Livelihood Security: Climate change, conflict and migration in - UNEP
Livelihood Security: Climate change, conflict and migration in - UNEP
Livelihood Security: Climate change, conflict and migration in - UNEP
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ated to <strong>in</strong>crease process<strong>in</strong>g time. Build<strong>in</strong>g on a critical VHI threshold (VHI values < 35 <strong>in</strong>dicate<br />
severe drought conditions), the datasets were reclassified <strong>in</strong> a subsequent step. Based on these<br />
reclassified layers (0: VHI > 35; 1: VHI < 35), f<strong>in</strong>ally, the number of drought affected seasons<br />
was calculated for each cell (16 x 16 km) for the period 1985 to 2009.<br />
DFO - FLOOD DATA<br />
As the data is provided <strong>in</strong> Map<strong>in</strong>fo Inter<strong>change</strong> Format on the DFO website, the first step was<br />
to convert the data to a common vector format. In a next step a subset of the data was<br />
created, show<strong>in</strong>g the major flood events <strong>in</strong> the region of <strong>in</strong>terest as polygons. F<strong>in</strong>ally, a net<br />
of artificial cells was created <strong>in</strong> order to calculate the number of flood events per cell for the<br />
years 1985 to 2009.<br />
CSI-CGIAR – SRTM v4 ELEVATION DATA<br />
As the SRTM v4 global digital elevation model (GDEM) is provided <strong>in</strong> 5 degree resolution tiles,<br />
the first step – after download<strong>in</strong>g the tiles - was to mosaic the tiles cover<strong>in</strong>g the target region.<br />
APD & GPWv3 - POPULATION DATA<br />
Population count data was acquired from different sources. Data from 1960 to 2000 was<br />
acquired from the <strong>UNEP</strong> African Population Database (APD) website, while data from 1990 to<br />
2010 was downloaded from the Gridded Population of the World (Version 3) portal. To determ<strong>in</strong>e<br />
if the GPWv3 data could be utilized to update the available time-series of population<br />
data as provided by <strong>UNEP</strong>-APD, Pearson’s correlation of both datasets (<strong>UNEP</strong>-APD <strong>and</strong> GPWv3)<br />
was calculated for three larger test areas. Follow<strong>in</strong>g this approach the overall population trend<br />
was calculated for two periods: 1) 1970-2010 <strong>and</strong> 2) 1980-2010.<br />
PRIO-CSCW – CONFLICT SITE DATA<br />
After the dataset was downloaded from the PRIO-CSCW website, a subset of the data for the<br />
region of <strong>in</strong>terest was created. Then, based on the given centre-po<strong>in</strong>t coord<strong>in</strong>ates <strong>and</strong> the<br />
radius variable, the estimated spatial extent of the <strong>conflict</strong>s <strong>in</strong> the target area were calculated.<br />
In order to have additional <strong>in</strong>formation on the number of <strong>conflict</strong>s a dissect (number of overlaps)<br />
was calculated based on the subset.<br />
Cartographic representation<br />
Follow<strong>in</strong>g analysis of the data, the result<strong>in</strong>g geospatial <strong>in</strong>formation layers were cartographically<br />
ref<strong>in</strong>ed <strong>in</strong> order to obta<strong>in</strong> a more <strong>in</strong>tuitive <strong>and</strong> appeal<strong>in</strong>g characterization of the results,<br />
mak<strong>in</strong>g both <strong>in</strong>terpretation <strong>and</strong> communication easier. Depend<strong>in</strong>g on the quality <strong>and</strong> format<br />
of the dataset different approaches were applied:<br />
•<br />
•<br />
•<br />
Angular polygon layers were smoothed mak<strong>in</strong>g use of Bezier <strong>in</strong>terpolation techniques.<br />
Coarse grids, such as the temperature or precipitation trend dataset (0.5 degree resolution),<br />
were converted to po<strong>in</strong>t layers <strong>in</strong> order to apply spatial <strong>in</strong>terpolation techniques (ord<strong>in</strong>ary<br />
krig<strong>in</strong>g) to create a cont<strong>in</strong>uous surface of f<strong>in</strong>er resolution (i.e. 0.1 degree resolution). Where<br />
necessary, a low-pass filter was utilized to further smooth the entire raster. In a next step the<br />
ref<strong>in</strong>ed grids were re-converted to polygons. F<strong>in</strong>ally, the polygons were smoothed mak<strong>in</strong>g<br />
use of Bezier <strong>in</strong>terpolation techniques.<br />
F<strong>in</strong>ally, where necessary, representation tools were utilized to enhance the visual<br />
representation of the result<strong>in</strong>g geospatial <strong>in</strong>formation layers.<br />
<strong>Livelihood</strong> <strong>Security</strong>: <strong>Climate</strong> Change, Migration <strong>and</strong> Conflict <strong>in</strong> the Sahel<br />
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