Indicator: A-41 Greenhouse - climate change projections
Data
Ranges of average annual warming(°C) for around 2030 and 2070 relative to 1990
Source: CSIRO Atmospheric Research 2001, Climate Change Projections for Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/projections2pp.pdf
Range of annual average rainfall change(%) for around 2030 and 2070 relative to1990
Source: CSIRO Atmospheric Research 2001, Climate Change Projections for Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/projections2pp.pdf
| Now | 2030 | 2070 | |
|---|---|---|---|
| Alice Spring | 28.6 | 29.8 ± 0.8 | 32.1 ± 2.5 |
| Adelaide | 21.4 | 22.4 ± 0.7 | 24.4 ± 2.2 |
| Brisbane | 25.5 | 26.5 ± 0.7 | 28.5 ± 2.2 |
| Broome | 32.2 | 33.4 ± 0.8 | 35.7 ± 2.5 |
| Cairns | 28.9 | 29.9 ± 0.7 | 31.9 ± 2.2 |
| Darwin | 31.9 | 33.1 ± 0.8 | 35.4 ± 2.5 |
| Melbourne | 19.8 | 20.8 ± 0.7 | 22.8 ± 2.2 |
| Perth | 23.3 | 24.3 ± 0.7 | 26.3 ± 2.2 |
| Sydney | 22.1 | 23.3 ± 0.8 | 25.6 ± 2.5 |
1 The quoted uncertainties represent the full range obtained from nine different climate models and forty emissions scenarios.
Source: CSIRO and AGO 2002, Future Climate Change in Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/cechet_2002a.pdf
| Now | 2030 | 2070 | |
|---|---|---|---|
| Alice Spring | 55 | 63 ± 5 | 73 ± 11 |
| Adelaide | 10 | 13.5 ± 2.5 | 21 ± 7 |
| Brisbane | 2.5 | 4.5 ± 1.5 | 20 ± 15 |
| Broome | 17 | 36 ± 17 | 57 ± 30 |
| Cairns | 3 | 5.5 ± 2.5 | 41 ± 35 |
| Darwin | 1 | 7.5 ± 5.5 | 42 ± 37 |
| Melbourne | 8 | 10.5 ± 1.5 | 15 ± 5 |
| Perth | 15 | 19 ± 3 | 29 ± 10 |
| Sydney | 2 | 3 ± 1 | 7 ± 4 |
Source: CSIRO and AGO 2002, Future Climate Change in Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/cechet_2002a.pdf
| Now | 2030 | 2070 | |
|---|---|---|---|
| Alice Spring | 285 | 295 ± 20 | 315 ± 65 |
| Adelaide | 454 | 435 ± 35 | 400 ± 110 |
| Brisbane | 1146 | 1100 ± 90 | 1010 ± 275 |
| Broome | 596 | 570 ± 95 | 525 ± 285 |
| Cairns | 2028 | 1945 ± 160 | 1785 ± 485 |
| Darwin | 1710 | 1710 ± 70 | 1710 ± 205 |
| Melbourne | 657 | 630 ± 50 | 580 ± 155 |
| Perth | 869 | 800 ± 105 | 660 ± 310 |
| Sydney | 1102 | 1070 ± 70 | 970 ± 265 |
Source: CSIRO and AGO 2002, Future Climate Change in Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/cechet_2002a.pdf
Source: CSIRO Atmospheric Research 2001, Climate Change Projections for Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/projections2pp.pdf
What the data mean
Figure 1 shows simulated ranges of warming for Australia. By 2030, annual average temperatures are 0.4 to 2.0°C higher over most of Australia, with slightly less warming in some coastal areas and Tasmania, and the potential for greater warming in the north-west.
By 2070, annual average temperatures are increased by 1.0 to 6.0°C over most of Australia with spatial variation similar to those for 2030. The range of warming is greatest in spring and least in winter. In the north-west, the greatest potential warming occurs in summer.
