What is influencing the climate right now, and how might that change?

The sub-tropical ridge has been stronger and further south than usual this year. This high pressure has reduced the number of cold fronts reaching southern Australia and weakened the ones that have made it. Adding to the dry has been a lack of tropical moisture spilling over the continent from oceans to our north. As a result, large parts of Australia have experienced less rainfall, clearer skies, warmer than usual days and locally frosty conditions.

So far, dry conditions during 2018 have largely occurred in the absence of our two key big-hitters when it comes to climate drivers; the El Niño-Southern Oscillation and the Indian Ocean Dipole (IOD). But, unfortunately, it looks like that situation has changed and these two drivers may have a stronger influence for at least the remainder of 2018.

ENSO Outlook status has been raised to El Niño ALERT.

The chances of an El Niño developing late in 2018 have increased and this week the Bureau moved to 'El Niño ALERT'. This means that model outlooks and observations indicate there is approximately a 70% chance that El Niño will develop in the coming months. Current patterns in the Pacific are similar to the early stages of past El Niño.

We've also seen a rise in values of the IOD index, with values over recent weeks indicating a positive IOD event has likely commenced.

El Niño and positive IOD events are typically associated with below average spring rainfall in central and southern Australia and a drier start to the wet season in Queensland and the Northern Territory. The development of either would favour continued dry weather, and increase the likelihood that widespread drought relief will be delayed until 2019. Higher than average temperatures, heatwaves, and more severe bushfire weather are also more likely during El Niño and positive IOD events.

It's been dry for a while

September 2018 was a very dry month, adding to low rainfall seen across many parts of Australia so far this year. September 2018 was not only the driest September in 119 years of record for Australia, but it was also the second-driest for any month of the year (behind only April 1902).

Rainfall for the year to date has been exceptionally low over the mainland southeast, with much of the region experiencing totals in the lowest 10% of records for January–September. Many locations in eastern New South Wales, eastern Victoria and southeast Queensland have received about 400 mm less rainfall than they usually would have by this time of the year.

Rainfall deciles for January to September 2018.

Much of southern Australia has experienced a persistent rainfall decline spanning several decades, which is adding to drought stress by drying the landscape.

Southwest Western Australia has experienced significantly lower cool season (April to October) rainfall since the mid-1970s, compared to observations since 1900, while for the southeast the drop has been more recent, emerging in the mid-1990s. These rainfall declines have been linked to circulation changes in the southern hemisphere influenced by the increase in greenhouse gases.

These rainfall changes have also been accompanied by much larger reductions in streamflow, particularly in the southwest of Australia where high flows have become much less frequent.

Timeseries graph Timeseries graph
April to October rainfall anomalies for southwestern (top) and southeastern (bottom) Australia, showing the decline in totals with respect to the 1961 to 1990 average. The main feature of the decline is significantly fewer wet years, meaning recovery from the dry years is patchy.

And it's also been unusually warm

Low rainfall has also been accompanied by very high daytime temperatures so far this year. Of course, Australian temperatures are warming in line with global trends, but in individual years variations which are likely to be largely natural (such as droughts) may act to add to or subtract from the broader trends.

Historically, droughts have often brought hot conditions, and this has been borne out in 2018. Maximum temperatures for January to September were the warmest on record for the Murray–Darling Basin and New South Wales, with neighbouring regions also much warmer than average.

These extremely warm days, combined with extremely low rainfall, have caused an intense drying of the Australian landscape in 2018, resulting in an early start to the bushfire season in New South Wales and Victoria, where damaging fire were observed as early as late winter.

So how might the year end?

Like all Australians, the Bureau hopes that farmers and those suffering through drought get the rainfall they need, but unfortunately, the outlook indicates that dry conditions are likely to continue for some time. Large parts of southern and eastern Australia are likely to see a drier than average end to the year, though odds favouring drier than average conditions tend to moderate as we head towards summer. Most of the country is likely to see a dry October, though local heavy falls can occur against a backdrop of broadly suppressed rainfall.

While some parts of New South Wales and southeastern Queensland have received very welcome rainfall in the first days of October, rainfall has been below average over much of over eastern Australia for so long (since early 2017) that this rainfall event hasn't been enough to break the drought.

Looking at temperature, outlooks show a very high chance of warmer than average days and nights through to the end of 2018. Considering that the year so far has already been very warm, this means 2018 has the potential to rank as another significant warm year. Seven of Australia's ten warmest years have occurred since 2005, with just one cooler than average year in the last decade (2011), highlighting how warmer than average temperatures now dominate Australia's climate.

Map Map
Climate outlook maps for October to December 2018: chance of exceeding median rainfall (left), and change of exceeding median maximum temperature (right).