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The Economics of Desertification, Land Degradation, and Drought

The Economics of Desertification, Land Degradation, and Drought

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was started in reaction to the GLASOD approach, in order to develop “a set tools to document,<br />

monitor, <strong>and</strong> evaluate” soil <strong>and</strong> water conservation (SWC) “know-how, to disseminate it around the<br />

globe, <strong>and</strong> to facilitate the exchange <strong>of</strong> experience” (Schwilch, Liniger, <strong>and</strong> Van Lynden 2004: 1). It<br />

was aimed at facilitating local <strong>and</strong> international exchange <strong>of</strong> knowledge by establishing the WOCAT<br />

network. A global map <strong>of</strong> SWC measures is still under construction. WOCAT also collected data on<br />

the costs <strong>of</strong> l<strong>and</strong> management practices, which could allow a determination <strong>of</strong> the costs <strong>of</strong> taking<br />

action to prevent or mitigate l<strong>and</strong> degradation. WOCAT conducted 42 case studies in 23 countries<br />

from six continents. However, the choice <strong>of</strong> the case study countries was not done in such a way that<br />

could allow extrapolation <strong>of</strong> the results to the rest <strong>of</strong> the world.<br />

Global <strong>Desertification</strong> Tension Zones<br />

<strong>The</strong> U.S. Department <strong>of</strong> Agriculture’s Natural Resources Conservation Service (NRCS) developed<br />

global maps on global desertification tension zones, which depict areas vulnerable to desertification,<br />

wind <strong>and</strong> water erosion by natural preconditions, <strong>and</strong> human impact (Eswaran, Lal, <strong>and</strong> Reich 2001).<br />

<strong>Desertification</strong> tension zones were described with two systems: zones under low-input agricultural<br />

systems, where the “productive capacity <strong>of</strong> the l<strong>and</strong> is stressed by mismanagement, generally by<br />

resource poor farmers,” <strong>and</strong> high-input agricultural systems, where tension zones “arise due to<br />

excessive use <strong>of</strong> agrochemicals, uncontrolled use <strong>of</strong> irrigation, <strong>and</strong> monoclonal plantations with<br />

minimal genetic diversity” (Eswaran, Reich, <strong>and</strong> Beinroth 1998: 1). Four degrees <strong>of</strong> severity (low,<br />

moderate, high, <strong>and</strong> very high), reminiscent to the GLASOD approach, show the degree <strong>of</strong> an area’s<br />

vulnerability to desertification or l<strong>and</strong> degradation (Figure 2.2). According to the definition <strong>of</strong><br />

desertification from UNEP, only arid, semiarid, <strong>and</strong> subhumid areas were integrated in this approach,<br />

excluding subhumid <strong>and</strong> humid, except for water erosion, which also affects humid areas.<br />

Figure 2.2—<strong>Desertification</strong> vulnerability<br />

Source: USDA-NRCS 1998.<br />

<strong>The</strong> purpose <strong>of</strong> the NRCS study was to identify <strong>and</strong> locate “desertification tension zones […]<br />

where the potential decline in l<strong>and</strong> quality is so severe as to trigger a whole range <strong>of</strong> negative<br />

socioeconomic conditions that could threaten political stability, sustainability, <strong>and</strong> the general quality<br />

<strong>of</strong> life” (Eswaran, Reich, <strong>and</strong> Beinroth 1998: 1). <strong>The</strong> approach <strong>of</strong> NRCS used several data input, such<br />

as the FAO/UNESCO Soil Map <strong>of</strong> the World (1:5,000,000) <strong>and</strong> a pedoclimate map that was compiled<br />

by a climate database from records for about 25,000 stations globally, using soil moisture <strong>and</strong><br />

temperature regimes that were superimposed on the soil map via GIS. <strong>The</strong> map <strong>of</strong> vulnerability to<br />

desertification was superimposed with an interpolated population density map from the Center for<br />

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