Skip to Main Content
Table 2

Climate indices investigated as potential predictors of Victoria's seasonal rainfall

PredictorsPredictor definitionRegionData source
SOI Anomaly of mean sea level pressure (MSLP) difference between Tahiti and Darwin Pacific KNMI Climate Explorer 
Nino3.4 Average SST anomaly over 5° S–5° N and 170°–120° W Pacific KNMI Climate Explorer 
DMI West Pole Index–East Pole Index: (Average SST anomaly over 10° S–10° N, 50°–70° E) – (Average SST anomaly over 10°S–Equator, 90°–110° E) Indian KNMI Climate Explorer 
PredictorsPredictor definitionRegionData source
SOI Anomaly of mean sea level pressure (MSLP) difference between Tahiti and Darwin Pacific KNMI Climate Explorer 
Nino3.4 Average SST anomaly over 5° S–5° N and 170°–120° W Pacific KNMI Climate Explorer 
DMI West Pole Index–East Pole Index: (Average SST anomaly over 10° S–10° N, 50°–70° E) – (Average SST anomaly over 10°S–Equator, 90°–110° E) Indian KNMI Climate Explorer 
Close Modal

or Create an Account

Close Modal
Close Modal