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40% of Earth’s land surface. Precipitation in these regions
                     is meager, so drylands are prone to desertification. Deserti-
                     fication describes a form of land degradation in which more
                     than 10% of productivity is lost as a result of erosion, soil
                     compaction, forest removal, overgrazing, drought, salini-
                     zation, climate change, water depletion, and other factors.
                     Most such degradation results from wind and water erosion
                     (Figure 9.11). Severe desertification can expand existing
                     desert areas and create new ones (Figure 9.12). This process
                     has occurred most dramatically in areas of the Middle East
                     that have been inhabited, farmed, and grazed for long peri-
                     ods—including the Fertile Crescent region, where agricul-
                     ture first originated (p. 235).
                        By some estimates, desertification endangers the food
                     supply or well-being of more than 1 billion people in over
                     100 countries and costs tens of billions of dollars in income
                     each year. China alone loses $6.5 billion annually from deser-
                     tification. In its western reaches, desert areas are expanding
                     because of overgrazing from over 400 million goats, sheep,
                     and cattle. In the Sistan Basin along the border of Iran and
                     Afghanistan, an oasis that supported a million livestock
                     recently turned barren in just 5 years, and windblown sand   Figure 9.12  Severe desertification can cause desert areas
                     buried more than 100 villages. In Kenya, overgrazing and   to expand. Here, immense sand dunes moving in from the Gobi
                     deforestation fueled by rapid population growth has left 80%   Desert are burying farm fields in northwestern China.
                     of its land vulnerable to desertification. Everywhere, soil
                     degradation forces ranchers to crowd onto poorer land and
                     farmers to reduce the fallow periods during which land lies
                     unplanted and can regain nutrients. In a positive feedback   As a result of desertification, gigantic dust storms from
                     cycle (pp. 124–125), both of these actions worsen soil deg-  denuded land in China are now blowing across the Pacific
                     radation further.                                    Ocean to North  America, and dust storms from  Africa’s
                        Desertification is expected to grow worse as climate   Sahara Desert blow across the Atlantic Ocean to the Caribbean
                     change alters rainfall patterns, making some areas drier.   Sea (see Figure 17.11c, p. 475). Such massive dust storms
                     A 2007 United Nations report estimated that 50 million   occurred in the United States during the early 20th century,
                     people could soon be displaced. The report also suggested   when desertification shook American agriculture and society
                     that industrialized nations  fund reforestation projects  in   to their very roots.
                     drylands of the developing world to slow desertification
                     while gaining carbon credits in emissions trading pro-
                     grams (pp. 201–202, 530–531).                        The Dust Bowl shook the United States
                                                                          Prior  to  large-scale  cultivation  of  North  America’s  Great
                                                                          Plains, native prairie grasses of this temperate grassland
                                      Soil structure problems             region held soils in place. In the late 19th and early 20th cen-
                                            (3.4%)    Chemical            turies, many settlers arrived in Oklahoma,  Texas, Kansas,
                                                      problems            New Mexico, and Colorado hoping to make a living there as
                                                      (9.7%)              farmers. Between 1879 and 1929, cultivated area in the region
                                                                          soared from 5 million ha (12 million acres) to 40 million ha
                                                                          (100 million acres). Farmers grew abundant wheat and ranch-
                                                                          ers grazed many thousands of cattle, sometimes expanding
                                   Wind                                   onto unsuitable land and causing erosion by removing native
                                   erosion                                grasses and altering soil structure.
                                   (41.8%)
                                               Water                         In the early 1930s, a drought worsened the ongoing
                                               erosion                    human impacts, and the region’s strong winds began to erode
                                               (45.2%)                    millions of tons of topsoil (Figure 9.13). Massive dust storms
                                                                          traveled up to 2000 km (1250 mi), blackening rain and snow
                                                                          as far away as New York and Washington, D.C. Some areas
                                                                          lost as much as 10 cm (4 in.) of topsoil in a few years. The
                                                                          most-affected region in the southern Great Plains became
                     Figure 9.11  Soil degradation on drylands is due primarily to
                     erosion by wind and water. Data from U.N. Environment Programme.   known as the Dust Bowl, a term now also used for the histori-
                     2002. Tackling land degradation and desertification. Washington and Rome:   cal event itself. The “black blizzards” of the Dust Bowl forced
             242     Global Environment Facility and International Fund for Agricultural Development.  thousands of farmers off their land.







           M09_WITH7428_05_SE_C09.indd   242                                                                                    12/12/14   2:59 PM
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