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Grasslands of the World.pdf - Disasters and Conflicts - UNEP

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The changing face <strong>of</strong> pastoral systems in grass-dominated ecosystems <strong>of</strong> eastern Africa 55<br />

(2) ei<strong>the</strong>r long-term experiments or observational studies at <strong>the</strong> pasture scale<br />

that assess <strong>the</strong> relative impacts <strong>of</strong> drought, livestock <strong>and</strong> o<strong>the</strong>r agents on ecosystem<br />

dynamics . Most <strong>of</strong> <strong>the</strong> research on l<strong>and</strong> degradation <strong>and</strong> desertification<br />

in Africa has been focused on <strong>the</strong> Sahel , which has been intensively studied<br />

since <strong>the</strong> first droughts in <strong>the</strong> 1970s. Some l<strong>and</strong>scape-scale studies based on<br />

a combination <strong>of</strong> fine-resolution satellite data <strong>and</strong> field measurements have<br />

been carried out in different parts <strong>of</strong> Africa <strong>and</strong> demonstrated <strong>the</strong> existence<br />

<strong>of</strong> local-scale degradation <strong>of</strong> rangel<strong>and</strong>s in Ferlo, Senegal (Diouf <strong>and</strong> Lambin,<br />

2001) <strong>and</strong> Turkana, Kenya, where highly affected areas covered only 5 percent<br />

<strong>of</strong> <strong>the</strong> l<strong>and</strong> surface (Reid <strong>and</strong> Ellis, 1995). The importance <strong>of</strong> studying l<strong>and</strong><br />

degradation <strong>and</strong> desertification problems over a sufficiently long period is<br />

illustrated by studies conducted in Burkina Faso by Lindqvist <strong>and</strong> Tengberg<br />

(1993) <strong>and</strong> later by Rasmussen, Fog <strong>and</strong> Madsen (2001). The first group <strong>of</strong><br />

scientists studied <strong>the</strong> amount <strong>of</strong> woody vegetation cover in three sites in<br />

nor<strong>the</strong>rn Burkina Faso (1955–89). They found that important loss in woody<br />

vegetation cover occurred during <strong>the</strong> first <strong>of</strong> a series <strong>of</strong> droughts that started<br />

in <strong>the</strong> late 1960s, when large areas <strong>of</strong> bare soil developed. The authors found<br />

little evidence <strong>of</strong> vegetation recovery until 1989, despite increasing rainfall since<br />

1985. Rasmussen, Fog <strong>and</strong> Madsen (2001) revisited <strong>the</strong> area, adding 10 years <strong>of</strong><br />

satellite data. They found a decrease in albedo <strong>and</strong> thus increase in vegetation<br />

cover over <strong>the</strong> period 1986–1996, which was confirmed by fieldwork, thus<br />

showing <strong>the</strong> recovery <strong>of</strong> vegetation after drought. Interviews with local people<br />

indicated that <strong>the</strong> species composition <strong>of</strong> <strong>the</strong> regenerating herbaceous vegetation<br />

has changed considerably since <strong>the</strong> late 1970s. L<strong>and</strong> degradation caused by<br />

heavy grazing pressure was mostly found in <strong>the</strong> proximity <strong>of</strong> important water<br />

resources , which probably cover only a small proportion <strong>of</strong> <strong>the</strong> l<strong>and</strong>scape in<br />

total. Schlesinger <strong>and</strong> Gramenopoulos (1996) also used <strong>the</strong> amount <strong>of</strong> woody<br />

vegetation cover as an indicator <strong>of</strong> desertification in western Sudan, but studied<br />

sites that were devoid <strong>of</strong> human use over <strong>the</strong> period 1943–1994. They analysed<br />

a time series <strong>of</strong> aerial photographs <strong>and</strong> Corona satellite images <strong>and</strong> did not find<br />

a significant decline in woody vegetation for <strong>the</strong> study period, despite several<br />

droughts having occurred during that period. Thus, at least in this area, <strong>the</strong>y<br />

showed that <strong>the</strong> Sahara is not exp<strong>and</strong>ing <strong>and</strong> that drought had little effect on<br />

woody vegetation. In ano<strong>the</strong>r part <strong>of</strong> <strong>the</strong> Sudan, <strong>the</strong> concentration <strong>of</strong> livestock<br />

around water points <strong>and</strong> settlements led to local loss <strong>of</strong> vegetative cover <strong>and</strong><br />

accelerated erosion (Ayoub, 1998). In contrast, o<strong>the</strong>rs have found that heavy<br />

livestock grazing around pastoral settlements in arid areas had minor impacts<br />

on woody vegetation <strong>and</strong> biodiversity , with impacts confined within <strong>the</strong> settlements<br />

<strong>the</strong>mselves (Sullivan, 1999). Woody vegetation can replace palatable<br />

grass species in heavily grazed areas, caused by grazing pressure ra<strong>the</strong>r than<br />

climate (Skarpe, 1990; Perkins, 1991).<br />

At <strong>the</strong> pasture or field level, <strong>the</strong> picture is more complex. Generally, livestock<br />

grazing , browsing <strong>and</strong> trampling causes loss <strong>of</strong> vegetation , competition

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