No significant shifts in winter rainfall odds for southeastern Australia

For southeastern Australia, the outlook for total rainfall over winter (June to August), shows no strong shifts in the odds favouring either wetter or drier conditions. This means the chances of above normal rainfall is about the same as the chance of below normal.

The pattern of seasonal rainfall odds across southeastern Australia is a result of recent warm conditions in the Indian Ocean and an increasing level of warmth in the Pacific. In most of the southeast, the influences from both these oceans provide a very slight bias toward drier conditions, but in northeastern NSW a Pacific Ocean pattern that promotes drier conditions is countered by a Indian Ocean pattern promoting a wetter than normal season.

For the June to August period, the chance of exceeding median rainfall is between 40 and 50% over nearly the whole of the southeastern region (see map). This means that for every ten years with ocean patterns like the current, about four or five years are expected to be wetter than average during winter, while about five or six years are expected to be drier.

In a few small patches along the southern coast of South Australia and Victoria, the chances of a wetter than normal winter drop below 40% indicating an increased risk of dry conditions.

New: Under the WATL part of the Bureau's website, there is an expanded set of seasonal rainfall outlook maps and tables, including the probabilities of seasonal rainfall exceeding given totals (e.g. 200 mm).

Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian rainfall. During winter, history shows this effect to be moderately consistent over most of northern NSW, large areas of Victoria, parts of the pastoral districts and far northeast of SA and the southeast coastal strip of Tasmania. However, confidence is only weakly to very weakly consistent in a band stretching from northwest South Australia, through southern NSW to eastern Victoria. Confidence is also weakly consistent in a second band extending along the southern coast of SA to western Victoria and the west coast of Tasmania

Recent trends in Pacific climate patterns and the latest outputs from computer models indicate an increased risk of an El Niño developing during winter and spring. The SOI is approximately −11 for the 30 days ending 23 May. For routine updates and comprehensive discussion on any developments please see the ENSO Wrap-Up.

Click on the map above for a larger version of the map. Use the reload/refresh button to ensure the latest forecast map is displayed. More detailed forecast maps, including the probabilities of seasonal rainfall exceeding given totals, can be found here.

More information on this outlook is available Monday to Friday from 9.00am to 5.00pm local time by contacting the Bureau's Climate Services sections in Queensland, NSW, SA, Victoria and Tasmania at the following numbers:

THE NEXT ISSUE OF THE SEASONAL OUTLOOK IS EXPECTED BY 23^rd June 2009

Corresponding temperature outlook

April 2009 rainfall in historical perspective

February to April 2009 rainfall in historical perspective

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).