Image: Jason O’Brien/AAP
At any one time, Earth’s atmosphere holds only about a week’s worth of rain. But rainfall and floods have devastated Australia’s eastern regions for weeks and more heavy rain is forecast. So where’s all this water coming from?
We recently investigated the physical processes driving rainfall in eastern Australia. By following moisture from the oceans to the land, we worked out exactly how three oceans feed water to the atmosphere, conspiring to deliver deluges of rain similar to what we’re seeing now.
Such research is important. A better understanding of how water moves through the atmosphere is vital to more accurately forecast severe weather and help communities prepare.
The task takes on greater urgency under climate change, when heavy rainfall and other weather extremes are expected to become more frequent and violent.
Big actors delivering rain
The past few months in eastern Australia have been very wet, including the rainiest November on record.
Then in February, heavy rain fell on already saturated catchments. In fact, parts of Australia received more than triple the rain expected at this time of year.
So what’s going on?
In the theatre that is Australia’s rainfall, there are some big actors – the so-called climate oscillations. They’re officially known as:
- El Niño-Southern Oscillation (ENSO): this cycle comprises El Niño and its opposite, La Niña. ENSO involves temperature changes across the tropical Pacific Ocean, affecting weather patterns around the world
- Southern Annular Mode (SAM): the north-south movement of strong westerly winds over the Southern Ocean
- Indian Ocean Dipole (IOD): changes in ocean temperatures and winds across the tropical Indian Ocean.
Like swings in a character’s mood, each climate mode has positive, negative and neutral phases. Each affect Australia’s weather in different ways.
ENSO’s negative phase, La Niña, brings wetter conditions to eastern Australia. The IOD’s negative phase, and SAM’s positive phase, can also bring more rain.
Going back in time
We studied what happens to the moisture supplying eastern Australian rainfall when these climate drivers are in their wet and dry phases.
We used a sophisticated model to trace moisture backwards in time: from where it fell as rain, back through the atmosphere to where it evaporated from.
We did this for every wet winter and spring day between 1979 and 2013.
This research was part of a broader study into where Australia’s rain comes from, and what changes moisture supply during both drought and heavy rain.
We found most rain that falls on eastern Australia comes from moisture evaporated from a nearby ocean. Typically, rain in eastern Australia comes from the Coral and Tasman seas. This is depicted in the strong blue colours in the figure below.
But interestingly, some water comes from as far as the Southern and Indian oceans, and some originates from nearby land areas, such as forests, bare soils, lakes and rivers.
Our research shows of all possible combinations of climate oscillations, a La Niña and a positive SAM phase occurring together has the biggest effect on eastern Australian rainfall. That combination is happening right now.
During La Niña, more moisture is transported from the ocean to the atmosphere over land and is more easily converted to rainfall when it arrives.
During the positive SAM, the usual westerly winds shift southward, allowing moisture-laden winds from the east to flow into eastern Australia.
Our research focused on winter and spring. However, we expect the current rainfall is the result of the same combined effect of the two climate oscillations.
The Indian Ocean Dipole is not active at this time of the year. But it was in a weak negative phase last spring, which tends to bring wetter-than-normal conditions.
Looking to future floods
The current La Niña event is past its peak and is predicted to dissipate in autumn. But because our catchments are so full of water, we still need to be on alert for extreme weather.
The current devastating floods are a sobering lesson for the future. They show the urgent need to understand and predict extreme events, so communities can get ready for them.
This article was co-written by:
Chiara Holgate receives funding from the Australian Research Council Centre of Excellence for Climate Extremes.
Agus Santoso receives funding from CSIRO. Agus Santoso is a CSIRO adjunct science leader, co-project leader at the Centre for Southern Hemisphere Oceans Research, associate investigator at the ARC Centre of Excellence for Climate Extremes, and is affiliated with the Australian Government’s National Environmental Science Program.
Alex Sen Gupta receives funding from the Australian Research Council as part of the Centre of Excellence for Climate Extremes and the Centre of Excellence in Antarctic Science