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Sub-seasonal to seasonal prediction of rainfall extremes in Australia
Corresponding Author
Andrew D. King
School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia
Correspondence
A. D. King, School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia.
Email: [email protected]
Search for more papers by this authorDebra Hudson
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorEun-Pa Lim
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorAndrew G. Marshall
Bureau of Meteorology, Hobart, Tasmania, Australia
Search for more papers by this authorHarry H. Hendon
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorTodd P. Lane
School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia
Search for more papers by this authorOscar Alves
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorCorresponding Author
Andrew D. King
School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia
Correspondence
A. D. King, School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia.
Email: [email protected]
Search for more papers by this authorDebra Hudson
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorEun-Pa Lim
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorAndrew G. Marshall
Bureau of Meteorology, Hobart, Tasmania, Australia
Search for more papers by this authorHarry H. Hendon
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorTodd P. Lane
School of Earth Sciences and ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Victoria, Australia
Search for more papers by this authorOscar Alves
Bureau of Meteorology, Melbourne, Victoria, Australia
Search for more papers by this authorFunding information: Australian Research Council, CE170100023; DE180100638
Abstract
Seasonal climate prediction to date has largely focussed on probabilistic forecasts for above- and below-average conditions in climate means. Here, we examine the possibility of making sub-seasonal to seasonal outlooks for daily-scale precipitation extremes in Australia. We first use observational data to show that significant relationships exist between climate modes, such as the El Niño–Southern Oscillation, and indices representing rainfall extremes across much of Australia. The strong observed teleconnections between climate modes and daily rainfall extremes suggest the potential for predictability on seasonal scales. The current Australian Bureau of Meteorology seasonal prediction system (ACCESS-S1) is examined for performance in predicting rainfall extreme indices using a range of measures. Ensemble hindcasts, consisting of 11 members initialised every month during 1990–2012, perform well for some extreme rainfall indices on short lead-times (up to 1 month). We note that at short lead-times, forecasts are aided by skilful weather prediction, so forecast performance drops at lead-times of a week or more. Forecast performance is lower in austral summer than other seasons and greater in the north and interior of the continent, particularly in the dry season, than elsewhere. The ACCESS-S1 ensemble is overconfident but exhibits some reliability in probabilistic forecasts of above- or below-average number of wet days and intensity of the highest daily maximum precipitation, especially in northern Australia. ACCESS-S1 captures the broad pattern of relationships between climate modes and rainfall extremes that are observed. For two case-studies of unusually extreme precipitation, ACCESS-S exhibits contrasting performance for forecasts of extreme rainfall anomalies beyond the first month. These results suggest that ACCESS-S1 may be used to produce outlooks for some rainfall indices, such as the number of wet days and the intensity of the wettest day, for the month ahead.
Supporting Information
Filename | Description |
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qj3789-sup-0001-Figures.docxWord 2007 document , 2.2 MB |
Figure S1 The difference between the ACCESS-S ensemble median lead-0 and AWAP in Rx1day for each calendar month. Stippling indicates where at least three-quarters of the 11-member ACCESS-S ensemble have differences of the same sign. Figure S2. The average values of Rx1day in each calendar month in AWAP. Mean-averages are computed for the 1990–2012 period consistent with the ACCESS-S hindcast window. Figure S3. Proportion correct of the sign of anomalies in lead-0 ACCESS-S ensemble-median forecasts for Rx1day. The proportion correct is shown for each calendar month. Figure S4. The Brier Skill Score for lead-0 Rx1day forecasts in each calendar month. Figure S5. Maps showing the ranks of most frequently observed total rainfall, Rx1day and WD relative to the ACCESS-S ensembles in the warm (November–April) and cool (May–October) seasons. Figure S6. As Figure 7 but for cool-season months (May–October). Figure S7. As Figure 8 but for northern Australia (north of 26°S) only. Figure S8. As Figure 8 but for southern Australia (south of 26°S) only. Figure S9. Spearman rank correlation coefficients through time for 1911–2017 in AWAP between each pair of rainfall indices in January (top-right half) and July (bottom-left half). |
Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.
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