Table 2.
Percentage change in projected or future (2011–2050) drought events relative to historic data (1891–2010) for all die-off sites in the analysis. Historic and future drought attributes are based on drought analysis of daily data from CSIRO Mk 3.5, A2 SRES scenario, medium sensitivity. Drought integral refers to the sum of monthly SPEI values during the event. Extreme events are defined as those with duration ≥8 months and where monthly SPEI and MTI values <0.02 and >0.98 percentiles, respectively. The return interval refers to the mean number of years between drought events.
Site | All drought events |
Extreme drought events |
||||||
---|---|---|---|---|---|---|---|---|
% change in mean duration | % change mean intensity | % change mean integral | % change frequency per decade | % change heat waves | % change frequency per decade | Historic return interval (years) | Future return interval (years) | |
Alpha | 76 | 8 | 107 | −12 | 122 | 11 | 14 | 12 |
Armidale | 3 | 1 | 11 | 19 | 66 | 11 | 18 | 16 |
Bollon | 11 | 6 | 18 | 48 | −55 | 48 | 21 | 8 |
Canberra | −10 | 6 | −2 | 36 | 72 | 85 | 18 | 10 |
Charters Towers | 29 | 9 | 35 | 16 | 49 | 11 | 25 | 25 |
Cobar | 30 | 15 | 47 | 44 | 184 | 122 | 18 | 7 |
Cooma | −16 | 14 | −9 | 48 | 82 | 27 | 14 | 12 |
Hobart | 35 | 2 | 42 | −9 | 118 | −26 | 41 | 49 |
Ipswich | 22 | 1 | 31 | 24 | 90 | 91 | 31 | 8 |
Jarrahdale | 35 | 6 | 42 | 9 | 114 | 11 | 21 | 16 |
Mt Macedon | 26 | 0 | 25 | 38 | 101 | 234 | 25 | 8 |
Mathinna | 32 | 6 | 41 | 2 | 41 | 178 | 62 | 10 |
Yeelirrie | −15 | 8 | −6 | 79 | 117 | 122 | 18 | 7 |
Tumbarumba | 0 | 8 | 4 | 53 | 65 | −36 | 18 | 25 |
Wilcannia | 13 | 15 | 38 | 30 | 98 | 85 | 21 | 10 |
Mean | 18 | 7 | 28 | 28 | 84 | 65 | 24 | 15 |
Min | −16 | 0 | −9 | −12 | −55 | −36 | 14 | 7 |
Max | 76 | 15 | 107 | 79 | 184 | 234 | 62 | 49 |