National Seasonal Temperature Outlook: probabilities for July to September 2010, issued 23rd June 2010
The national outlook for temperatures over the period July-September shows a moderate to strong tendency in the odds favouring warmer than normal daytime temperatures over WA, NT, Queensland, and northern NSW. Warmer than normal minimum temperatures are also favoured over most of WA, Queensland, NSW and parts of NT and South Australia.
The pattern of seasonal temperature odds across Australia is due to recent higher than average temperatures in both the Pacific (decaying El Niño) and Indian Oceans.
The chance that the average July-September maximum temperature will exceed the long-term median maximum temperature, is between 60 and 70% over WA, NT, Queensland, and northern NSW, with 70-75% chances across the northern parts of NT and Queensland (see map). This means that for every ten years with ocean patterns like the current, about six to seven July-September periods would be expected to be warmer than average across these areas, while about three to four would be cooler.
Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian temperatures. During July-September, history shows this effect on maximum temperatures to be moderately consistent in WA, the NT, Queensland, northern and eastern NSW, and far northern Tasmania. Elsewhere it is only weakly consistent (see background information). Therefore, this outlook should be used with caution in western NSW and much of SA.
The chance that the average minimum temperature for July to September is favoured to be above the long-term median minimum temperature, is between 60 and 75% over Queensland, most of WA, northern NSW, and parts of northern SA and eastern NT (see map), with chances approaching 85% in parts of western and southern WA. Across the remainder of the country the chances are between 40 and 60%, meaning that a warmer or cooler than normal conditions are both about as equally likely.
History shows the oceans' effect on minimum temperatures during July-September to be moderately consistent over Queensland and the east of the NT, the southern half of WA, and parts of north and east NSW. Elsewhere the effect is only weakly or very weakly consistent.
Click on the maps above for larger versions of the maps. Use the reload/refresh button to ensure the latest forecast maps are displayed.
The following climate meteorologists in the National Climate Centre can be contacted about this outlook: Agata Imielska on (02) 9296 1539, Grant Beard on (03) 9669 4527, David Jones on (03) 9669 4085.
Regional commentary is available from the Climate Services Sections in the Bureau's Regional Offices:
|(07) 3239 8660
|New South Wales -
|(02) 9296 1555
|(03) 9669 4949
|(03) 6221 2043
|South Australia -
|(08) 8366 2664
|Western Australia -
|(08) 9263 2222
|The Northern Territory -
|(08) 8920 3813
THE NEXT ISSUE OF THE SEASONAL OUTLOOK IS EXPECTED BY 22nd July 2010
The Bureau's seasonal outlooks are general statements about the probability or risk of wetter or drier than average weather over a three-month period. The outlooks are based on the statistics of chance (the odds) taken from Australian rainfall/temperatures and sea surface temperature records for the tropical Pacific and Indian Oceans. They are not, however, categorical predictions about future rainfall, and they are not about rainfall within individual months of the three-month outlook period. The temperature outlooks are for the average maximum and minimum temperatures for the entire three-month outlook period. Information about whether individual days or weeks may be unusually hot or cold, is unavailable.
This outlook is a summary. More detail is available from the contact people or from SILO (Seasonal Climate Outlook Products).
Probability outlooks should not be used as if they were categorical forecasts. More on probabilities is contained in the booklet The Seasonal Climate Outlook - What it is and how to use it, available from the National Climate Centre. These outlooks should be used as a tool in risk management and decision making. The benefits accrue from long-term use, say over 10 years. At any given time, the probabilities may seem inaccurate, but taken over several years, the advantages of taking account of the risks should outweigh the disadvantages. For more information on the use of probabilities, farmers could contact their local departments of agriculture or primary industry.
Model Consistency and Outlook Confidence: Strong consistency means that tests of the model on historical data show a high correlation between the most likely outlook category (above/below median) and the verifying observation (above/below median). In this situation relatively high confidence can be placed in the outlook probabilities. Low consistency means the historical relationship, and therefore outlook confidence, is weak. In the places and seasons where the outlooks are most skilful, the category of the eventual outcome (above or below median) is consistent with the category favoured in the outlook about 75% of the time. In the least skilful areas, the outlooks perform no better than random chance or guessing. The rainfall outlooks perform best in eastern and northern Australia between July and January, but are less useful in autumn and in the west of the continent. The skill at predicting seasonal maximum temperature peaks in early winter and drops off marginally during the second half of the year. The lowest point in skill occurs in early autumn. The skill at predicting seasonal minimum temperature peaks in late autumn and again in mid-spring. There are also two distinct periods when the skill is lowest - namely late summer and mid-winter. However, it must always be remembered that the outlooks are statements of chance or risk. For example, if you were told there was a 50:50 chance of a horse winning a race but it ran second, the original assessment of a 50:50 chance could still have been correct.
The Southern Oscillation Index (SOI) is calculated using the barometric pressure difference between Tahiti and Darwin. The SOI is one indicator of the stage of El Niño or La Niña events in the tropical Pacific Ocean. It is best considered in conjunction with sea-surface temperatures, which form the basis of the outlooks. A moderate to strongly negative SOI (persistently below −10) is usually characteristic of El Niño, which is often associated with below average rainfall over eastern Australia, and a weaker than normal monsoon in the north. A moderate to strongly positive SOI (persistently above +10) is usually characteristic of La Niña, which is often associated with above average rainfall over parts of tropical and eastern Australia, and an earlier than normal start to the northern monsoon season. The Australian impacts of 25 El Niño events since 1900 are summarized on the Bureau's web site (El Niño - Detailed Australian Analysis).
© Australian Government, Bureau of Meteorology