An image showing a barren, dry landscape with cracks on the ground, indicative of desertification in AfricaSemi-arid Niger is at risk for further desertification.
Desertification in Africa is a form of land degradation that involves the conversion of productive land into desert or arid areas. This issue is a pressing environmental concern that poses a significant threat to the livelihoods of millions of people in Africa who depend on the land for subsistence.[1][2] Geographical and environmental studies have recently coined the term desertification. Desertification is the process by which a piece of land becomes a desert, as the word desert implies.[3] The loss or destruction of the biological potential of the land is referred to as desertification.[4] It reduces or eliminates the potential for plant and animal production on the land and is a component of the widespread ecosystem degradation. Additionally, the term desertification is specifically used to describe the deterioration of the world's drylands, or its arid, semi-arid, and sub-humid climates. These regions may be far from the so-called natural or climatic deserts, but they still experience irregular water stress due to their low and variable rainfall. They are especially susceptible to damage from excessive human land use pressure.[3] The causes of desertification are a combination of natural and human factors, with climate changeexacerbating the problem. Despite this, there is a common misconception that desertification in Africa is solely the result of natural causes like climate change and soil erosion. In reality, human activities like deforestation, overgrazing, and unsustainable agricultural practices contribute significantly to the issue. Another misconception is that, desertification is irreversible, and that degraded land will forever remain barren wastelands. However, it is possible to restore degraded land through sustainable land management practices like reforestation and soil conservation.[5] A 10.3 million km2 area, or 34.2% of the continent's surface, is at risk of desertification. If the deserts (Sahara and Kalahari) are taken into account, the affected and potentially affected area is roughly 16.5 million km2 or 54.6% of all of Africa. 5.7 percent of the continent's surface is made up of very severe regions, 16.2 percent by severe regions, and 12.3 percent by moderate to mild regions.[3]
According to three criteria: climate, inherent vulnerability, and human and animal pressure, the United Nations recognizes four degrees of desertification hazards: very severe, severe, moderate, and slight.[6][4] When land becomes completely unusable, it is said to have experienced very severe desertification. Examples of this include moving dunes, extensive large gully systems, and salt-crusted, nearly impervious soils in previously irrigated areas. These circumstances are thought to be economically irreversible.[3] Severe desertification and moderate desertification are classified according to the extent of accelerated soil erosion and denudation, the change to less desirable vegetation, or the loss of crop yield due to reversible salinization or irrigated soils. Where there has been little to no degradation of the plant cover or soil, it is represented by the second category, slight desertification.[3]
History
The term desertification is most often associated with French botanist André Aubréville's 1949 work on African rainforests, although research claims that it may be traced back to 19th-century French colonial North Africa.[7] The Comité d'Etudes[fr] commissioned research to investigate the prehistoric growth of the Sahara Desert, which was caused by natural occurrences at the time.[8] The phenomenon has been around for thousands of years in Africa and is not new. However, as populations have grown and human activity has increased, desertification has exacerbated significantly in recent decades.
Desertification can be traced back thousands of years in Africa, with evidence discovered in ancient literature and archaeological documents. However, the magnitude and severity of the problem have grown in recent decades as a result of a mix of natural and human factors.[9] Desertification became an increasingly severe issue in Africa over the twentieth century, causing widespread environmental deterioration and jeopardizing the livelihoods of millions of people who rely on the land for food.[10] In response, governments, non-governmental groups, and international organizations have devised a variety of solutions, including reforestation, soil conservation, and sustainable land management methods.[11]
Over the past century, the Sahara desert has been expanding by more than 7,600 sq km a year and is now 10% larger than it was in 1920.[12] Desertification and desert growth were not first caused primarily by human-induced climate change, as they are now. The world's greatest deserts were generated by natural processes that interacted over time, such as water evaporation, rising winds, warm airfall, and low humidity. Human activity, on the other hand, has recently come to either expand or contract these deserts. To put Africa's contributions into context, the Sahara has been quickly expanding since the 1920s, spanning 10% more territory than it did previously, according to a study conducted by National Science Foundation (NSF) funded scientists at the University of Maryland (UMD).[13] The drought of the 1980s was not the first man-made disaster to hit the Sahel region. The desert has been subjected to a lengthy succession of droughts, the most notable of which was the Sahelian drought and famine of 1968. It continued until 1985 and was directly responsible for approximately 100,000 deaths and the disturbance of millions of lives.[14] Human resource exploitation (such as overgrazing and deforestation) was first thought to be the sole cause of the drought. Nonetheless, large-scale climate changes may have contributed to the drought. Despite being the most severely impacted region in Africa, the Sahel is not the only one afflicted by desertification. The Karoo in South Africa, has experienced semi-arid conditions for the last 500 years, Somalia, which has experienced three major drought crises in the last decade alone, and Ethiopia, which has seen 75% of its land affected by desertification and a major famine between 1983 and 1985.[15][16]
Causes
According to some academics, human causes only play a very minor supportive role in the processes of desertification, with climate being the main cause. Other researchers reverse the significance of these two factors.[17] Desertification in Africa is caused by both natural and man-made forces. Climate change, which has resulted in increased aridity and decreasing rainfall in many regions, and soil erosion, which happens naturally but can be exacerbated by human activity, are the principal natural elements that lead to desertification.[18] For instance, it might be difficult to tell if desertification or desert expansion is the result of climate change or human activity.[19] Desertification in Africa is exacerbated by human factors such as deforestation, overgrazing, and unsustainable farming methods such as monoculture and excessive use of chemical fertilizers. For example, deforestation reduces the quantity of plants that may anchor soil and protect it from erosion, whereas overgrazing depletes vegetation and exposes soil to erosion and degradation.[20] For instance, it has been argued that the Sahara's edges are primarily the result of human activity, with climate playing merely a supporting role. A third group assigns almost equal blame to man and the environment.[21][22] Poor land management techniques, such as crop rotation, the use of heavy machinery that compacts soil, and unsustainable water management methods, all contribute to desertification. Mining and oil exploration can also contribute to desertification by disturbing natural ecosystems and reducing soil quality.[23] Population expansion and poverty can exacerbate the situation by increasing resource demand and resulting in unsustainable land use practices. All of these causes have contributed to the degradation of fertile soil, posing a serious threat to the livelihoods of millions of Africans who rely on the land for subsistence.
