1998
DOI: 10.1002/(sici)1099-145x(199809/10)9:5<375::aid-ldr304>3.0.co;2-2
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Desertification and drylands development: what can be done?

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Cited by 43 publications
(19 citation statements)
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“…But their main targets were images that UNEP added to 'polish' the boundary object to improve its salience to governments, e.g. unidirectional and irreversible frontier expansion of desert fringes (Mainguet and Da Silva, 1998), and overestimates of the extent of the problem (Thomas and Middleton, 1994). They could be forgiven for confusing the two, since UNEP's elaborations contradicted the views of its experts and UNCOD.…”
Section: Methodsmentioning
confidence: 99%
“…But their main targets were images that UNEP added to 'polish' the boundary object to improve its salience to governments, e.g. unidirectional and irreversible frontier expansion of desert fringes (Mainguet and Da Silva, 1998), and overestimates of the extent of the problem (Thomas and Middleton, 1994). They could be forgiven for confusing the two, since UNEP's elaborations contradicted the views of its experts and UNCOD.…”
Section: Methodsmentioning
confidence: 99%
“…This earlier emphasis on 'desert-like conditions' has since shifted towards a more specific descriptor in which desertification is now considered to be "land degradation in arid, semi-arid and dry sub-humid areas resulting from various factors including climatic variations and human activities" (UNCCD, 1994: Article 1). Expansion of desert fringes constitutes only a small part of desertification (Glenn et al, 1998) and the perception of desertification as a process of desert enlargement has now been rejected (Mainguet and Da Silva, 1998).…”
Section: Introductionmentioning
confidence: 99%
“…However, the degradation processes associated with desertification affect several subsystems as well as their interactions at multiple spatial and temporal scales. For instance, adverse effects on soil quality involve depletion of soil fertility, but also reduce soil-water storage (Mainguet and Da Silva, 1998), which, in turn, can constrain seed germination and vegetation reestablishment, modify climax vegetation, disrupt biogeochemical cycles, alter water and energy balances, and conse-quently lead to a loss of ecosystem resilience (Lal, 2001). This cascade of disturbances may result in a reduction of the C sequestration capacity of a given ecosystem, which is clearly a symptom of the loss of biological productivity, resulting in a positive feedback to global warming.…”
mentioning
confidence: 99%