Northern Aust Seasonal Temperature Outlook: probabilities for May to July 2011, issued 19th April 2011
The north Australian outlook for mean maximum temperatures averaged over the start of the dry season (May to July period), shows a mixed pattern of odds. Cooler than normal daytime and night-time temperatures are favoured in most areas, however warmer nights are favoured across southern Queensland.
The pattern of seasonal temperature odds across north Australia has been produced using recent Pacific and Indian Ocean temperature patterns. This outlook is a result of cool conditions in the central tropical Pacific Ocean associated with the current La Niña, as well as warm conditions in the Indian Ocean.
The chance that the average May to July maximum temperature will exceed the long-term median maximum temperature is below 40% across the southwestern Northern Territory, as well as in southeast Queensland (see map). This means that for every ten years with ocean patterns like the ones currently observed, about six May to July periods would be expected to be cooler than average in these areas, with about four being warmer.
Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian temperatures. During the May to July period, history shows the effect on maximum temperatures to be consistent to moderately consistent across over the northern halves of Queensland and the Northern Territory elsewhere the effect is weak or very weak (see background information).
The average minimum temperature for the start of the dry season (May to July) is favoured to be above the long-term median minimum temperature across most of Queensland. The largest probabilities of 75 to 80% occur in southeast Queensland. In contrast, the outlook favours cooler night-time temperatures over most of the Northern Territory, with the largest probabilities of 40 to 45% being located in central-western NT.
History shows the oceans' effect on minimum temperatures during the May to July period to be moderately consistent over most of the Northern Territory and Queensland.
Click on the maps above for larger versions of the maps. Use the reload/refresh button to ensure the latest forecast maps are 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 24th May 2011
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.
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 past El Niño events since 1900 are summarized on the Bureau's web site (El Niño - Detailed Australian Analysis), and past La Niña events (La Niña - Detailed Australian Analysis)
© Australian Government, Bureau of Meteorology