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Climate variability, climate change and water resource strategies for ...

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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 />

i<br />

Executive summary<br />

Background <strong>and</strong> motivation<br />

In many parts of the world, <strong>variability</strong> in climatic conditions is already resulting in wide ranging<br />

impacts, especially on <strong>water</strong> <strong>resource</strong>s <strong>and</strong> agriculture. <strong>Climate</strong> <strong>variability</strong> is already being observed<br />

to be increasing, although there remain uncertainties about the link to <strong>climate</strong> <strong>change</strong>. However, the<br />

link to <strong>water</strong> management problems is obvious.<br />

Water is a limiting <strong>resource</strong> <strong>for</strong> development in South Africa <strong>and</strong> a <strong>change</strong> in <strong>water</strong> supply could<br />

have major implications in most sectors of the economy, especially in the agriculture sector. Factors<br />

that contribute to vulnerability in <strong>water</strong> systems in southern Africa include seasonal <strong>and</strong> inter-annual<br />

variations in rainfall, which are amplified by high run-off production <strong>and</strong> evaporation rates.<br />

Current modelling scenarios suggest that there will be significant <strong>climate</strong> <strong>change</strong> 1 impacts in South<br />

Africa (Hewitson et al. 2005). <strong>Climate</strong> <strong>change</strong> is expected to alter the present hydrological <strong>resource</strong>s<br />

in southern Africa <strong>and</strong> add pressure on the adaptability of future <strong>water</strong> <strong>resource</strong>s (Schulze & Perks<br />

2000) . During the past 20 years, most of Africa has experienced extensive droughts, the last three<br />

being 1986-88, 1991-92 <strong>and</strong> 1997-98 (after Chenje & Johnson 1996). If the occurrence of drought<br />

became more frequent, the impact on <strong>water</strong> <strong>resource</strong>s <strong>and</strong> consequently agriculture would be<br />

significant.<br />

Notwithst<strong>and</strong>ing the substantial uncertainties around rainfall projects, there is a tendency <strong>for</strong> the<br />

majority of models to suggest a decrease in rainfall over the western part of southern Africa in the<br />

coming decades. Based on these projections, the most severe impacts are likely to occur in this<br />

region, where small towns <strong>and</strong> subsistence farmers are most vulnerable. The available literature<br />

suggests that it would be prudent to account <strong>for</strong> <strong>climate</strong> <strong>change</strong> in <strong>water</strong> <strong>resource</strong> planning to meet<br />

the development objectives of South Africa. The Minister of Water Affairs, Mr Ronnie Kasrils, has<br />

also acknowledged that “it is possible that the effects of global <strong>climate</strong> <strong>change</strong> will influence the<br />

availability of <strong>water</strong> <strong>and</strong> patterns of use during the next few decades” (Kasrils 2002).<br />

With this in mind, this study investigates the adaptive 2 capacity of small towns <strong>and</strong> communities in<br />

the Northern Cape province to <strong>climate</strong> <strong>variability</strong> 3 , specifically drought. By testing these <strong>strategies</strong><br />

against sustainable development criteria, planning policies <strong>for</strong> national <strong>and</strong> <strong>water</strong> <strong>resource</strong> planning<br />

<strong>and</strong> management are recommended to ensure <strong>water</strong> security against the impacts of <strong>climate</strong> <strong>change</strong>.<br />

Main objectives<br />

1) To demonstrate the <strong>change</strong> in temperature <strong>and</strong> rainfall due to <strong>climate</strong> <strong>variability</strong> <strong>and</strong> projected<br />

<strong>climate</strong> <strong>change</strong> in small towns in the Northern Cape <strong>for</strong> the past 30 years.<br />

2) To document existing coping <strong>strategies</strong> in times of <strong>climate</strong> <strong>variability</strong>, i.e. drought, in small<br />

towns in the Northern Cape.<br />

3) To propose long term <strong>strategies</strong> <strong>for</strong> dealing with the impacts of predicted <strong>climate</strong> <strong>change</strong> in<br />

small towns in the Northern Cape.<br />

1 <strong>Climate</strong> Change: A <strong>change</strong> in <strong>climate</strong> which is attributed directly or indirectly to human activity that alters the<br />

composition of the global atmosphere <strong>and</strong> which is in addition to natural <strong>climate</strong> <strong>variability</strong> over comparable<br />

time periods (Midgley et al. 2005). The time scale would be in decades to centuries.<br />

2 Adaptation: Adjustment in natural or human systems to anew or changing environment. Adaptation to <strong>climate</strong><br />

<strong>change</strong> refers to adjustment in natural or human systems in response climatic stimuli <strong>and</strong> is institutes to<br />

moderate the effects of <strong>climate</strong> <strong>change</strong> (Midgley et al. 2005).<br />

3 <strong>Climate</strong> Variability: Refers to variations in the mean state of the <strong>climate</strong> on all temporal <strong>and</strong> spatial scales beyond<br />

that of individual events. The time scale could be in months to years. (after IPCC 2001b).

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