Changing climate
Africa and Sub-Saharan Africa in particular
are highly vulnerable to climate change. As a consequence of greenhouse gas
emissions, our planet is heating up (Carter, R.C. and Parker, A). According to
the The Intergovernmental Panel on Climate Change (IPCC) in 2007 humans`
influence on climate change can no longer be denied. Figure 1 shows the temporal growth of rising air temperature in the years
since 1870. As you can see the global air temperature has risen up to 0.75°C in
2015. Rising temperatures mean that areas will get drier, droughts will
increase and more extreme weather will occur. Also the hydrological cycle is
linked to certain aspects of climate change within temperature and radiation balance. (Batels et al., 2008).
Figure 1: Global air temperature (http://www.cru.uea.ac.uk/).
No rain, no crops
Africa is highly dependent upon the
agricultural sector. The value added in the GDP is very high, as in Chad where
52,39% of the GDP was generated by the agricultural sector (The
World Bank). Cash crops are essential parts of the African economy. But to
grow the crops a huge amount of water is needed. Most of the Sub-Saharan
countries suffer with little rainfall. Farmers are using irrigation systems,
dependent on groundwater to grow their crops. The demand for freshwater is
rising. As the rainfall is characterised for high variability, the population
relies on shallow or deep groundwater. R. Carter and C. Bevan estimated the
number affected by one billion people. These reservoirs need to be recharged by
the annual rainfall to ensure water supply.
Table 1: Rate of mean annual rainfall and
rainfall range in Sub-Saharan countries (Source: ARTES) By Carter, R.C. and
Parker, A., (2009).
Table 1 highlights the mean annual
rainfalls in certain countries of Sub-Saharan Africa in context with the
rainfall range. The deviation between the mean annual rainfall and the range is
enormous. Countries like Niger have got 45% less rainfall than the mean
rainfall should be. Any changes in the annual rainfall either temporal or
spatial distribution, are expected to influence the water balance (Carter, R.C.
and Parker, A., 2009.). This of course has a huge on impact on African farmers,
which are dependent on the agricultural sector. As I said before the rainfall
in Africa is characterised by high variability between years, but trough,
climate change, the variation of rainfall will be more extreme than is it now. Carter,
R.C. and Parker, A. believe “the question of the likely impact of climate
change on renewable groundwater resources is highly relevant, but under-researched”.
References:
Carter,
R. C. & Bevan, J. E. (2008) Groundwater development for poverty alleviation
in sub-Saharan Africa. In: Applied Groundwater Studies in Africa (ed. by S.
Adelana & A. M. MacDonald), 25–42. IAH Selected Papers on Hydrogeology no.
13, CRC Press, Taylor & Francis, UK.
Carter, R.C. and Parker, A., 2009.
Climate change, population trends and groundwater in Africa. Groundwater
and climate in Africa: a review. Hydrological Sciences JournalVol.
54(4), pp. 676-689.
This second post engages well with some of the literature on climate change and water in Africa. One question that springs to mind is this: is climate change in the next couple of decades expected to deliver changes that are outside of the extreme variability in hydrological conditions that is already experienced in Africa? Might it be argued that adaptation to existing hydrological variability would go a long way to adapting to projected climate change impacts? How do these impacts weigh up against demographic pressures on water resources including population growth, urbanisation, and the push towards irrigated agriculture?
ReplyDeleteThere are many changes associated with climate change. For my, hydrological variability is an obvious issue that leads us to feel the changes. Of course there are much more impacts, such as demographic pressure, urbanisation or agriculture. I recommend my post about “Water scarcity in addition to a growing population” to link the hydrological variability to further changes.
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