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New Australian climate developing
Home › AEGIC News and Stories › New Australian climate developing
PLEASE NOTE: as of June 30, 2016, AEGIC no longer conducts these activities. Dr David Stephens will continue to work in crop and climate forecasting in a private fee-for-service capacity as part of a new venture, Agrometerology Australia. Other private crop forecasting services available in Australia include Australian Crop Forecasters.
Seasonal rainfall zones shift across Australia since 2000
Australian Seasonal Rainfall Zones Based on rainfall data 1990-1999
A new climate is emerging in Australia, according to new maps released by the Australian Export Grains Innovation Centre (AEGIC).
AEGIC analysed data from more than 8000 Bureau of Meteorology stations around the country and discovered that traditional rainfall zones have changed significantly since 2000.
The findings will be presented as part of a talk entitled "South-west Western Australia is losing its Mediterranean Climate" by AEGIC agro-meteorologist Dr David Stephens at the 2016 GRDC Perth Grains Research Update (Perth Convention Centre, 29 February-1 March 2016).
Dr Stephens said the new analysis revealed striking changes to the Australian climate over the past 16 years.
"Since 2000, there has been a general increase in summer rainfall across Australia, and a corresponding decrease in winter rainfall, leading to shifts in rainfall zones extending for hundreds of kilometres," Dr Stephens said.
"Rainfall between May to October over much of the heavily populated regions of southern Australia has decreased 10-30%, while summer rain has increased up to 40% in some areas.
"This change in climate has major implications for farming and pastoral systems as the profitability of different crop types changes, disease risk changes, and the composition of rangeland grasses changes with stocking rates."
The analysis revealed significant shifts in rainfall zones since 2000, which can be seen in the maps above. Summary:
For regions with a Mediterranean climate, winter (and winter dominant) rainfall zones are contracting in a south-westerly direction.
In northern and eastern areas, summer (and summer dominant) rainfall zones are expanding southward.
Between these regions, there is a uniform rainfall zone where summer and winter rainfall are similar. The southern boundary of this zone has shifted from southern/central New South Wales down into central Victoria and the Mallee region of south-east South Australia.
In the south-west of Western Australia, a uniform rainfall zone has appeared along the eastern edge of the wheat-belt from Beacon to Southern Cross to Grass Patch.
Most rainfall zone boundaries have typically shifted 100-400km over the last 16 years. The only expansion of the winter rainfall zone has occurred in southeast Tasmania where winter rainfall has become more reliable.
Dr Stephens said the analysis highlighted that the shift to earlier sowing of winter crops measured recently by AEGIC should continue because early sown crops take advantage of any additional summer soil moisture.
"They also experience a lower evaporative demand through the growing season, and are less affected by declining rain in October and rising spring temperatures," he said.
"In pastoral regions in much of Western Australia, increasing summer rain with a reduction in rainfall variability has assisted perennial C4 (tropical) plants at the expense of C3 (temperate) grasses (especially in southern areas), while in central and northern Queensland, an increase in rainfall variability has been detrimental on pasture production and stocking rates".
"Australia is going to need some of the most water-efficient farming systems in the world to mitigate the effects of a drier and warmer climate in Southern Australia. Research in this area is vital because Australian crop yields have been among the most affected by climate change compared to other grain exporting nations."
These changes appear to be related to changes in barometric pressure, sea surface temperatures and upper level westerly winds.
In the mid-1970s, there was a weakening of the Indian Ocean Trough to the west of Perth which appears to be related to a decline in winter rainfall since then. In the 2000s, this trough has weakened further in conjunction with strengthening high pressures over Australia.
In addition, sea surface temperatures have warmed in all seasons, which is beneficial for summer rainfall.
However, a more marked warming in oceans west of Perth in winter has an inverse relationship to rainfall and has contributed to weaker cloud-band activity in recent years.
At a Hemispheric scale, one of the drivers of weather is the temperature gradient between the equator and the South Pole. This gradient dropped at the beginning of the 2000s as westerly winds in May-July weakened over Australia."
The variability in annual rainfall across Australia has changed since 2000. Reduced variability in some regions is due to the loss of wet years, as in south-west Australia, or more consistent average to above average rain, as in the north-western parts of the country and southern South Australia."
In contrast variability in annual rainfall has increased in inland Victoria, southern New South Wales and much of central Queensland.
Keir Tunbridge
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