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The effect of climate change on surface water - CSIRO Land and Water

The effect of climate change on surface water - CSIRO Land and Water

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Calibrati<strong>on</strong> results<br />

Run<str<strong>on</strong>g>of</str<strong>on</strong>g>f (mm)<br />

600<br />

450<br />

300<br />

150<br />

Annual run<str<strong>on</strong>g>of</str<strong>on</strong>g>f vs rainfall Model – observed run<str<strong>on</strong>g>of</str<strong>on</strong>g>f<br />

Bancell Brook – <strong>Water</strong>ous<br />

0<br />

600 800 1000 1200 1400 1600<br />

Rainfall (mm)<br />

1975-1994<br />

1995-2007<br />

• In about half <str<strong>on</strong>g>of</str<strong>on</strong>g> catchments, run<str<strong>on</strong>g>of</str<strong>on</strong>g>f coefficients have reduced over the<br />

recent past (1995 to 2007) – that is, the same amount <str<strong>on</strong>g>of</str<strong>on</strong>g> rainfall<br />

produces less run<str<strong>on</strong>g>of</str<strong>on</strong>g>f<br />

• Our rainfall-run<str<strong>on</strong>g>of</str<strong>on</strong>g>f models are over predicting run<str<strong>on</strong>g>of</str<strong>on</strong>g>f during the recent<br />

period<br />

<strong>CSIRO</strong> South-West Western Australia Sustainable Yields Project – Surface <strong>water</strong><br />

Modelled – observed (mm)<br />

100<br />

50<br />

0<br />

-50<br />

Bancell Brook – <strong>Water</strong>ous<br />

-100<br />

1970 1980 1990 2000 2010<br />

Year

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