Mixed rainfall outlook for late spring to mid-summer

The latest seasonal rainfall outlook issued by the Bureau of Meteorology, shows a mixed pattern of odds for exceeding the median rainfall over the late spring to mid-summer period (November-January). Drier than normal conditions are indicated for SE Queensland and much of NSW, whereas above average three-month totals are favoured in western and northern Queensland and in northwest WA.

The pattern of seasonal rainfall odds across Australia is a result of higher than average temperatures in both the Pacific and Indian Oceans. The warm Pacific biases the climate towards drier than average across eastern and northern Australia, but the warm Indian Ocean promotes wetter than average conditions across the tropics and in western WA.

The chances of exceeding the median rainfall for the November to January period, are between 30 and 40% over the eastern half of NSW and in SE Queensland, with a few areas having 25 to 30% chances. These probabilities mean that BELOW median falls have about a 60 to 75% chance of occurring.

So in years with ocean patterns like the current, about six or seven November to January periods out of ten are expected to be drier than average in these parts of eastern Australia, with about three or four out of ten being wetter.

In contrast, two regions - one covering parts of north and west Queensland and the other extending from the northwest to the interior of WA, have a 60 to 65% chance for the three-month rainfall total to exceed the long-term median. This equates to six seasons being wetter than average and four drier for every ten years with ocean temperatures similar to the present.

Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian rainfall. During the November to January period, history shows this effect to be moderately consistent across much of Tasmania, NSW, Queensland and the NT, but generally weakly consistent elsewhere (see background information).

The Southern Oscillation Index (SOI), negative for the fifth straight month, rose from −16 in August to −5 in September. The approximate SOI for the 30 days ending 23rd October was −14.

The current El Niño conditions, of which the low SOI is but one indicator, are very likely to persist for the rest of 2006, which would qualify it as an official El Niño event. For routine updates and comprehensive discussion on the latest data relating to El Niño, together with details on what the phenomenon is and how it has affected Australia in the past, please see the ENSO Wrap-Up.

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Regional versions of this media release are available: | Qld | NSW | Vic | Tas | SA | WA | NT |

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 23^rd NOVEMBER 2006

Corresponding temperature outlook

September 2006 rainfall in historical perspective

July to September 2006 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 (www.bom.gov.au/silo/products/SClimate.shtml).

• 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 23 El Niño events since 1900 are summarized on the Bureau's web site (www.bom.gov.au/climate/enso/).