Chapter 4 Climate Impacts and Responses
Introduction
Climate variability and trends impact on Australia’s
economy, environment and society. Australian research
organisations are conducting many research projects to understand
the magnitude of climate change (including natural variability
and human induced climate change) and the physical drivers that
underpin our ability to forecast and manage its impacts.
Australia’s average temperature varies by up to 1 degree
Celsius from year to year, and has experienced a warming trend of
about 0.8°C since 1910, most of this since 1950. Averaged
over Australia, maximum temperatures have risen 0.56°C since
1910 and minimum temperatures have risen 0.96°C, with the
largest warming since about 1950. According to CSIRO projections
released in mid-2001, which use as their reference point the
Third Assessment Report of the Intergovernmental Panel on Climate
Change (IPCC), annual average temperatures over most of the
continent could be 0.4 to 2°C greater than 1990 by 2030. By
2070, average temperatures are projected to increase by 1 to
6°C. Warmer conditions will produce more extremely hot days
and fewer cold days and frosts. Greatest warming is to be
expected in spring and winter will warm the least.
Australia’s current rainfall averaged over the whole
continent is about 450mm a year, varying between 300-800mm in any
year (with the variability much larger in specific regions).
Averaged over Australia, annual total rainfall has increased
slightly since 1910 and the intensity of heavy rainfall has also
risen. According to the CSIRO projections, rainfall decreases are
projected for the southwest of Western Australia and for parts of
the southeast of the continent and Queensland. Most other
locations have an even chance of wetter or drier conditions.
Decreases are projected to be most pronounced in winter and
spring. Some inland and eastern coastal areas are projected to
become wetter in summer, and some inland areas to become wetter
in autumn. These projections include the effect of simulated
changes in El Niño and La Niña events.
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