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Livelihood Security: Climate change, conflict and migration in - UNEP

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In comb<strong>in</strong>ation with volatile global commodity markets,<br />

ex<strong>change</strong> rate fluctuations <strong>and</strong> availability of<br />

food aid, such drops <strong>in</strong> production risk compound<strong>in</strong>g<br />

the rise <strong>in</strong> the price of staples such as rice, corn<br />

<strong>and</strong> wheat. 123 Rises <strong>in</strong> food prices affect the poorest<br />

<strong>and</strong> most vulnerable population groups the most,<br />

<strong>and</strong> can lead to suffer<strong>in</strong>g <strong>and</strong> social unrest.<br />

3.6 Areas vulnerable to sea-level<br />

rise<br />

Map 10 shows coastal areas vulnerable to future<br />

sea-level rise. Five colour categories are used to<br />

illustrate levels of risk relative to elevation, with the<br />

most vulnerable zones be<strong>in</strong>g areas with an elevation<br />

of m<strong>in</strong>us 5 metres (m) below sea-level (l<strong>and</strong><br />

surface only) to 1 m above sea-level. All coastal<br />

regions of up to 5 m <strong>in</strong> elevation have been identified<br />

as potentially at risk because of <strong>in</strong>creased<br />

coastal erosion, saltwater <strong>in</strong>trusion, <strong>and</strong> seawater<br />

<strong>in</strong>undation. Cross-referenced population data <strong>in</strong>dicates<br />

that a 0-1 m rise <strong>in</strong> sea-level could affect over<br />

3 million people <strong>in</strong> this region. More <strong>in</strong>formation on<br />

the l<strong>and</strong> area <strong>and</strong> percentage of the population at<br />

risk from future sea-level rise <strong>in</strong> the study area can<br />

be found <strong>in</strong> Annex 7.<br />

The IPCC predicts an 18-59 cm sea-level rise<br />

globally by the year 2100. However, more recent<br />

reports po<strong>in</strong>t to likely global sea-level rise of close<br />

to a metre or more by the end of the century as<br />

a result of, for example, faster melt<strong>in</strong>g of the ice<br />

sheets <strong>in</strong> Greenl<strong>and</strong>. 124 In the region covered <strong>in</strong> this<br />

report, this rise is expected to have a major effect<br />

on some coastal areas.<br />

The most vulnerable areas shown on the map are<br />

near Nouakchott <strong>in</strong> Mauritania (709,000 <strong>in</strong>habitants),<br />

which is located 2-3 m below sea-level, <strong>and</strong><br />

parts of the coastl<strong>in</strong>e east of Accra <strong>in</strong> Ghana to<br />

Porto-Novo <strong>in</strong> Nigeria, <strong>in</strong>clud<strong>in</strong>g Ben<strong>in</strong>. Much of the<br />

western coastal zone of the Sahel, <strong>in</strong>clud<strong>in</strong>g parts<br />

of Senegal, the Gambia, Gu<strong>in</strong>ea-Bissau, Gu<strong>in</strong>ea,<br />

as well as further south all the way to Sierra Leone,<br />

is also vulnerable due to its low elevation (0-1 m<br />

above sea-level). Furthermore, six of the largest cities<br />

of the region – Lagos (10.5 million <strong>in</strong>habitants),<br />

Abidjan (4.1 million), Dakar (2.8 million), Accra (2.3<br />

million), Conakry (1.6 million) <strong>and</strong> Lomé (1.6 million)<br />

– could be affected as they are located on<br />

the coast, as would smaller cities such as Cotonou,<br />

<strong>Livelihood</strong> <strong>Security</strong>: <strong>Climate</strong> Change, Migration <strong>and</strong> Conflict <strong>in</strong> the Sahel<br />

Banjul, Bissau <strong>and</strong> Porto Novo, <strong>and</strong> dense urban<br />

areas close to the Senegal River, the Saloum Delta,<br />

<strong>and</strong> the Volta Delta. 125 Sea-level rise could also<br />

have an impact on agricultural production that<br />

occurs on or near the coast, <strong>and</strong> cause saltwater<br />

<strong>in</strong>trusion <strong>in</strong>to freshwater lagoons <strong>and</strong> lake systems.<br />

3.7 Synthesis maps<br />

Maps 11 <strong>and</strong> 12 synthesize the <strong>in</strong>formation presented<br />

<strong>in</strong> the four maps show<strong>in</strong>g <strong>change</strong>s <strong>in</strong> temperature,<br />

precipitation, drought <strong>and</strong> flood<strong>in</strong>g (Maps<br />

6-9), with a view to identify<strong>in</strong>g “hotspots.” Map 11<br />

depicts the areas where the most extreme <strong>change</strong>s<br />

<strong>in</strong> these <strong>in</strong>dividual climate <strong>in</strong>dicators have taken<br />

place, while Map 12 considers the four climate<br />

<strong>in</strong>dicators together, highlight<strong>in</strong>g the areas affected<br />

by the most cumulative <strong>change</strong> over the last 40<br />

years. Data on population dynamics <strong>and</strong> <strong>conflict</strong><br />

is also overlaid on these maps.<br />

Map 11 shows clear general trends <strong>in</strong> climate for<br />

the study region, with the north experienc<strong>in</strong>g the<br />

most extreme <strong>in</strong>creases <strong>in</strong> temperature <strong>and</strong> highest<br />

number of droughts, <strong>and</strong> the central areas fac<strong>in</strong>g<br />

a high frequency of flood<strong>in</strong>g. The most significant<br />

<strong>change</strong>s <strong>in</strong> precipitation are found along parts of<br />

the coast, as well as along a belt stretch<strong>in</strong>g from<br />

northern Nigeria <strong>in</strong>to southern Chad. In addition,<br />

the map shows areas where major <strong>change</strong>s <strong>in</strong><br />

<strong>in</strong>dividual climate <strong>in</strong>dicators overlap, <strong>in</strong> particular<br />

<strong>in</strong> western Mauritania, some areas <strong>in</strong> Burk<strong>in</strong>a Faso,<br />

Niger <strong>and</strong> southern Ghana, as well as <strong>in</strong> the northern<br />

parts of Nigeria <strong>and</strong> southern Chad. A more<br />

nuanced analysis of areas affected by cumulative<br />

<strong>change</strong>s <strong>in</strong> the climate <strong>in</strong>dicators is presented <strong>in</strong><br />

Map 12.<br />

The “hotspots” identified <strong>in</strong> Map 12 were determ<strong>in</strong>ed<br />

by “normaliz<strong>in</strong>g” the data for the <strong>in</strong>dividual<br />

<strong>in</strong>dicators – i.e. st<strong>and</strong>ardiz<strong>in</strong>g their values <strong>in</strong> order<br />

to make them comparable to one another. Further,<br />

the four climate <strong>in</strong>dicators were given equal weight<br />

<strong>in</strong> order to analyze their comb<strong>in</strong>ed occurrences<br />

<strong>and</strong> cumulative impact (for more <strong>in</strong>formation on<br />

the methods used, please refer to Annex 3). The<br />

colour cod<strong>in</strong>g used <strong>in</strong> the pie charts for each<br />

hotspot represents the approximate proportional<br />

<strong>in</strong>fluence of each climate <strong>in</strong>dicator for the specific<br />

area. While this simplified methodology does<br />

not <strong>in</strong>corporate population <strong>and</strong> <strong>conflict</strong> variables,<br />

47

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