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More droughts, more flooding rains for Australia
by Dr Peter Whetton,
CSIRO DAR
Australia will be
hotter and drier in coming decades according to CSIRO's latest climate
change estimates. "Rising
concentrations of greenhouse gases are the culprit," says Dr Peter Whetton
from CSIRO Atmospheric Research.
In 2001. CSIRO released
these projections regarding the likely extent of climate change in Australia
and the expected impacts across the country."Warmer
conditions will produce more extremely hot days and fewer cold days,"
says Dr Whetton.Over
most of the continent, annual average temperatures will be 0.4 to 2°C
greater than 1990 by 2030. By 2070, average temperatures are likely to
increase by 1 to 6°C. The temperature ranges quoted indicate the
scientific uncertainty associated with the projections.
"The warming won't
be the same everywhere," he says. "There will be slightly less warming
in some coastal areas and Tasmania, and slightly more warming in the north-west."
South-western
Australia can expect decreases in rainfall, as can parts of south-eastern
Australia and Queensland. Wetter conditions are possible in northern and
eastern Australia in summer and inland Australia in autumn.
In areas that experience
little change or an increase in average rainfall, more frequent or heavier
downpours are likely. Conversely, there will be more dry spells in regions
where average rainfall decreases."We
may also see more intense tropical cyclones, leading to an increase in
the number of severe oceanic storm surges in the north. Rises in sea level
would worsen this effect," says Dr Whetton.
Sea level is likely
to rise at a rate of between 0.8 and 8.0 cm per decade, reaching 9 to
88 cm above the 1990 level by the year 2100."Evaporation
will increase over most of the country. When combined with changes in
rainfall, there is a clear decrease in available moisture across the country,"
says Dr Whetton.
Changing climate is
likely to have a profound effect on Australia, with many winners and losers.
"A better understanding
of the likely impacts of climate change can contribute to adaptation strategies
designed to minimise adverse impacts and optimise benefits," says Dr Whetton.
"Natural ecosystems most at risk are coral reefs, alpine ecosystems, mangroves
and wetlands. Also under threat are tropical forests, savannas, deserts
and native grasslands. "Natural
systems have little opportunity to adapt to climate change. Higher temperatures
and lower rainfall will be a threat. Climate change and sea level rise
will add to the vulnerability of many of Australia's wetlands."
Higher carbon dioxide
concentrations will increase plant productivity and the efficiency with
which plants use water. A moderate rise in temperature will increase plant
growth in temperate areas but may reduce it in the north. Warmer
conditions will reduce frost damage to many crops. However, fruit trees
need cold weather to set fruit, so some fruit yields may decline. Wheat
yield will rise with warmer conditions if rainfall doesn't change. A rainfall
decline of 20 per cent with temperature increases of more than 1°C
will lower yield.
"The net effect on
agriculture will be a trade-off between the positive impact of higher
carbon dioxide and the negative effect of lower rainfall and higher temperatures,"
says Dr Whetton. Forests
will benefit from a carbon dioxide-enriched atmosphere, but gains may
be offset by warmer conditions. "Some
tropical pests, like the Queensland fruit fly, may spread southwards.
Other temperate pests, like the light brown apple moth, may move to cooler
areas," says Dr Whetton. "We're also likely to experience more water shortages
and less snow."
CSIRO scientists contribute
to the Intergovernmental Panel on Climate Change, which is the international
group charged with assessing the latest science on greenhouse. CSIRO's
new projections incorporate IPCC findings. CSIRO issued its last climate
change projections in 1996. These new projections suggest a greater temperature
increase than was proposed in the past. Rainfall changes are similar in
direction but greater in magnitude than those released five years ago.
May,
2001
For
more information please contact
CSIRO Atmospheric Research

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