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Recommendation 10 |
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The Committee recommends that the Australian Government direct the Australian Building Codes Board to review the Building Code of Australia to ensure that it better provides for energy efficiency standards suitable for varied climate zones. |
5.19 Energy efficiency in buildings is mainly driven through regulating the design of new constructions. The Committee received evidence that encouraging energy efficiency in pre-existing buildings should also be a priority.
5.20 Ms White stated that each year there is an increase of only two percent in Australia’s residential building stock, implying that 98 percent of Australia’s building stock consists of pre-existing buildings. Encouraging energy efficiency in existing buildings could thus deliver a significant reduction in household emissions.[11]
5.21 A range of options are available to reduce energy usage in existing buildings depending on the regional climate:
n increasing insulation and double glazing windows;
n installation of energy efficient ventilation systems;
n installation of energy efficient light bulbs such as fluorescent lamps or LED lighting;
n installation of energy efficient heating systems such as geothermal and solar heating;
n installation of energy efficient cooling systems such as evaporative cooling;
n installation of energy efficient water heating systems such as gas or solar water heaters; and
n upgrading appliances to modern models with higher energy efficiency.[12]
5.22 There is a range of barriers preventing the uptake of energy efficient technologies and practices in existing buildings.
5.23 One of the central factors preventing an increase in energy efficiency in buildings is a lack of the necessary experts to advise on and implement energy efficiency measures. In turn, a lack of supply of experts increases the cost of their services, thus increasing the cost of upgrading the energy efficiency of existing buildings.
5.24 Business operators may lack incentives to invest in increasing the energy efficiency of existing properties. Operators may be focused on short term profits whereas the benefits of increased energy efficiency are generally only realised in the long-term. Thus operators are not likely to choose to invest significant capital in upgrading their current properties.
5.25 In the rental market, any potential benefits from increased energy efficiency will be felt by the tenants through lower energy bills, resulting in little or no benefit to the landlord. Thus, landlords have few incentives to upgrade the energy efficiency of their existing investments.[13]
5.26 The New South Wales Government currently manages the National Australian Built Environment Rating System (NABERS). This is a voluntary national initiative through which property owners can reliably assess the energy efficiency of their properties and seek ways to improve their energy efficiency.[14]
5.27 Australian Government agencies, in conjunction with NABERS and subject to the 2006 Energy Efficiency in Government Operations policy, must meet mandatory energy efficiency targets, and thus reduce the amount of emissions resulting from Government operations. Part of these efficiencies must be gained through achieving a specific level of efficiency, denoted by a star rating, in existing buildings.[15]
5.28 Ms White discussed some of the disadvantages of the star rating system in warmer parts of the Australia:
We need to be careful that any rules that are put in place regarding the building sector do not drive the obsolescence of existing buildings, because that would not be a good environmental outcome. …When you build a new building it takes at least 30 years to reclaim the annual operating energy that could be saved, so it really is not the best environmental outcome to have any policy that drives the knocking down of existing buildings and a preference for new buildings.[16]
5.29 Rather, Ms White advocated a system where improvements on current energy ratings should be sought. For example, an improvement of one star during the reporting period as opposed to having to achieve a mandatory 4.5 star rating. Ms White stated that this form of programme would lessen the dangers of building obsolescence whilst maintaining the incentive for land holders to increase efficiency.[17]
5.30 Ms White outlined a range of mechanisms available to governments to reward increased energy efficiency in homes. Ms White advocated a reduction in council rates or accelerated depreciation for homes with high energy efficiency and grants to assist in retrofitting of energy efficient technologies.[18]
5.31 The Committee has already discussed the impact changes in land use can have on carbon sequestration. However, land use change can also impact the climate more directly. Studies have shown that a reduction in vegetation across a region may affect temperature and rainfall levels in that region.
