The Department of Environment and Science (DES) monitors sea-surface temperature (SST) anomalies in key regions of the Pacific Ocean over autumn, winter and spring, and provides objective outlooks for summer (November to March) rainfall on this basis. The Science Division of DES considers that the probability of ‘near-average’ summer (November to March) rainfall is higher than normal for most of Queensland, whereas the probability of either a ‘wet’ or ‘dry’ summer is lower than normal. Read more (PDF)
Rainfall in Queensland over spring and summer is influenced by the El Niño-Southern Oscillation (ENSO) – a coupled atmospheric and oceanic phenomenon which is strongly persistent at seasonal timescales. Values of key ENSO indices, including the Southern Oscillation Index (SOI) and SSTs in the central equatorial Pacific Ocean, tend to ‘lock-in’ during spring (August to October) and persist through summer (November to March). The SST anomaly in the key Niño 3.4 region of the Pacific over spring was warmer than normal (+0.5°C) and the average value of the SOI was minus 4.2. These values, whilst close to El Niño thresholds, remain within the ENSO-neutral range.
The most recent rainfall outlook from the Bureau of Meteorology (http://www.bom.gov.au/climate/outlooks/) indicates a higher than normal probability of below-median rainfall across much of Queensland from November to January. This three-month outlook is based on the Bureau’s ACCESS-S1 global climate model, which has recently replaced POAMA as the basis of the Bureau’s seasonal prediction system.
DES independently calculates rainfall probabilities for the Queensland summer (November to March) based on an experimental system known as SPOTA-1 (Seasonal Pacific Ocean Temperature Analysis - version 1). SPOTA-1 provides an objective comparison of historical summer rainfall with Pacific Ocean SST anomalies from March through to October each year. The final SPOTA-1 update for 2018 indicates, for most of Queensland, a higher than normal probability of ‘near-average’ (Decile 3 to 7) summer rainfall, and a lower than normal probability of either a ‘wet’ or ‘dry’ summer (> Decile 7 or < Decile 3 summer rainfall respectively). On the same basis, the probability of above-median summer rainfall is near-normal for most of Queensland.
It should be noted that seasonal outlooks are probabilistic, rather than deterministic, in nature. For example, if an outlook is described as having a 60 per cent probability of above median rainfall, there is also a 40 per cent probability of below median rainfall. In cases where outcomes with a high probability may be more likely, this does not mean that less probable events will not occur in any given year.
For more information please contact Ken Day at: firstname.lastname@example.org.