Southeast Australian rainfall outlook
Issued 28 August 2013
The chance of exceeding the median rainfall for spring is more than 60% over most of southeast Australia. The chance rises to more than 70% over central Victoria. Such odds mean that for every ten years with similar climate patterns to those currently observed, about six to seven spring periods would be expected to be wetter than average over these areas, while about two to three would be drier.
The chance of receiving a wetter or drier than normal spring is roughly equal (i.e., close to 50%) over most of South Australia, with the exception of the southeast where chances exceed 60%.
The negative Indian Ocean Dipole (IOD) event that has been influencing Australian climate since mid-May has weakened over the past four weeks. Despite this, sea surface temperature patterns continue to be consistent with a negative dipole event. The majority of climate models expect this negative IOD event to persist until mid-spring. A negative IOD during winter and spring increases the chances of above-average rainfall over southern Australia. This is reflected in the rainfall outlook, with most of southeast Australia expecting above normal rainfall.
The tropical Pacific has remained ENSO-neutral since mid-2012. The dynamical seasonal outlook model suggests ENSO-neutral conditions will remain for the rest of 2013. This means there is no strong shift in the odds from the tropical Pacific.
Warmer than normal sea surface temperatures currently surround much of western and southern Australia. Warmer sea surface temperatures can provide more moisture to the atmosphere, which in combination with the right weather systems (e.g. interactions with fronts or northwest cloudbands) may result in increased rainfall.
How accurate is the outlook?
Outlook accuracy is related to how consistently the oceans and broadscale climate affect Australian rainfall. During spring, historical accuracy shows the outlook to be moderately consistent over most of southeast Australia. Over western and northern parts of SA and the southern tip of Tasmania the effect is only weakly to very weakly consistent.