailstorms, thunderstorms, gale, bushfires, heatwaves, drought, and flash flooding from heavy rain. Sydney is rarely affected by cyclones, although remnants of cyclones do affect the city.
Effects of the El Niño–Southern Oscillation in Australia are present across most of Australia, particularly the north and the east, and are 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 28 El Niño and 19 La Niña events in Australia including the current 2023 El Niño event, which was declared on 17th of September in 2023. 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.
2022 was an extremely wet year for Australia, coming out of a back-to-back La Niña in the summer of 2021-22, a Negative Indian Ocean Dipole developing over the winter and a third back-to-back La Niña in the spring of 2022.
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