5.32 The impacts of land clearing on climate can be divided into two categories: biogeochemical and biogeophysical.[19]
5.33 Biogeochemical refers to the transfer between living things and the physical environment.[20] A good example is the ‘water cycle’, which describes the continuous rotation of water between the atmosphere, the land and living things.
5.34 The biogeochemical effect of land clearing is already recognised in climate science through the concept of carbon sequestration: as vegetation is cleared, less carbon dioxide is removed from the atmosphere.[21]
5.35 Biogeophysical refers to the effect of living things on the physical environment. A common example is the use of plants to prevent erosion.[22]
5.36 Biophysical effects on the environment are starting to be considered very seriously as part of the climate change debate. There are four principal biophysical effects of concern to climate scientists:
n a reduction in leaf cover means that less moisture is transmitted to the atmosphere through the process of transpiration resulting in less convective build up;
n as land cover is altered, so are the reflective properties of that area, which means that land clearing changes the ratio of solar radiation absorbed and reflected by a particular region;
n the conversion of woody vegetation to low lying crops and pastures decreases aerodynamic drag in the atmosphere which in turn increases the strength of surface winds; and
n changing the structure of vegetation affects the water runoff patterns across the altered region thus affecting the balance between runoff, evaporation, and surface and sub-soil moisture.[23]
5.37 Studies by Feddema et al, and, in Australia, McAlpine et al, show that land clearing is affecting temperature and rainfall on a regional scale and may even be influencing global weather patterns. [24]
5.38 The evidence indicates that whether a reduction in vegetation will result in a cooling or warming effect depends on the latitude and geographical nature of the region. For example, snow generally reflects more solar radiation than alpine vegetation. A reduction in vegetation in a region with snow cover may result in a larger amount of solar radiation being reflected, which in turn may cause a cooling effect. However in other areas, with different geographical attributes, land clearing may force a warming effect.[25]
5.39 The Australian landscape has undergone a significant amount of land clearing since European settlement. Land clearing in Australia has primarily taken the form of converting native vegetation to pastures and cropland.
5.40 In 2007, researchers from the University of Queensland, Queensland Government, the University of Colorado and the CSIRO completed a study concluding that the clearing of native vegetation has resulted in significant changes in regional climate in Western Australia and eastern Australia.
5.41 The study compared two simulations of the Australian climate for the period 1949-2003. One simulation recreated the climate for this period with pre-European land cover characteristics whilst the other simulation reproduced the climate over this period with modern day land cover characteristics.
5.42 To accurately carry out these simulations, the study used satellite imagery data on leaf area to build a map, with a resolution of eight kilometres, of vegetation in modern-day Australia, reflecting the significant land clearing that has taken place. The map was then used to extrapolate Australia’s pre-European vegetation characteristics where no land clearing had taken place. These two different sets of information were then used to run two climate simulations.[26]
5.43 The simulation showed that modern day land clearing produced significantly higher temperatures than the simulation with no land clearing. These temperature differences showed a correspondence with areas where major clearing of native vegetation had taken place, such as eastern and southwest Western Australia.[27]
5.44 The study further indicated that, in the scenario accounting for modern-day land clearing, the mean summer rainfall in eastern Australia and southwest Western Australia was lower by four to 12 percent and four to eight percent respectively compared to the non-cleared scenario.[28]
5.45 In other words, the study inferred that land clearing increased the severity of drought. In particular, the study concluded that temperatures during the 2002–2003 El Nino event were 0.75-2.0 degrees Celsius higher than they would have been if the land had not been cleared. [29]
5.46 Similar climate modelling studies provide additional evidence for the effect of land clearing on temperatures and rainfall:
n Two separate studies from 1989 and 1992 both modelled climate in the Amazon with and without land clearing. The studies found that where forest had been converted to pasture, there was an increase in temperature and decrease in rainfall. Further, the 1992 study found that the length of the dry season increased in areas where deforestation had taken place.[30]
