Desertification in the Sahel:
climatic or human driven
causes?
Pierre OZER1 and André OZER2
1 Environment Science & Management Dpt., pozer@ulg.ac.be 2 Dpt. of Geography, aozer@ulg.ac.be
Archeological sites and lake deposits (8000 B.P.)
Introduction
Desertification is land degradation in arid, semi-arid
and dry sub-humid areas resulting from various
factors, including climatic variations and human
activities. (UNCCD)
Desertification is taking place due to population
pressure, socioeconomic and policy factors which
lead to overgrazing, deforestation and poor
agricultural practices. In addition, rainfall shortages
enhance degradation in the fragile drylands
Focus on the Sahel
150 mm
700 mm
Hyper-arid climate Arid &
semi-arid climate Dry subhumid
OZER et al., in press 250 350 450 550 650 750 1921 1931 1941 1951 1961 1971 1981 1991 2001 P lu v io m ét ri e a n n u el le ( m m ) . Pluviométrie annuelle Moyenne centrée [9 ans] Moyenne 1921-1967 Moyenne 1968-2004 Moyenne 1968-1987 Moyenne 1994-2004 Sahelian rainfall (1921 – 2004) Rainfall abrupt change in 1968 108 mm 1921-1968 1969-1987 1988-2004
Drought…
In 1963, the size of Lake Chad was about 23500 km
2.
After over 30 years of rainfall shortages (2000), its
area was reduced to 1355 km
2.
2000 1963
Drought… How large is the problem?
NIGER
Drought… How large is the problem?
300 mm
limit for agriculture (millet)
NIGER
Isohyets moved southwards by up to 200 km !
Drought…
Held et al., 2005
Held et al., 2005
Will it rain tomorrow ?
« Short-term » dramatic drought (early 1980s)
« Long-term » structural rainfall shortages (from ~~ 2050s ?)
Human activities
Who’s with me ???
Human population in the Sahel (1950 – 2005) and projections 0 60 120 180 240 1950 1960 1970 1980 1990 2000 2010 2020 2030 2040 2050 P o p u la ti o n ( m il li o n s) . 1950-2005 Low variant Medium variant High variant After UNPP, 2007 16 193 35 64
21
… agricultural overexploitation Maradi, Niger, ~500 mm
22
… overgrazing
Zinder area, Niger, ~400 mm
23
… overgrazing
Zinder area, Niger, ~400 mm
24
…forest resources reduction for … local use Zinder area, Niger, ~400 mm
25
Increasing population leads to…
…forest resources reduction to feed enlarging cities in fuelwood Zinder area, Niger, ~400 mm
26
Increasing population leads to…
…forest resources reduction to feed enlarging cities in fuelwood Zinder area, Niger, ~400 mm
27
Increasing population leads to…
…forest resources reduction to feed enlarging cities in fuelwood Zinder area, Niger, ~400 mm
0 50 100 150 200 250 300 350 400 450 500 1961 1966 1971 1976 1981 1986 1991 1996 2001 2006 YEARS T R E N D S ( 1 9 6 1 = 1 0 0 ) . POPULATION
CULTIVATED AREAS (MILLET) YIELDS (MILLET)
LIVESTOCK ROUNDWOOD
Human pressure trends in the Sahel (1961 – 2007) (1961 = 100)
DEFORESTATION
OVERGRAZING AGRICULTURAL
0 50 100 150 200 250 300 350 400 450 500 1961 1966 1971 1976 1981 1986 1991 1996 2001 2006 YEARS T R E N D S ( 1 9 6 1 = 1 0 0 ) . POPULATION
CULTIVATED AREAS (MILLET) YIELDS (MILLET)
LIVESTOCK ROUNDWOOD
Human pressure trends in the Sahel (1961 – 2007) (1961 = 100)
DEFORESTATION
OVERGRAZING AGRICULTURAL
PRESSURE
INCREASING GAP BETWEEN POPULATION INCREASE AND FOOD PRODUCTION !!!
30
Urban population trends in the Sahel (1961 – 2005) (1961 = 100) 0 500 1000 1500 2000 2500 3000 3500 1961 1966 1971 1976 1981 1986 1991 1996 2001 YEARS T R E N D S ( 1 9 6 1 = 1 0 0 ) . Mauritania Senegal SAHEL
Geomorphological
consequences
37
…sand movement threatening infrastructures… Gouré area, Niger, ~300 mm
38
…soil erosion witnessed by tree roots… Gouré area, Niger, ~300 mm
39
…sand movement threatening roads… Gouré area, Niger, ~300 mm
40
…sand movement impacting roads… Gouré area, Niger, ~300 mm
41
…totally degraded soils (sand sea)… Maine-Soroa area, Niger, ~400 mm
42
…sand dunes movement threatening oasis… Maine-Soroa area, Niger, ~400 mm
43
…sand dunes movement threatening oasis… Maine-Soroa area, Niger, ~400 mm
Dust storm distribution during the dry
season in the Sahel
« Humid » period 1951-1968
« Recent » period 1987-1997
Evolution of the number of days affected
by dust storms during the dry season
(Tombouctou, Mali, 1930-1997)
-10 10 30 50 70 90 110 1 9 3 0 1 9 3 3 1 9 3 6 1 9 3 9 1 9 4 2 1 9 4 5 1 9 4 8 1 9 5 1 1 9 5 4 1 9 5 7 1 9 6 0 1 9 6 3 1 9 6 6 1 9 6 9 1 9 7 2 1 9 7 5 1 9 7 8 1 9 8 1 1 9 8 4 1 9 8 7 1 9 9 0 1 9 9 3 1 9 9 6 J o u rs d e v is ib il it é < 5 0 0 d a mJours visi <500 dam
Moyenne lissée 5 ans
ERS 1/2 SAR (07/08.12.1995) – Interférométrie – Image de cohérence (Aleg – Mauritanie)
Evolution of the landscape in the
Makaortchi-Gayi region (S-E Niger)
Stable soils Moving dunes Vegetation Quartzite soils Delta Delta 0.2% 0.24% 0.56% 23% 14% 6% Moving dunes 8% 14% 36% Vegetation 1987 1975 1957-1958
52
So…
Desertification
in the Sahel in
the near future ?
Current rainfall Expected rainfall 0 60 120 180 240 P o p u la ti o n ( m il li o n s) . 1950-2005 Low variant Medium variant High variant Expected population Current population
53