Warm nights for Queensland

Northern Aust Seasonal Temperature Outlook: probabilities for May to July 2012, issued 24th April 2012

Warm nights for Queensland

The northern Australian temperature outlook for May to July 2012 shows:

  • Queensland is more likely to see warm nights this season
  • cooler days more likely over southern Queensland and the southwest NT
  • This outlook is strongly influenced by warmer than normal waters in the Indian Ocean. Cooler than normal tropical Pacific waters associated with the 2011-12 La Niña have had a lesser impact.

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

    The chance that the average minimum temperature for May to July will exceed the long-term median minimum temperature is greater than 60% across Queensland, with odds greater than 75% in Queensland's southeast. This means that for every ten years with ocean patterns like the ones currently observed, about six to eight would be expected to be warmer than average, with the other two to four being cooler. Most of the NT has a near equal chance for above average temperatures, with higher odds for warm minimum temperatures along the eastern border and in the Gulf Country (see map above).

    History shows the oceans' effect on minimum temperatures during the May to July period to be moderately consistent across the NT and Queensland.

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

    The chance that the average May to July maximum temperature will exceed the long-term median maximum temperature is between 30 and 40% over the the southwest NT and southeast Queensland. In other words, there is a 60 to 70% chance of cooler days over this region.

    Outlook confidence is related to how consistently the Pacific and Indian Oceans affect Australian temperatures. During the May to July period, history shows this effect on maximum temperatures to be moderately consistent across tropical Australia. The effect is very weak in southern Queensland and the Alice Springs District of the NT for this time of year. (see background information). Users should exercise caution in these areas of low skill.


    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:

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



    Corresponding rainfall outlook

    Maximum temperature departures from average for January to March 2012 - base period 1961-1990

    Minimum temperature departures from average for January to March 2012 - 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. 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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