Continuing increased rainfall odds for southeast Queensland

Northern Aust Seasonal Rainfall Outlook: probabilities for May to July 2010, issued 22nd April 2010

Continuing increased rainfall odds for southeast Queensland

The northern Australian outlook for total rainfall over the first three months of the northern dry season, May to July, shows a moderate to strong shift in the odds favouring a wetter than normal quarter over southern parts of Queensland.

The pattern of seasonal rainfall odds across northern Australia has been produced using recent Pacific and Indian Ocean temperature patterns. The Indian Ocean is dominant in this outlook with reinforcement from the Pacific.

probability of exceeding median rainfall - click on the map for a larger version of the map

The chances of exceeding the median rainfall for May to July are above 60% over the southern third of Queensland (see map). Within this region, the chances of a wetter than normal three months exceed 75% in an area straddling the NSW/Qld border centred near Goondiwindi.

This means that for every ten years with ocean patterns like the current, about six to eight May to July periods are expected to be wetter than average over this broad region of southern Queensland, while about two to four periods are drier.

Across the rest (and most) of northern Australia, the chances of exceeding the median May to July rainfall are between 40 and 60%, meaning that above average falls are about as equally likely as below average falls. However, it should be noted that in the northern part of the NT, rainfall is commonly low during this period, contributing only a small fraction of the annual total.

An expanded set of seasonal rainfall outlook maps and tables, including the probabilities of seasonal rainfall exceeding given totals (e.g. 200 mm), is available on the "Water and the Land" (WATL) part of the Bureau's website.

Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian rainfall. During the May-July period, history shows this effect to be moderately consistent in a band from the central Northern Territory across most of the southern two-thirds of Queensland. Elsewhere the effect is only weakly or very weakly consistent (see background information).

The El Niño event across the Pacific Basin has continued to break down during the past month. Most leading climate models indicate further cooling and a return to a neutral (near-average Pacific temperatures) pattern by the southern winter. The SOI is approximately +11 for the 30 days ending 19 April. For routine updates and comprehensive discussion on any developments regarding El Niño or La Niña, 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 information on this outlook is available by contacting the Bureau's Climate Services sections in Queensland and the Northern Territory at the following numbers:

Brisbane -(07) 3239 8660
Darwin -(08) 8920 3813

 

THE NEXT ISSUE OF THE SEASONAL OUTLOOK IS EXPECTED BY 25th May 2010

Corresponding temperature outlook

March 2010 rainfall in historical perspective

January to March 2010 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).

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