The Queensland Climate Change Centre of Excellence (the Centre) considers that the probability of above or below-median rainfall for the next three-month period (May to July) is normal (40-60 per cent) for most of Queensland. This outlook is based on the currently neutral state of the El Niño-Southern Oscillation (ENSO) phenomenon. The current sea-surface temperature pattern in the extra-tropical Pacific indicates a higher than normal probability of above-median rainfall for the coming summer (November to March). Read more (PDF, 237K, last updated 02:12PM, 11 May 2012)*
The Centre’s understanding is 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)). The PDO modulates the impact of ENSO on summer rainfall in Queensland.
The Bureau of Meteorology (BoM) have stated that all major indicators of ENSO lie well within the ENSO-neutral range, with a survey of global models suggesting a continuation of neutral conditions, at least into early winter. BoM also notes an increased risk, indicated by some but not all models, of El Niño conditions evolving during winter or spring (‘ENSO Wrap-Up’ (PDF)* April 24).
As at 1 May 2012, the Centre notes that:
The Centre reaffirms previous advice that, at this time of year (known as the ‘Autumn predictability gap’), ENSO indices are least reliable for seasonal forecasting. The Centre will closely monitor the SOI and sea-surface temperatures in coming months when ENSO conditions tend to ‘lock in’ and become a more reliable indicator of rainfall for the season ahead.
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 and, for this reason, each approach may convey a different outlook, particularly for specific locations.
The Centre produces two statistical climate risk assessment schemes. They are:
The Centre's 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 the upcoming 2012/13 summer, based on the experimental SPOTA-1 scheme is now available and indicates a higher than normal probability of above-median rainfall for much of Queensland. This outlook is based on an index of March sea-surface temperature anomalies in both the South-West Pacific and the North Pacific which, in part, reflect the current ‘cool’ state of the PDO. This outlook will be modified when the SPOTA-1 scheme takes into account a monthly ENSO index from June through to November this year.
The Centre'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 or below-median rainfall for the next three-month period (May to July) is near-normal (50 per cent) for most of Queensland. This analysis is based on the SOI having fallen from March to April as discussed further in the Centre's Australia's Variable Rainfall poster (PDF, 9.3M, last updated 03:09PM, 29 July 2016)*, or the Centre's archive of historical rainfall maps).
The Centre understands that 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 historical information is becoming increasingly available.
The Centre's Long Paddock website provides the historical archive of SPOTA-1 reports and past commentaries on the SOI phase scheme. Users should also consider the wide range of information available each month describing the current state of the ocean/climate system, for example the 'ENSO Wrap-Up' (PDF)*.
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 is also dependent upon current pasture condition and soil water status. The Centre’s AussieGRASS model takes these factors into account in producing seasonal pasture growth probabilities
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