Issued 3 August 2007

Most states still affected by rainfall deficiencies

At the yearly time-scale, rainfall deficiencies are evident in all states and territories, with the exception of the Northern Territory. As July 2007 was wetter than July 2006 in western WA, Victoria and southeast SA, there was a slight easing of 12-month deficits in those regions compared with the situation at the end of June. However, southeast Queensland, Tasmania and the Eyre Peninsula experienced a drier July this year thereby causing 12-month rainfall deficiencies to expand and intensify.

12-month rainfall deficiencies

For the 12-month period from August 2006 to July 2007, there were serious to severe rainfall deficiencies over southern and eastern Australia in an arc extending across the Eyre Peninsula and southeastern SA, southwest, south-central and northeast Victoria, and the tablelands and western slopes in southeastern NSW. A large part of southeast Queensland was also affected, as were Tasmania (except for the southwest), and parts of western WA between Carnarvon and Perth as well as areas between Wagin and Albany.

Record low falls for this particular 12-month period were recorded southeast of Melbourne, in much of northern and central Tasmania, in the far southeast of SA and along WAs west coast between Shark Bay and districts to the south of Geraldton.

Over the past three months (May to July), rainfall deficiencies have developed in southwest WA between Geraldton and Kalgoorlie and between Kalgoorlie and Esperance, these being areas largely unaffected by 12-month deficiencies.

Click on the map for larger view

Click on the map for larger view
Black and white | High resolution colour

The worst of the long-term deficiencies are likely to remain for some time. For them to be removed by the end of October, for example, falls over the next three months would need to be in the highest 10% of the historical record in some areas, especially near Melbourne, in northern Tasmania, western WA and southeast Queensland.

The deficiencies discussed above have occurred against a backdrop of multi-year rainfall deficits that have severely stressed water supplies in the east and southwest of the country.

An important consideration in the recovery from drought is the different rate at which systems respond to rainfall deficiencies. At the current time, many catchments in eastern Australia are excessively dry from a very protracted period of below average rainfall and above average temperatures. This means that it will take above average rainfall just to produce average runoff, and very considerable rainfall to make a material difference to water storages.