A large shifting area of sub-Saharan Africa,
north of the savannas of southern Africa. The Sahel includes
parts of Senegal, Mauritania, Mali, Burkina Faso, Nigeria,
Niger, Chad, Sudan, Ethiopia, and Eritrea.
The Sahel region offers one of the world’s most tragic
examples of how poorly managed agricultural practices, when
mixed with long-term drought conditions, can lead to disaster
and permanent desertification. Sahel means boundary in Arabic,
and the Sahel forms the southern boundary of the world’s
largest desert, the Sahara. It is home to about 25 million people,
most of whom are nomadic herders and subsistence farmers.
In the summer months of June and July, heating normally
causes air to rise and this is replaced by moist air from the
Atlantic, which brings 14–23 inches (35.5–58.5 cm) of rain
per year. In the Sahel the normal northward movement of the
wet intertropical convergence zone stopped during an El-
NiƱo-Southern Oscillation (ENSO) event in 1968. Further climatic
changes in the 1970s led to only about half of the
normal rain falling until 1975. The additional lack of moisture
brought on complications from the temperature cycles of
the northern and southern oceans becoming out of synchronicity
at this time, and the region suffered long-term
drought and permanent desertification.
As the rains continued to fail to come, and the air masses
continued to evaporate surface water, the soil moisture was
drastically reduced, which further reduced evaporation and
cloud cover. The vegetation soon died off, the soils became dry
and hot, and near surface temperatures were further increased.
Soon the plants were gone, the soils were exposed to the wind,
and the region became plagued with blowing dust and sand.
Approximately 200,000 people died, and 12 million head of
livestock perished. Parts of the region were altered to desert,
with little chance of returning to the previous state.
The desertification of the Sahel was enhanced by the
agricultural practices of the people of the region. Nomadic
and marginal agriculture was strongly dependent on the monsoon,
and when the rains did not come for several years, the
natural and planted crops died and many of the remaining
plants were used as fuel for fires to offset the cost of fuel.
This practice greatly accelerated the desertification process.
The Sahara is now thought to be overtaking the Sahel by
migrating southward at approximately three miles per year
(4.8 km/yr). Much of Africa including the Sahel region has
become increasingly dry and desert-like over the past hundred
years or more, and any attempts to restart agriculture
and repopulate regions evacuated during previous famines in
this region may be fruitless and lead to further loss of life.
See also DESERT; SAHARA DESERT.
salt dome See DIAPIR.














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