You wouldn’t know it from the torrential rains that have inundated large parts of New South Wales and Queensland this year, but average late-autumn rainfall over southeast Australia has declined significantly since the 1990s.
Less rain in these areas is an expected consequence of global warming. In both the northern and southern hemispheres, the paths of the weather systems that bring rain in the middle latitudes have been moving away from the equator and towards the poles.
We studied in detail the drop in rainfall during April and May in southeast Australia, and found it is just one consequence of far-reaching changes in the behaviour of high-altitude winds over Australia.
These high-altitude winds are called jet streams: narrow bands of rapidly flowing air that typically occur at altitudes around the cruising height of commercial passenger aircraft. In April and May, the westerly jet stream over southeast Australia normally splits into a northern branch (called the subtropical jet) and a southern branch (called the polar-front jet).
Since the mid 1990s, the location of this split has moved and the speeds of the winds involved have also changed. We found these changes, which are related to global warming, are responsible for a decrease in the number of low-pressure systems bringing rain to southeast Australia.
The maps you might see on weather apps or TV forecasts usually show what’s going on at ground level: high- and low-pressure systems, cold fronts, and so on. However, these ground-level systems are largely driven by the jet streams and related atmospheric processes.
Humidity and rotation
As well as the changes in the jet stream, there are two other important changes reducing rainfall in the early cool season.
First, the air over parts of inland southeast Australia has become significantly drier since the 1990s.
And second, areas of strongly rotating air have moved further east and south, over the Tasman Sea.
Both humidity and air rotation are important contributors to the development of low-pressure areas that bring rain. As a result of these changes, there has been a significant decrease in late autumn rainfall in southeast Australia.
The bigger picture
Much of the variation in rainfall from year to year depends on the phase of El Niño–Southern Oscillation (ENSO), a large-scale climate phenomenon over the Pacific Ocean. When this is in one phase, called La Niña, eastern Australia experiences lower temperatures and higher rainfall – in the opposite phase, El Niño, it’s the other way around.
In the absence of La Niña years, and particularly groups of repeat La Niña events such as those of 2010–12 and 2020–22, we have seen extreme droughts following dry summers and dry late-autumn periods.
Changes in the atmospheric circulation, especially in the jet stream location and strength, have contributed to the multiple-year droughts we have seen since the 1990s, namely, the periods 1997–2007 and 2017–2019. For example, rain-bearing “east coast lows” are often forming further south, and there are fewer cut-off low pressure systems over inland southeast Australia.
The effects of drought at ground level are easy to see.
The drought periods since 1997 have killed huge numbers of river fish, reduced the viability of broad acre and pastoral farming and other economic industries, and reduced river flows and sustainable access to water in many areas. In a future warming climate, these drought periods are expected to continue.
However, changes to the jet stream also have less obvious effects at higher altitudes. In particular, these changes have implications for air transport.
Changes in speed, location and structure of jet streams will mean planes will use more fuel on many routes, including in Australia. Less favourable winds, and an increase in sudden “clear-air turbulence”, will increase aviation fuel consumption.
The authors do not work for, consult, own shares in or receive funding from any company or organization that would benefit from this article, and have disclosed no relevant affiliations beyond their academic appointment.
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