Sahel
From Wikipedia, the free encyclopedia
- See also Sahel, Tunisia, a region of eastern Tunisia.
The Sahel (from Arabic ساحل, sahil, shore, border or coast of the Sahara desert) is the boundary zone in Africa between the Sahara to the north and the more fertile region to the south, known as the Sudan (not to be confused with the country of the same name).
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[edit] Geography
The Sahel is primarily savanna and runs from the Atlantic Ocean to the Horn of Africa, changing from semi-arid grasslands to thorn savanna. Over the history of Africa the region has been home to some of the most advanced kingdoms benefiting from trade across the desert. Collectively these states are known as the Sahelian kingdoms.
The countries of the Sahel today include Senegal, Mauritania, Mali, Burkina Faso, Niger, Nigeria, Chad, Sudan, and Eritrea.
A map of the region can be viewed here.
[edit] Environment
About 12,500 years ago, the Sahel was a part of the Saharan desert, and was covered in sand dunes which have shaped the landscape that we see today. The Sahel receives 150–500 mm (6–20 in) of rainfall a year, primarily in the monsoon season. The rainfall is characterized by great variation from year to year and from decade to decade. The most important limitations to land productivity in the Sahel are water and soil fertility. Soils in the Sahel are mostly acidic (which results in aluminum toxicity to plants), and are very low in nitrogen and phosphate.
There is a strong correlation between rainfall in the Sahel region and intense hurricane activity in the Atlantic[1].
[edit] Transhumance
Traditionally, most of the people in the Sahel have been semi-nomads, farming and raising cattle in a system of transhumance, which is probably the most sustainable way of utilizing the Sahel. The difference between the dry north with higher levels of soil-nutrients and the wetter south is utilized so that the herds graze on high quality feed in the North during the wet season, and trek several hundred kilometers down to the south, to graze on more abundant, but less nutritious feed during the dry period. Increased permanent settlement and pastoralism in fertile areas has been the source of conflicts with traditional nomadic herders.
[edit] Droughts
- Further information: Sahel drought
There was a major drought in the Sahel in 1914, caused by annual rains far below average, that caused a large-scale famine. The 1960's saw a large increase in rainfall in the region, making the Northern drier region more accessible. There was a push, supported by governments, for people to move northwards, and as the long drought-period from 1968 through 1974 kicked in, the grazing quickly became unsustainable, and large-scale denuding of the terrain followed. Like the drought in 1914, this led to a large-scale famine, but this time it was somewhat tempered by international visibility and an outpouring of aid. This catastrophe led to the founding of the International Fund for Agricultural Development. Furthermore, there is now compelling evidence that shows the drought that lasted from the late sixities and into the mid to late 80's is due to a phenomena called Global Dimming.
[edit] External links and references
- ^ Landsea, C., and Gray, n. The Strong Association between Western Sahel Monsoon Rainfall and Intense Atlantic Hurricanes. Journal Of Climate, Vol. 5, No. 5, May 1992.
- Notes on Sahel Africa
- CILSS
- Institut du Sahel
- Batterbury, S.P.J. 1998. Shifting Sands. The Geographical May: 40–45.
- Batterbury, S.P.J. & A. Warren. 2001. The African Sahel 25 years after the great drought: assessing progress and moving towards new agendas and approaches. Global Environmental Change 11(1): 1–96.
- Sahel rainfall index, 1898–2002
- Desertification — a threat to the Sahel
- Climate research summary - Sahel drought: past problems, an uncertain future Text, graphics and animations from NOAA / Geophysical Fluid Dynamics Laboratory
[edit] See also
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