Indicator: A-01 Annual variation in the Southern Oscillation Index
Data
Southern Oscillation Index - annual
Source: Bureau of Meteorology 2005, Monthly and annual Southern Oscillation Index data.
What the data mean
El Nino events are shown on the graph as the area below zero. La Nina events are shown by the area above zero. The data shows that Australia has been experiencing an El Nino event since 2001. The data also shows that there have been more frequent and severe El Nino events since the mid 1970s than the previous periods. Furthermore, La Nina events are less pronounced.
Data Limitations
Nil
Issues for which this is an indicator and why
Atmosphere — Climate variability and change - Weather
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate.
Other indicators for this issue:
- 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-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
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts 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-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-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
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts on inland waters.
Other indicators for this issue:
- 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-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
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts 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-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-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
Coasts and Oceans — Condition of the ocean and coastal waters - Climatic and carbon dioxide factors
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts on coasts and oceans, especially coastal 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-41 Greenhouse - climate change projections
- 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 — Contributions and pressures between the coasts and oceans and the atmosphere - Climate and carbon dioxide
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts on coasts and oceans, especially coastal 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-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
Australian Antarctic Territory — Environment - Atmosphere, climate and oceans
A number of studies indicate that the El Nino-Southern Oscillation (ENSO) explains 30 - 40% of the year-to-year variability of Australia’s climate, particularly rainfall. The Southern Oscillation Index (SOI) is a well-established measure of this phenomenon. El Nino events are associated with below-normal rainfall and often drought over much of northern and eastern Australia. They generally occur every two to seven years and are generally followed by La Nina events, which are associated with higher rainfall. Changes in the timing of these events may be indicative of longer term changes in climate which may have significant impacts on the Antarctic continent.
Other indicators for this issue:
- AAT-01 Monthly mean air temperature anomalies at Australian Antarctic stations
- AAT-04 Concentrations of greenhouse gases
- AAT-05 Average deep water temperatures
- AAT-06 Average deep water salinity
- A-12 Trend in the area of the ozone hole
Further Information
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