Seasonal Climate Outlook

Recent climate

Rainfall in January was above average for the majority of the wheatbelt and below average for the south-west corner and parts of the Great Southern area of the wheatbelt. Weekly rainfall totals up to 2 February included 108mm in New Norcia, 130mm in Toodyay East, 171mm in Quairading, 92mm in Hyden and 60mm in Esperance Downs. A second cloudband on 9-10 February associated with a tropical low pressure system moving across the Pilbara and Gascoyne brought large falls and major flooding to areas in the Great Southern. Weekly rainfall totals up to 13 February included 134mm in Beverley, 153mm in Esperance, 181mm in Dumbleyung and 239mm in Ravensthorpe. Some of this rain may still be present in the soil at seeding time, but check DAFWA soil water maps and soil water tool.

January SWWA maximum temperatures were average to above average and minimum temperatures were below average to average.

The El Niño–Southern Oscillation (ENSO) remains neutral, and current predictions are generally for neutral conditions. Indian Ocean sea surface temperatures (SSTs) north of Australia are currently cooler than normal. This is probably due to the recent tropical activity in the Kimberley. The Madden Julian Oscillation is in an active phase but has moved out into the Pacific Ocean away from the Australian region. The Bureau is expecting an average to above average number of tropical cyclones this season and despite having recorded only one tropical cyclone so far, numerous tropical lows have had a impact on the climate of WA over the past months. A continuation of this activity could lead to more rainfall for the northern and eastern wheatbelt if lows move through the region (Olwyn in March 2015 and Elaine in March 1999). For a summary of Pacific and Indian Ocean outlooks, see the Climate Model Summary produced by the Bureau.

The influence of the Indian Ocean Dipole (IOD) on Australian climate is weak during December-April. This is due to the monsoon trough shifting south over the tropical Indian Ocean and changing the overall wind circulation, which in turn prevents an IOD ocean temperature pattern from being able to form. Current outlooks suggest a neutral IOD for the end of autumn.

The Southern Annular Mode (SAM), also known as the Antarctic Oscillation (AAO), describes the north–south movement of the westerly wind belt that circles Antarctica, dominating the middle to higher latitudes of the southern hemisphere. SAM is currently negative but is expected to switch to positive in the middle of February. SAM generally has little influence over SWWA in summer.

In January the atmospheric pressure was below normal over the southwest. A persistent sub-tropical ridge (higher than average pressure across the continent) means there is likely to be fewer low pressure systems than average and passing cold fronts may not extend as far north as usual over the next few months.

The table below gives a summary of past month and three month southwest Western Australia (SWWA) climate conditions, and can be used as an indication of what is likely to occur in the near future, if climate conditions follow the current pattern.

Additional information

• Bureau of Meteorology’s severe weather outlook