Indicator: BD-15 Examples of impacts of climate variability on selected species, habitats or ecosystems
Data
Long-term datasets indicating changes or impacts due to climate variability are scarce. The following from Pittock (2003), Climate Change: An Australian Guide to the Science and Potential Impacts, summarises some studies on the issue.
A general increase in overstorey cover in central Queensland over the second half of the 20th century is forecast, during a period of higher than average rainfall. This contrasts with a trend in Tasmania toward an increased incidence of drought and eucalypt dieback.
Encroachment by Eucalyptus pauciflora into subalpine grasslands has been documented. In the alpine zone, there is evidence of shifts in vertebrate ranges to higher elevations over the thirty-year period to 1999. Records indicate a higher maximum altitudinal distribution for all three macropod species and for four species of introduced mammal, including the rabbit.
The landward transgression of mangroves into saltmarsh environments in the estuaries of Queensland, New South Wales, Victoria and South Australia over the past five decades is a widespread trend, with saltmarsh losses ranging up to 80%. Increases in rainfall and altered tidal regimes are implicated.
In some areas of the Northern Territory, expansion of some tidal creek systems has occurred since the 1940s, invading freshwater wetlands. More than 17 000 ha of formerly freshwater wetlands have been affected and another 35-40% of the plains are threatened. Both sea level rise and increases in rainfall have contributed to this situation.
There have been some major changes in seabird breeding distribution since the late 19th century in the transition zone between tropical and temperate seabird species off the coast of Western Australia. At least eight species have formed new breeding locations well to the south of their historical range and/or have seen marked population increases at their more southerly colonies. These changes correlate with an increased frequency of the El Nio phase of the Southern Oscillation.
Source: Australian Greenhouse Office, 2003, Climate Change: An Australian Guide to the Science and Potential Impacts, Canberra, viewed N/A, http://www.greenhouse.gov.au/science/guide/index.html.
| This lists the most vulnerable species of endemic vertebrates, those that are predicted to lose greater than 50% of their current area of core environment with only a 1 C increase in temperature | |
|---|---|
| FROGS | |
| Thornton Peak Nursery-Frog | Cophixalus sp Thornton Peak |
| Magnificent Broodfog | Pseudophryne covacevichae |
| Pipping Nursery-Frog | Cophixalus hosmeri |
| Northern Barred Frog | Mixophyes sp. Nov. |
| Tangerine Nursery-Frog | Cophixalus neglectus |
| Bloomfield Nursery-Frog | Cophixalus exiguus |
| Mountain Top Nursery-Frog | Cophixalus monticola |
| Northern Tinkerfrog | Taudactylus rheophilus |
| MAMMALS | |
| Atherton Antechinus | Antechinus godmani |
| Mahogany Glider | Petaurus gracilis |
| Daintree River Ringtail Possum | Pseudochirulus cinereus |
| Lemuroid Ringtail Possum | Hemibelideus lemuroides |
| Herbert River Ringtail Possum | Pseudochirulus herbertensis |
| Spotted-tailed Quoll | Dasyurus maculatus |
| SKINKS | |
| Thornton Peak Skink | Calyptotis thorntonensis |
| Bartle Frere Skink | Techmarscincus jigurru |
| Czechura's Litter Skink | Saproscincus czechurai |
| Saproscincus lewisi | Eulamprus frerei |
| Lampropholis robertsi | Glaphyromorphus mjobergi |
| BIRDS | |
| Golden Bowerbird | Prionodura newtoniana |
| Atherton Scrubwren | Sericornis keri |
| Mountain Thornbill | Acanthiza katherina |
Source: Rainforest CRC 2003, Global Warming in the Wet Tropics, Co-operative Research Centre for Tropical Rainforest Ecology and Management, Cairns, viewed N/A, http://www.rainforest-crc.jcu.edu.au/publications/issueSeries/issuesSeries.htm.
