Warmer temperatures favoured for all of southeast Australia

Southeastern Aust Seasonal Temperature Outlook: probabilities for January to March 2011, issued 17th December 2010

Warmer temperatures favoured for all of southeast Australia

The outlook for maximum and minimum temperatures averaged over the January to March period favours warmer daytime and night time temperatures across all of southeast Australia. Warmer conditions are particularly favoured to occur across Victoria, southeastern South Australia and southwestern New South Wales.

The pattern of seasonal temperature odds across Australia is a result of recent warm conditions in the Indian Ocean as well as cool conditions in the equatorial Pacific Ocean associated with the current La Niña event.

The chance that the average January to March maximum temperature will exceed the long-term median maximum temperature is more than 65% across almost all areas of New South Wales, Tasmania and South Australia, with particularly strong probabilities (greater than 75%) across most of Victoria, southwestern New South Wales and southeastern South Australia. This means that for every ten years with ocean patterns like those currently observed, about six to eight years would be expected to be warmer than average during this summer, with about two to four being cooler.

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

Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian temperatures. During the March quarter, history shows the effect on maximum temperatures to be strongly consistent over northeastern New South Wales, and moderately consistent over Victoria, Tasmania, and South Australian agricultural areas. The effect is weak or very weak in southeastern New South Wales and South Australian pastoral areas. (see background information).

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

The average minimum temperature for January to March is likewise favoured to be above the long-term median minimum temperature for all of southeast Australia, with the strongest odds, in excess of 75%, over southeastern South Australia, western Victoria and southwestern New South Wales.

History shows the oceans' effect on minimum temperatures during the March quarter to be moderately to strongly consistent over almost all of southeast Australia.

 

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 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:

Sydney -(02) 9296 1555
Adelaide -(08) 8366 2664
Melbourne -(03) 9669 4949
Hobart -(03) 6221 2043

 

THE NEXT ISSUE OF THE SEASONAL OUTLOOK IS EXPECTED BY 20th January 2011

Corresponding rainfall outlook

Maximum temperature departures from average for September to November 2010 - base period 1961-1990

Minimum temperature departures from average for September to November 2010 - 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.

  • 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)

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