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<strong>Climate</strong> <strong>variability</strong>, <strong>climate</strong> <strong>change</strong> <strong>and</strong> <strong>water</strong> <strong>resource</strong> <strong>strategies</strong> <strong>for</strong> small municipalities<br />

5.3.6 Pofadder<br />

All GCM control runs capture the rainfall seasonality represented in the SAWS observed (Figure<br />

21). HADAM A2 slightly over-predicts the observed summer rainfall while CSIRO A2 <strong>and</strong> CSIRO<br />

B2 under-predict the observed. ECHAM A2’s summer rainfall is most akin to the SAWS observed.<br />

All GCMS have a tendency to slightly under-represent the observed winter precipitation. Summer<br />

rainfall increases are suggested in all future GCM scenarios (Figure 22), most notably in the<br />

ECHAM A2 model. Winter rainfall decreases are suggested by HADAM A2 <strong>and</strong> increases by the<br />

other three scenarios.<br />

POFADDER<br />

80<br />

70<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

CSIRO<br />

A2 OBS<br />

CSIRO<br />

B2 OBS<br />

ECHAM<br />

A2 OBS<br />

HADAM<br />

A2 OBS<br />

SAW S<br />

OBS.<br />

DJF mm/month<br />

JJA mm/month<br />

Figure 21: Comparison between GCM observed <strong>and</strong> SAWS observed precipitation <strong>for</strong><br />

Pofadder (in mm/mo)<br />

POFADDER<br />

80<br />

70<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

DJF mm/month<br />

JJA mm/month<br />

CSIRO<br />

A2<br />

CSIRO<br />

B2<br />

ECHAM<br />

A2<br />

HADAM<br />

A2<br />

SAW S<br />

OBS.<br />

Figure 22: Comparison between GCM future <strong>and</strong> SAWS observed precipitation <strong>for</strong><br />

Pofadder (in mm/mo)<br />

22

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