Indicator: A-02 Rainfall trends - annual mean rainfall
Data
Annual Rainfall for Australia
Source: Bureau of Meteorology 2005, Annual all-Australian mean rainfall.
Trend in Annual Total Rainfall: 1900-2004 (mm/10yrs)
Source: Bureau of Meteorology, Australia
Trends in annual total rainfall for three time periods, 1900-2005, 1950-2005 and 1970-2005
Source: Bureau of Meteorology, 2006
What the data mean
Spatially, regional rainfall trends from 1900 to 2004 show both increases and decreases. Large increases (greater than 20 mm per ten years) since 1950, intensifying since 1970, have been observed in north-west Australia. Decreases since 1950, intensifying since 1970, have occurred in all the eastern states, South Australia and much of the Northern Territory.
The rainfall graph shows an increase in annual rainfall averaged across the continent over the reporting period 1900 to 2004. The increase from the mid 1970s is more pronounced. This is interesting given that the area affected by decreased rainfall seems to be greater than the area affected by increased rainfall. It also contrasts with the data relating to the Southern Oscillation Index, which shows that there have been more frequent and severe El NiƱo events (drier periods) since the mid 1970s.
Data Limitations
Nil
Issues for which this is an indicator and why
Atmosphere - Climate variability and change - Weather
Australia is the driest inhabited continent on earth. Its interior has one of the lowest rainfalls in the world and about three-quarters of the land is arid or semi-arid. Rainfall trends are important from an environmental and an economic perspective. For thousands of years, Australia has experienced strong year-to-year variations in rainfall. These natural variations and any more extreme variations or changes in the normal scope of variation that may result from anthropogenic climate change that may result from anthropogenic climate change are important indicators for the condition of the atmosphere.
Other indicators for this issue:
- A-01 Annual variation in the Southern Oscillation Index
- 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-06 Extreme weather-related effects - cost of weather-related disasters
- 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
Land - Contributions and pressures between the land and the atmosphere - Climate
Australia is the driest inhabited continent on earth. Its interior has one of the lowest rainfalls in the world and about three-quarters of the land is arid or semi-arid. Rainfall trends are important from an environmental and an economic perspective. For thousands of years, Australia has experienced strong year-to-year variations in rainfall. These natural variations and any more extreme variations or changes in the normal scope of variation that may result from anthropogenic climate change are important indicators for the pressure of this change on the land.
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-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-41 Greenhouse - climate change projections
- 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
Inland Waters - Catchment scale influences - Influence of climate variability and change
Australia is the driest inhabited continent on earth. Its interior has one of the lowest rainfalls in the world and about three-quarters of the land is arid or semi-arid. Rainfall trends are important from an environmental and an economic perspective. For thousands of years, Australia has experienced strong year-to-year variations in rainfall. These natural variations and any more extreme variations or changes in the normal scope of variation that may result from anthropogenic climate change are important indicators for the pressure of this change on inland waters.
Other indicators for this issue:
- A-01 Annual variation in the Southern Oscillation Index
- 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-41 Greenhouse - climate change projections
- 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
Biodiversity - Pressures on biodiversity - Climate variability
Australia is the driest inhabited continent on earth. Its interior has one of the lowest rainfalls in the world and about three-quarters of the land is arid or semi-arid. Rainfall trends are important from an environmental and an economic perspective. For thousands of years, Australia has experienced strong year-to-year variations in rainfall. These natural variations and any more extreme variations or changes in the normal scope of variation that may result from anthropogenic climate change are important indicators for the pressure of this change on 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-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-41 Greenhouse - climate change projections
- 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
Further Information
Key
Links to another web site
Links to data in the DRS
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