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The Australian Climate

Climate and Physical Changes

 

 

What has happened

What is likely to happen this century

Atmospheric CO2

  • CO2 emissions have risen from ~280 ppm since ~1850 to ~400 ppm in 2013
  • The rate of emissions is accelerating, from ~1% p.a. in the 1990s, to nearly 6% in 20101
  • Emissions trajectories will depend on global mitigation efforts but the general expectation is for a doubling of pre-industrial levels by the end of the 21st century2. Emissions are currently tracking the highest emissions scenario described by the IPCC in 2007

Temperature

  • Average annual surface temperatures in Australia have risen +0.94ºC over the past 100 years3.
  • It is likely that warming will be greatest over inland Australia 4,5, however, coastal regions are predicted to experience the greatest change relative to current climate208

Rainfall

  • SW Australia has become drier since the 1970s and autumn/winter rainfall has declined in the SE since the mid-1990s6
  • The NW has become wetter since the 1950s 7
  • There is high probability that rainfall will decline further in the SW and potentially in the SE 4,5, 8
  • In eastern and northern Australia, the direction of future rainfall change remains uncertain 4,5, 9

Snow and frost

  • Late-season snow depth has declined significantly in the Snowy Mountains since the late 1950s10
  • Models predict a very high probability that both snow depth and area will decline - e.g.: the area in mainland Australia with an average annual snow cover of at least thirty days is projected to decline by 14 - 54% by 2020, and by 30 - 93% by 205010

Sea level

  • Mean sea level has risen by around 1-2mm/year across Australia over the past century17 with rates of over 6 mm/year in northern Australia over the last 20 years11
  • There is a high probability that sea level will rise, e.g.: up to 80cm this century, and continue to rise for at least several more centuries12 


Extreme events*

Temperature extremes

  • Hot days (>35ºC) have become more frequent and cold days (<0oC) have declined 13,14,15,16
  • Increased numbers of warm nights, fewer frosts and longer heat-waves are predicted to be very likely 13,14, 17
  • Increased numbers of warm nights, fewer frosts and longer heat-waves are predicted to be very likely 13,14, 17

Precipitation extremes

  • There has been a strong decrease, since 1910, in the intensity of rain falling on very wet days, and in the number of very wet days, in south-west Australia. There has been a strong increase in the proportion of annual rainfall falling on very wet days in the north-east18
  • Extreme rainfall events are projected to increase 5, although considerable spatial variation is expected18
  • Extreme rainfall events are projected to increase 5, although considerable spatial variation is expected18

Drought

  • Regional warming has increased the intensity of recent droughts in south-eastern Australia 19, 20,21
  • Climate models project that drought occurrence is likely to increase in southern Australia 22,23,24,25  

Tropical cyclones

  • There has been no significant change in the number of tropical cyclones or the proportion of intense storms since the 1980s 26
  • It is possible that tropical cyclones may increase in intensity but decrease, or stay similar, in frequency 27

Fire

  • Extreme fire weather has increased since the 1970s especially in the southeast of the continent28
  • It is highly likely that the number of very high fire danger days will increase in the south-east. Less certain projections are for no change or a decrease in the north-east) 29,30
  • The effects of fire regimes will depend on interactions between weather, fuel mass and moisture, and ignition events 31,32,33

Extreme sea level events

  • There is some evidence of an increase in the incidence of extreme high sea levels (excluding tsunamis) 34
  • Projected sea level rise are highly likely to lead to large increases in the frequency of extreme sea level events12, 35

*Changes in the El Niño Southern Oscillation (ENSO) phenomenon in response to anthropogenic climate change are uncertain but could significantly influence rainfall and temperature extremes, droughts, fire danger, tropical cyclones, and marine conditions.

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