n A 2002 climate modelling exercise established that changes to the land surface in the Amazon directly affects the circulation patterns of clouds and thus changes the level of rainfall in the Amazon.[31]
n A 2003 study of the Tocantins River in the Amazon demonstrated that deforestation has increased runoff from precipitation in the region, thus altering river flows and soil moisture in the region.[32]
n Finally, a global climate modelling study from 2000 demonstrated that land clearing affects temperature differently depending on the latitude and geographical nature of the region. The study suggested that deforestation in high latitude alpine regions results in a cooling effect.[33]
5.47 Dr McAlpine, a researcher from the 2007 study on land clearing in Australia, advised the Committee that:
…when we start getting the interaction of a drier climate from increased concentrations of carbon dioxide in the atmosphere and we move into a more drought-prone climate, the land surface is going to dry, the vegetation is going to become more stressed, and our ability to keep the remaining vegetation in the landscape is going to become more difficult. Potentially we are going to see a stronger feedback of the land surface on climate, which could actually make our climate change impacts even worse than what is predicted...[34]
5.48 Dr McAlpine further commented on the interconnectedness of the impacts of land clearing across separate regions:
When we change the land use and clear the vegetation, we essentially change the radiative force that is coming off the land surface and also the surface hydrology and the transpiration rates, which then has an impact on the atmosphere—the ability of that atmosphere to produce convective rainfall, which also affects circulation patterns beyond the area where the clearing occurred.[35]
5.49 This proposal is again supported by studies from abroad. A 2004 modelling exercise indicated that land clearing in the Amazonia and Central Africa severely reduces rainfall in the U.S. Midwest during summer and reduces rain fall on the Californian coast in winter.[36] A similar study found that land clearing in Australia and Africa may affect the Asian monsoon season.[37]
5.50 In regard to land clearing’s importance as a driver of climate change Dr McAlpine concluded:
I am confident that I can say that [land clearing] is part of the problem and that climate change is a multidimensional process.[38]
5.51 A key question is the magnitude of land clearing’s effect on climate change. Some studies conclude that whilst the effect of land clearing is perceptible on a regional scale, its overall impact on global average temperatures is minor.[39] However, others argue that the spatial scale of land clearing at a global level is comparable to the size of the oceanic drivers that influence the El Niño.[40] In Dr McAlpine’s view:
… when we come to Australia … I would say that [land clearing] is getting up there to being equal with carbon dioxide in terms of some of its effects. I think it is the interaction between the two. As one changes, it is going to accelerate the feedback of the other ones.[41]
5.52 If Dr McAlpine is correct, then the restoration of cleared vegetation could significantly ameliorate the regional effects on temperature and rainfall of global heating. Dr McAlpine was of the view that the restoration of vegetation in certain regions may lead to higher rainfall and lower temperatures.[42]
5.53 The 2007 Australian climate modelling study, of which Dr McAlpine took part, also recommends that protecting and restoring Australia’s vegetation should be a priority in mitigating the effects of climate change.[43]
5.54 It is the view of the Committee that Dr McAlpine may have identified a way of limiting the effects of global heating in certain regions. This is an area that requires further investigation and is too valuable a possibility to be passed up.
Recommendation 11 |
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The Committee recommends that the Australian Government investigate using revegetation as an adaptation mechanism to reduce temperature and increase rainfall in applicable parts of Australia. |
5.55 This chapter has examined two adaptation strategies for Australia to manage climate change. The Committee has not set out to undertake a thorough review of adaptation strategies, and has limited itself to reporting on those strategies that were presented to it during the course of the inquiry.
5.56 As climate change becomes more noticeable, adaptation strategies are likely to become more important for Australia. We need to begin the process of identifying and developing adaptation strategies now.
Recommendation 12 |
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The Committee recommends that the Australian Government conduct an inquiry into adaptation strategies for climate change. This inquiry should include consideration of projected sea-level rise due to climate change and its impact upon Australian coastal communities and neighbouring countries. |
Kelvin Thomson MP
Chair