Warmer days favoured for large parts of Australia

The national outlook for maximum temperatures averaged over the September quarter (July to September) shows warmer than normal days are favoured for large parts of the country, except in the far south and far north.

The pattern of seasonal temperature odds across Australia is a result of recent warm conditions in the Indian Ocean and an increasing level of warmth in the Pacific. The chance that the average July-September maximum temperature will exceed the long-term median maximum temperature ranges from 60 to 70% across most of WA, the southern halves of both the NT and Queensland, northern SA and all but the southern areas of NSW. In the southeast inland of Queensland the chance approaches 75%. This means that for every ten years with ocean patterns like the current, about six or seven years would be expected to be warmer than average during the September quarter over this broad zone stretching west-east across Australia, with about three or four years being cooler. The chances of a higher than normal seasonal average is between 50 and 60% in the far north, southern SA, southern NSW, Victoria and Tasmania. Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian temperatures. During the September quarter, 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 outlook for mean minimum temperatures over July-September shows the chance of a seasonal average above the long-term median minimum temperature is between 40 and 60% over most of the country. The only exception is across some areas of inland southern WA where the probability of increased warmth is between 60 and 65%. History shows the oceans' effect on minimum temperatures in July to 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.

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Regional versions of this media release are available: | Northern Aust | Southeastern Aust | WA |

Regional commentary is available from the Climate Services Sections in the Bureau's Regional Offices:

THE NEXT ISSUE OF THE SEASONAL OUTLOOK IS EXPECTED BY 24^th July 2009

Corresponding rainfall outlook

Archive of previous National Seasonal Rainfall Outlooks

Archive of previous National Seasonal Temperature Outlooks

Maximum temperature departures from average for March to May 2009 - base period 1961-1990

Minimum temperature departures from average for March to May 2009 - base period 1961-1990

Background Information

• 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).