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

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

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Figure 2 . Mapp<strong>in</strong>g climate hotspots <strong>in</strong> the Sahel<br />

The datasets used for each of the <strong>in</strong>dicators are<br />

described <strong>in</strong> detail <strong>in</strong> Annex 5. Coastal areas vulnerable<br />

to <strong>in</strong>undation based on potential sea-level rise<br />

are shown <strong>in</strong> Map 10. Also calculated us<strong>in</strong>g mapp<strong>in</strong>g<br />

data is the l<strong>and</strong> area <strong>and</strong> the percentage of<br />

the population <strong>in</strong> CILSS countries affected by the<br />

four climate <strong>in</strong>dicators (see Annex 6).<br />

Two synthesis maps comb<strong>in</strong>e the data to identify<br />

“hotspots.” Map 11 depicts the areas where the<br />

most extreme <strong>change</strong>s have taken place <strong>in</strong> the four<br />

<strong>in</strong>dividual climate <strong>in</strong>dicators. Map 12 considers the<br />

four climate <strong>in</strong>dicators together, show<strong>in</strong>g the areas<br />

affected by the most cumulative <strong>change</strong> over the<br />

last 40 years. The hotspots identified <strong>in</strong> these two<br />

synthesis maps are of specific <strong>in</strong>terest for follow-up<br />

activities, <strong>in</strong>clud<strong>in</strong>g specific adaptation policies<br />

<strong>and</strong> programmes.<br />

Included on each of the maps are two additional<br />

layers show<strong>in</strong>g population trends <strong>and</strong> large-scale<br />

<strong>conflict</strong> occurrences dur<strong>in</strong>g the same time periods.<br />

The <strong>conflict</strong> layer highlights areas with higher<br />

<strong>in</strong>security <strong>and</strong> often more fragile governance<br />

structures. The population data is of <strong>in</strong>terest <strong>in</strong> order<br />

to underst<strong>and</strong> where populations are most at risk<br />

from climate-related factors.<br />

30<br />

CLIMATE INDICATORS<br />

Slow onset Sudden onset<br />

Sea level rise Temperature Ra<strong>in</strong>fall Drought Flood<br />

CHANGES<br />

Extreme Cumulative<br />

CLIMATE HOTSPOTS<br />

3.2 Changes <strong>in</strong> temperature<br />

Map 6 depicts the absolute <strong>change</strong>s <strong>in</strong> mean<br />

seasonal temperature <strong>in</strong> degrees Celsius (°C)<br />

between 1970 <strong>and</strong> 2006. The data is aggregated<br />

from weather stations located <strong>in</strong> the region with<br />

read<strong>in</strong>gs taken annually from May to October. This<br />

period <strong>in</strong>cludes the ra<strong>in</strong>y <strong>and</strong> cropp<strong>in</strong>g season<br />

months of July to September, as well as “buffer”<br />

months to capture natural variance. This period has<br />

been chosen because it is the most critical time<br />

period for agriculture-based livelihoods. Six colour<br />

categories represent seasonal temperature rang<strong>in</strong>g<br />

from a decrease <strong>in</strong> mean temperature of -0.5°C<br />

to an <strong>in</strong>crease of greater than 2.0°C.<br />

The data shows that there has been an overall rise <strong>in</strong><br />

mean seasonal temperature <strong>in</strong> CILSS countries from<br />

1970 to 2006 of approximately 1° C (see Figure 3).<br />

The only area to experience a decrease <strong>in</strong> seasonal<br />

temperature is <strong>in</strong> southern Mali near Bamako, <strong>and</strong><br />

small adjo<strong>in</strong><strong>in</strong>g parts of Burk<strong>in</strong>a Faso <strong>and</strong> Gu<strong>in</strong>ea.<br />

There have been very significant <strong>in</strong>creases (between<br />

1.5°C <strong>and</strong> 2°C) <strong>in</strong> the north of the region, <strong>in</strong>clud<strong>in</strong>g<br />

<strong>in</strong> far eastern Chad <strong>and</strong> the northern regions of<br />

Mali <strong>and</strong> Mauritania. Increases <strong>in</strong> temperature of<br />

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

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