Model results indicate that future increases in daily maximum and minimum temperature will be similar to the changes in average temperature. This contrasts with the greater increase in minima than maxima observed over Australia in the 20th century.
Changes in daily temperature extremes can be influenced by changes in daily variability and changes in average maximum or minimum temperature. CSIRO modelling results for Australia indicate that future changes in variability are relatively small and the increases in average maximum and minimum temperature mainly determine the change in extremes.
Figure 2 shows changes in annual average rainfall for around 2030 and 2070, relative to 1990. Changes tend toward a decrease in the south-west (-20% to +5% by 2030 and -60% to +10% by 2070), and in parts of the south-east and Queensland (-10% to +5% by 2030 and -35% to +10% by 2070). Most other locations show changes that vary from -10% to +10% by 2030 and -35% to +35% by 2070.
Source: CSIRO Atmospheric Research 2001, Climate Change Projections for Australia, viewed 22 Mar 2006, http://www.cmar.csiro.au/e-print/open/projections2pp.pdf.
Tables 1, 2 and 3 show projections for temperatures and rainfall for various Australian cities for 2030 and 2070 estimated by CSIRO and the Australian Greenhouse Office. They have projected that temperatures will increase by around 1 degree by 2030 (± 0.8) and by between 3 and 3.5 degrees by 2070 (± 2.5). In terms of rainfall, most locations show a 4% decrease in rainfall by 2030 and a 12% decrease by 2070.
Data Limitations
The projections are based on results from computer models that involve simplifications of real physical processes that are not fully understood. The data represents scenarios based on assumptions. Different assumptions may produce different results.
Issues for which this is an indicator and why
Atmosphere — Climate variability and change - Greenhouse
Greenhouse gas emissions and atmospheric concentrations are measurable, and provide insight into the potential for climate change. Weather phenomena are also measurable but may be indicative of either climate change or of natural fluctuations. Neither provides useful insight into what we may expect in terms of long-term changes of climate. Modelling of how climate might be changing and might change over the course of the next century is probably the only useful indicator for this.
Other indicators for this issue:
- A-07 Greenhouse - carbon dioxide concentrations and growth rates
- A-08 Greenhouse - change in total carbon dioxide equivalent emissions by gas
- A-38 Greenhouse - methane concentrations and growth rates
- A-39 Greenhouse - nitrous oxide concentrations and growth rates
- A-40 Greenhouse - change in total carbon dioxide equivalent emissions per capita and gross domestic product
- A-42 Greenhouse - carbon dioxide equivalent emissions by sector
- A-43 Greenhouse - carbon dioxide equivalent emissions by primary fuel type
- A-44 Greenhouse - carbon dioxide equivalent emissions by mode of travel and road transport emissions by vehicle type
- A-45 Greenhouse - agricultural sector carbon dioxide equivalent emissions
- A-46 Greenhouse - carbon dioxide equivalent emissions from land use, land use change and forestry
- Greenhouse - climate change projections
- LD-05 Terrestrial carbon loss rate and rate of land carbon sequestration
- LD-39 Change in biomass stock
- CO-03 Sea level
- CO-04 Sea surface temperature variability
- CO-44 Marine chlorophyll concentration
- CO-60 Sea salinity
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
- AAT-15 Glacier movement
Land — Contributions and pressures between the land and the atmosphere - Climate
Climate change projections can assist in the analysis of climatic pressures and climate driven changes to the land and terrestrial biodiversity.
Other indicators for this issue:
- LD-05 Terrestrial carbon loss rate and rate of land carbon sequestration
- LD-24 Severe drought and wildfire correlation
- A-01 Annual variation in the Southern Oscillation Index
- A-02 Rainfall trends - annual mean rainfall
- A-03 Rainfall extremes - inter-annual variations in annual extreme rainfall
- A-04 Temperature trends - annual mean temperature anomalies
- A-05 Temperature extremes - percentage area of extreme annual mean temperatures
- BD-15 Examples of impacts of climate variability on selected species, habitats or ecosystems
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
- AAT-15 Glacier movement
- A-45 Greenhouse - agricultural sector carbon dioxide equivalent emissions
Coasts and Oceans — Contributions and pressures between the coasts and oceans and the atmosphere - Climate and carbon dioxide
Climate change projections can assist in the analysis of climatic pressures on the oceans and marine biodiversity.