The decline in distribution of species richness of regionally endemic terrestrial vertebrates with increasing temperature
Source: Krockenberger, A. K, Kitching, R. L. and Turton, S. M 2003, Environmental Crisis: Climate Change and Terrestrial Biodiversity in Queensland, CooperativeResearch Centre for Tropical RainforestEcology and Management. RainforestCRC, Cairns, viewed N/A, http://www.rainforest-crc.jcu.edu.au/publications/research reports/ReportPDFs/environmentalCrisisResearchReport.pdf.
Tropical forests
Tropical forests of north Queensland are sensitive to climate change. Large changes in the distribution of forest environments were simulated even for relatively modest climate change scenarios. Significant shifts in the extent and spatial distribution of such forests were considered likely, with the strongest effects being felt in the boundary regions between different types of forest such as rainforest and open woodland. It is suggested that most forests in tropical Queensland will in the near future experience climates that are more appropriate to other forest types. Highland rainforests in particular demonstrated strong sensitivity.
Source: Walsh, K, Cai, W, Hennessy, K, Jones, R, McInnes, K, Nguyen, K, Page C and Whetton, P 2002, Climate Change in Queensland under Enhanced Greenhouse Conditions, CSIRO, viewed N/A, http://www.longpaddock.qld.gov.au/ClimateChanges/pub/FullReportHighRes.pdf.
What the data mean
Research indicates that impacts from climate change are occurring now in a range of habitat types including those in alpine, tropical, coastal, brigalow and tidal areas. Many models predict greater impacts in the future.
Data Limitations
Impacts due to climate change are difficult to measure because change can result from the interaction of a number of pressures, including natural fluctuations of climate that may take place over far longer periods than since data collection of any kind commenced. Most data are based on predictive models and data on current impacts on biodiversity are limited.
It is also difficult to obtain trend data in relation to management response to climate variability eg vegetation corridors may be planted to connect climate change refuges but also for other purposes such as salinity control.
Issues for which this is an indicator and why
Biodiversity — Pressures on biodiversity - Climate variability
As there is no continent-wide method of measuring changes that can be directly attributed to climate change across all species and habitats, examples of changes that appear to be directly attributable to this cause is at present the only useful indicator of the pressure of climate change on 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
- 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-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
Inland Waters — Catchment scale influences - Influence of climate variability and change
As there is no continent-wide method of measuring changes that can be directly attributed to climate change across all species and habitats, examples of changes that appear to be directly attributable to this cause is at present the only useful indicator of the pressure of climate change on freshwater 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-41 Greenhouse - climate change projections
- A-47 Rainfall deficiencies - drought
- LD-24 Severe drought and wildfire correlation
- 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
As there is no continent-wide method of measuring changes that can be directly attributed to climate change across all species and habitats, examples of changes that appear to be directly attributable to this cause is at present the only useful indicator of the pressure of climate change on 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
- 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
Land — Contributions and pressures between the land and the atmosphere - Climate
As there is no continent-wide method of measuring changes that can be directly attributed to climate change across all species and habitats, examples of changes that appear to be directly attributable to this cause is at present the only useful indicator of the pressure of climate change on 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
- 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
- A-45 Greenhouse - agricultural sector carbon dioxide equivalent emissions
Further Information
Climate Change Impacts on Biodiversity in Australia, Outcomes of a workshop sponsored by the Biological Diversity Advisory Committee, 1-2 October 2002:
Rainforest CRC:
- Impacts of Climate Change on Rainforest Ecosystems and Biodiversity
- Climate Change - An Australian Guide to the Science and Potential Impacts ( Pittock (ed.) 2003)
- Impacts and Adaptation Working Group
Macquarie University Climate Change Ecology Group:
Qld Department of Natural Resources & Mines:
- Climate changes
- Environmental Crisis: Climate Change and Terrestrial Biodiversity in Queensland (Krockenberger et al. (eds) 2003)
- Natural Resources and Mines - Climatic information
AIMS
- Reefs at Risk: A programme of action (2002)
- The Implications of Climate Change for Australia’s Great Barrier Reef (Hoegh-Guldberg and Hoegh-Guldberg 2004)
- Reef Futures - Homepage
- The problems that climate change causes for wildlife
- National Biodiversity and Climate Change Action Plan 2004-2007
Key
Links to another web site
Links to data in the DRS
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