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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 />

5.3.2 Leliefontein<br />

The SAWS observed data <strong>for</strong> winter shows much higher precipitation levels than the GCM observed<br />

data. However, summer precipitation is more comparable, with the SAWS data being slightly higher<br />

than HADAM A2, CSIRO A2 <strong>and</strong> CSIRO B2 <strong>and</strong> lower than ECHAM A2 (Figure 13). ECHAM A2<br />

gets the seasonality of the precipitation incorrect. HADAM A2 displays a precipitation decrease in<br />

both seasons, whereas CSIRO A2, CSIRO B2 <strong>and</strong> ECHAM A2 all indicate an increase, this being<br />

notable in the case of CSIRO A2 <strong>and</strong> CSIRO B2 (Figure 14). Hence, it is evident that the directional<br />

response is unclear.<br />

LELIEFONTEIN<br />

120<br />

100<br />

80<br />

60<br />

40<br />

DJF mm/month<br />

JJA mm/month<br />

20<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 />

Figure 13: Comparison between GCM observed <strong>and</strong> SAWS observed precipitation <strong>for</strong><br />

Leliefontein (in mm/mo)<br />

LELIEFONTEIN<br />

120<br />

100<br />

80<br />

DJF mm/month<br />

60<br />

JJA mm/month<br />

40<br />

20<br />

0<br />

CSIRO<br />

A2<br />

CSIRO<br />

B2<br />

ECHAM<br />

A2<br />

HADAM<br />

A2<br />

SAWS<br />

OBS.<br />

Figure 14: Comparison between GCM future <strong>and</strong> SAWS observed precipitation <strong>for</strong><br />

Leliefontein (in mm/mo)<br />

18

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