Other indicators for this issue:
- CO-03 Sea level
- CO-04 Sea surface temperature variability
- CO-44 Marine chlorophyll concentration
- CO-60 Sea salinity
- CO-72 Changes in sea acidity/alkalinity
- CO-76 Examples of the impact of climate variability on selected coastal and marine species, habitats or ecosystems
- A-01 Annual variation in the Southern Oscillation Index
- BD-15 Examples of impacts of climate variability on selected species, habitats or ecosystems
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
- AAT-15 Glacier movement
Coasts and Oceans — Condition of the ocean and coastal waters - Climatic and carbon dioxide factors
Climate change projections can assist in the analysis of climate driven changes to the condition of the oceans and marine biodiversity.
Other indicators for this issue:
- CO-03 Sea level
- CO-04 Sea surface temperature variability
- CO-44 Marine chlorophyll concentration
- CO-60 Sea salinity
- CO-72 Changes in sea acidity/alkalinity
- A-01 Annual variation in the Southern Oscillation Index
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
- AAT-15 Glacier movement
Biodiversity — Pressures on biodiversity - Climate variability
Climate change projections can assist in the analysis of climatic pressures and climate driven changes to terrestrial, aquatic and marine biodiversity.
Other indicators for this issue:
- BD-15 Examples of impacts of climate variability on selected species, habitats or ecosystems
- LD-05 Terrestrial carbon loss rate and rate of land carbon sequestration
- LD-24 Severe drought and wildfire correlation
- CO-03 Sea level
- CO-04 Sea surface temperature variability
- CO-44 Marine chlorophyll concentration
- CO-60 Sea salinity
- CO-76 Examples of the impact of climate variability on selected coastal and marine species, habitats or ecosystems
- A-01 Annual variation in the Southern Oscillation Index
- A-02 Rainfall trends - annual mean rainfall
- A-03 Rainfall extremes - inter-annual variations in annual extreme rainfall
- A-04 Temperature trends - annual mean temperature anomalies
- A-05 Temperature extremes - percentage area of extreme annual mean temperatures
- AAT-15 Glacier movement
- A-36 Rainfall extremes - percentage area experiencing extreme wet and dry conditions
- A-37 Temperature trends - spatial trend in mean annual temperatures
- A-47 Rainfall deficiencies - drought
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
Inland Waters — Catchment scale influences - Influence of climate variability and change
Climate change projections can assist in the analysis of climatic pressures and climate driven changes to freshwater systems and aquatic biodiversity.
Other indicators for this issue:
- A-01 Annual variation in the Southern Oscillation Index
- A-02 Rainfall trends - annual mean rainfall
- A-03 Rainfall extremes - inter-annual variations in annual extreme rainfall
- A-04 Temperature trends - annual mean temperature anomalies
- A-05 Temperature extremes - percentage area of extreme annual mean temperatures
- A-36 Rainfall extremes - percentage area experiencing extreme wet and dry conditions
- A-37 Temperature trends - spatial trend in mean annual temperatures
- A-47 Rainfall deficiencies - drought
- LD-24 Severe drought and wildfire correlation
- BD-15 Examples of impacts of climate variability on selected species, habitats or ecosystems
- AAT-12 Changes in colonies of plants on Heard Island
- AAT-14 Ice sheet mass balance and sea ice extent
- AAT-15 Glacier movement
Human Settlements — Services provided by the environment to human settlements - Air
A tolerable climate is one of the key services provided to human settlements by the atmosphere. Greenhouse gas projections provide information on changes in the capacity of the atmosphere to provide that service.
Further Information
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