Hi all – yes, it’s that time of year again. We are all busy, whether we want to be or not. It can be so at work or just with family and friends. Whatever the cause (usually associated with the silly season of course), it impacts on what we normally do. It is, of course, the case with Blog posting also. I’ll still be posting, however, I can’t be sure just how often I’ll be able to do so. So the ‘moral’ of the story – there may not be as many posts over the next couple of week, until at least the 4th of January 2016. I’m also hoping to take a short break or two – so that will also impact on posting.
Anyway all the best to you all at this time of year and may it be safe, healthy and fun.
The Millennium Drought ended more than five years ago, but several years of below-average rainfall and El Niño have brought drought back to many parts of Australia. Our latest report on water in Australia shows rainfall is continuing to decline in eastern Australia and increase in the north.
However in urban areas, where water use has not changed significantly since the Millennium Drought, more water is available for use thanks to technologies such as desalination and recycling.
In a recent article on The Conversation, the Bureau of Meteorology put the case that Australia can now better manage water resources using new water information capability.
Last week the Bureau released a new assessment report on our national water availability and use. Water in Australia 2013–14 examines climatic conditions and the physical hydrology to create the most recent national assessment of Australia’s water resources.
The main findings are outlined below.
Since 1950, rainfall has increased in Australia’s north and northwest, but declined along the west coast and most of eastern Australia. This pattern was reflected in 2013–14.
Rainfall affects streamflow and groundwater replenishment, which in turn affects our available water resources.
In southern Queensland and northern New South Wales, a severe drought, which started in 2012, continued in 2013–14. As expected, streamflow in these areas was very much below average in drought-impacted areas.
The volume of groundwater stored in aquifers is very large compared with surface water and responds more slowly to external influences. As a result, most bores across the country had average groundwater levels in 2013–14.
In South Australia and Queensland, more than one-third of all bores had an above-average level. Below-average groundwater levels were present in 5–20% of bores in each State and Territory.
Australia has extensive water supplies and their use is managed by various institutional arrangements. Water availability is being increased by using recycled and desalinated water. At the same time, greater protection is being afforded to the environment through the purchase of entitlements from water users and investments in water-saving infrastructure.
Since the Millennium Drought, Australia’s water market has thrived, facilitating the buying and selling of water rights to allow water to be moved and put to more effective use. Entitlement trade increased in 2013–14 to about 2400 gigalitres (GL), and can partly be attributed to entitlements being transferred to the Commonwealth for the environment and partly to declining water storage levels that prompt buyers into the market to secure more water. Allocation trade in 2013–14 was around 5500 GL.
As well as ensuring sustainable water supply for human needs, water resources are managed to ensure that environmental needs are met. Environmental water holders in the Murray–Darling Basin held 3192 GL of surface water entitlements at the end of 2013–14 (increasing from 3160 GL at the end of 2012–13). Of the total allocated environmental water available in 2013–14, 68% was delivered for environmental purposes and 27% was carried over to 2014–15.
Total water use across Australia was estimated at 23 500 GL in 2013–14. Irrigation (57% of total use) and urban consumption (17% of total use) were the top two water uses.
The main irrigation use in 2013–14, at just over 9500 GL, was in the Murray–Darling Basin. The estimated total surface water use for irrigation in the Murray–Darling Basin decreased from 11 000 GL in 2012–13 to about 8400 GL in 2013–14—a drop of 24%.
Groundwater use for irrigation increased by 18%, to 1100 GL, because of drier conditions and limited surface water allocation announcements — particularly in the northern Basin.
Outside the Basin, 3900 GL were used for irrigation, mainly in the Queensland and Victorian coastal regions, the coastal regions surrounding Perth and Adelaide, northeastern Tasmania, and in the Ord irrigation scheme in northern Australia.
Urban residential use in 2013–14 was 185 kilolitre per property, up 3% from 2012–13. However, use per property has not increased significantly from the levels at the end of the Millennium Drought. Total water use in 2013–14 in the major cities showed no significant changes from the recent past.
Though water availability exceeded use in 2013–14, shortages were experienced across large parts of the continent. With Australia’s highly variable and changing climate there will be ongoing challenges to meet the water needs of our nation.