Land clearing destroys plants and local
ecosystems and removes the food and habitat on which other native species rely. Clearing allows weeds and
invasive animals to spread, affects
greenhouse gas emissions and can lead to
soil degradation, such as
erosion and
salinity, which in turn can affect water quality. The following table shows the native vegetation inventory assessment of native vegetation by type prior to European settlement and as at 2001–2004. (Given in units of square kilometres)
Land condition As the land cover is crucial to land condition, land clearing exerts significant pressure on land condition. Removal of vegetation also leaves soil bare and vulnerable to erosion. Soil stability is essential to avoid
land degradation.
Soil erosion Soil erosion is very significant pressure on land condition because it undermines existing vegetation and habitats and inhibits vegetation and other biotas that inhabit the vegetation from re-establishing, thus resulting in a "negative"
feedback loop. Terrestrial vegetation is a source of nutrient replenishment for soils. If vegetation is removed, there is less biological matter available to break down and replenish the
nutrients in the soil. Exposing soil to erosion leads to further
nutrient depletion.
Salinity Another consequence of land clearing is
dryland salinity. Dryland salinity is the movement of salt to the land surface via groundwater. In Australia, there are vast amounts of salt stored beneath the land surface. Much of
Australian native vegetation has adapted to low rainfall conditions, and use deep
root systems to take advantage of any available water beneath the surface. These help to store salt in the earth, by keeping groundwater levels low enough so that salt is not pushed to the surface. However, with land clearing, the reduced amount of water that previously got pumped up by the roots of the trees means that the
water table rises towards the surface, dissolving salt in the process. Salinity reduces plant productivity and affects the health of rivers and streams. Salinity also affects the lifespan of roads and other infrastructure, affecting the economy and transportation.
Biodiversity Land clearing is a major cause of habitat loss and fragmentation in Australia and is listed as a key threat to many threatened plant and animal species. The removal of native vegetation reduces habitat availability and food and shelter resources, increasing the risk of population decline and extinction. National conservation assessments indicate that habitat loss linked to deforestation affects a large proportion of threatened species. Of approximately 1,250 threatened plant species and 390 threatened terrestrial animal species, land clearing and associated habitat degradation are identified as threats for 964 plant species and 286 animal species. Species affected include Carnaby's cockatoo, the southern cassowary, Bennett's tree-kangaroo, the Cape York rock-wallaby, the black-flanked rock-wallaby, and the koala, which is classified as Vulnerable in Queensland and New South Wales.
Climate change Land clearing contributes to climate change by releasing carbon stored in vegetation and soils and by reducing the capacity of ecosystems to absorb carbon dioxide. When trees are removed or burned, stored carbon is released into the atmosphere, increasing greenhouse gas emissions. Deforestation and forest degradation account for a significant share of global greenhouse gas emissions, and land clearing remains an important source of emissions within Australia's land-use sector. Vegetation loss can also influence local and regional climate conditions by reducing shade and moisture and increasing surface temperatures.
Deforestation and climate extremes An organisation checked the impacts on climate extremes and droughts by analysing daily rainfall and surface temperature output from the Mark 3 GCM. This work, the first of its kind, demonstrated an increase in the number of dry days (35 °C), a decrease in daily rainfall intensity and cumulative rainfall on rain days, and an increase in duration of droughts under modified land-cover conditions. These changes were statistically significant for all years across eastern Australia and especially pronounced during strong
El Niño events. These studies have demonstrated that LCC has exacerbated the mean climate anomaly and climate extremes in the southwest and eastern Australia, thus resulting in longer-lasting and more severe
droughts. == Regional trends ==