The Science Delivery Division of the Department of Science, Information Technology, Innovation and the Arts (DSITIA) notes that there is currently no strong signal for rainfall being either above or below the long-term median over the next three-month period (May to July). DSITIA’s initial long-lead outlook for the 2013/14 summer (November to March) indicates, for much of Queensland, a slightly higher than normal probability of above-median summer rainfall. Read more (PDF, 335K, last updated 04:08PM, 10 May 2013)*
Seasonal forecasts are based on the current and projected state of the ENSO phenomenon and on factors which alter the impact of ENSO on Queensland rainfall (e.g. the Pacific Decadal Oscillation (PDO)).
Historically, by the end of May, ENSO conditions tend to ‘lock in’ and become a more reliable indicator of rainfall for the season ahead. DSITIA will closely monitor ENSO indices including the Southern Oscillation Index (SOI) and sea-surface temperatures in the coming months.
Extensive areas of inland Queensland, and some northern regions, have now experienced well-below average to extremely-low rainfall over the past three- six- and twelve-month periods. As at 1 April,13 of 73 Queensland regional council areas, comprising approximately one-third of the State, were drought declared. These regional councils include Boulia, Burke, Carpentaria, Croydon, Cloncurry, Diamantina, Doomadgee, Etheridge, Flinders, McKinlay, Murweh, Paroo and Richmond. Conversely, water storages remain near capacity in much of central and south-eastern Queensland, which received very high summer rainfall.
There are various approaches used to provide rainfall outlooks. These approaches tend to differ in terms of the components of the climate system that are considered. For this reason, each approach may convey a different outlook, particularly for specific locations.
DSITIA uses two statistical schemes to develop its forecasts of seasonal rainfall:
The experimental SPOTA-1 scheme provides long-lead probabilities of summer (November to March) rainfall for Queensland from mid-April through to mid-November each year. An initial outlook for summer 2013/14 based on the experimental SPOTA-1 scheme is now available. The SPOTA-1 scheme currently indicates, for much of Queensland, a slightly higher than normal probability of above-median summer rainfall. This assessment is based on an index of March sea-surface temperature anomalies which reflect the current ‘cool’ phase of the PDO. This assessment will be modified when the SPOTA-1 scheme takes into account a monthly ENSO index from June through to November this year.
DSITIA’s SOI Phase scheme provides probabilities of rainfall for the coming three-month season based on SOI values over the previous two months. The SOI Phase scheme currently indicates that the probability of above-median rainfall across most of Queensland is 40 to 60 per cent for the next three-month period (May to July). This analysis is based on the SOI being in a ‘Consistently Positive’ phase at the end of April, as discussed further in the Australia's Variable Rainfall poster (PDF, 9.3M, last updated 03:09PM, 29 July 2016)*, or the Department's archive of historical rainfall maps).
Each of the above schemes may have their own particular following. Although such schemes cannot provide outlooks with absolute certainty, users of the information who follow a skilful scheme should benefit from doing so in the long-term. Users should consider the historical track record of any scheme, and such information is becoming increasingly available. DSITIA's Long Paddock website provides an archive of SPOTA-1 reports and past commentaries on the SOI Phase scheme.
Whilst DSITIA places emphasis on the SPOTA-1 and SOI-Phase analyses, a much wider range of information from national and international agencies is also considered. DSITIA pays particular attention to the Bureau of Meteorology’s 'ENSO Wrap-Up' (PDF)* which is updated fortnightly on the Bureau’s website.
ENSO influences other climate variables apart from rainfall (e.g. temperature, pan evaporation and vapour pressure). This means that the impact of ENSO on crop or pasture growth can be stronger than on rainfall alone. The impact of ENSO on pasture growth, for example, is also dependent upon current pasture condition and soil water status. DSITIA’s AussieGRASS model takes these factors into account in producing seasonal pasture growth probabilities.
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