In the Sahel, desertification is mostly attributed to wind erosion.[24] To put it simply, wind erosion is the phenomenon when a strong wind removes a field's topsoil. Wind erosion depletes the nutrients in the soil because the topsoil often contains more nutrients than the subsoil.[25][26][27] This lowers the production of the soil. Furthermore, the loss of topsoil can expose the subsurface with inferior physical qualities, which lowers the permeability of the soil. Furthermore, wind erosion can hinder crop growth by burying crops beneath blown sand and causing physical harm (abrasion).[28][25]
Affected areas
Three different regions of the continent are affected by desertification: Mediterranean Africa, the Sudano-Sahelian region, and Africa south of the Sudano-Sahelian.[3][29] Severe and very severe areas are to be found in the five Mediterranean countries of Africa: Egypt, Algeria, Libya, Morocco, and Tunisia. The Gasfa Peninsula in Tunisia is a prime example of a region in the Mediterranean that has undergone very severe or irreversible conditions of desertification.[30] Most of the 19 countries in the Sudano-Sahelian region experience similar conditions (severe to very severe), whereas most of Africa south of the Sudano-Sahelian experiences mild to severe risks associated with desertification. About 36 African nations are affected by drought and desertification collectively.[3] The Sahel region, which includes Senegal, Mauritania, Mali, Niger, Chad, Sudan, and Eritrea, has been plagued by frequent droughts, overgrazing, and deforestation, resulting in soil deterioration and desertification.[31] In a restricted sense, the term Sahel region refers to an area that spans around 400 km from north to south and approximately 4000 km from east to west along the southern ridges of the Sahara Desert and experiences 200 to 600 mm of annual rainfall on average.[25] In this location, the little quantity of rainfall mixed with the less productive and highly sandy soil (explained in detail below) is generating chronic food shortages, and a catastrophic famine can be precipitated when the region is afflicted by drought.[25] In 1974, at least 750,000 people in Mali, Niger, and Mauritania had to rely solely on food aid to survive, and during the drought that lasted from 1972 to 1984, at least 100,000 people died. According to the United Nations Department of Economic and Social Affairs World Population Prospects, the six Sahel countries had a population of about 30 million people at that time.[32][25] Long-term droughts and exploitation of natural resources have plagued the Horn of Africa which comprises Somalia, Ethiopia, and Kenya. Land degradation has occurred in Southern Africa, including Zimbabwe, Botswana, Namibia, and South Africa, as a result of unsustainable farming techniques, overgrazing, and deforestation. Desertification has also affected North Africa, which includes Egypt, Libya, Algeria, Tunisia, and Morocco, as a result of climate change, overgrazing, and unsustainable agricultural practices. Food and water shortages, population displacement, and biodiversity loss are all repercussions of desertification in these places, underscoring the critical need for sustainable land use practices and environmental conservation initiatives throughout Africa.[33]
Agriculture
Desertification affects roughly 45% of Africa's land area, with 55% at high or extremely high risk of future degradation. Climate change and desertification have a significant impact on food security through their effects on agricultural productivity.[34] Substantial data is pointing to the negative effects of climate change and desertification not just on crop yields, but also on agricultural productivity and income losses in dry lands. Forecasts for Sub-Saharan Africa indicate that rising temperatures, an increase in the number of heat waves, and increased aridity will have an impact on rain-fed agricultural systems. Climate change would reduce mean yields for 11 main world crops - millet, eld pea, sugar beet, sweet potato, wheat, rice, maize, soybean, groundnut, sunflower, and rapeseed - by 15% in Sub-Saharan Africa and 11% in the Middle East and North Africa by 2050 if carbon fertilization is not used.[35] Desertification has reduced agricultural output and incomes while also contributing to biodiversity loss in many dryland regions. It is also expected to lower crop and livestock output, change the makeup of plant species, and reduce biological diversity throughout dry lands. Crop production in Sub-Saharan Africa, in particular, may be reduced by 17-22% by 2050 as a result of climate change. In 2017, around 821 million people worldwide were food insecure, with Africa accounting for 31%.[36] Sub-Saharan Africa, notably East Africa, had the world's greatest proportion of undernourished people in 2017, with 28.8% and 31.4%, respectively. Long-term monitoring in North Africa (1978-2014) revealed the disappearance of significant perennial plant species owing to drought and desertification, such as Stipa tenacissima and Artemisia herba alba.[36]
In the northern part of the sahel, where rainfall is scarce, livestock farming based on nomadic grazing is practiced; in the southern part of the country, where rainfall is more than the cultivation limit (annual precipitation of approximately 300 mm), drought-resistant crops like pearl millet (Pennisetum glaucum (L.) R. Br.), sorghum (Sorghum bicolor (L.) Moench), cowpeas (Vigna unguiculata (L.) Walp), and peanuts (Arachis hypogaea L.) are grown without irrigation.[25] Nevertheless, because of its proximity to the cultivation limit, the wide variations in annual rainfall, and the occurrence of dry spells, it is challenging to maintain a consistent yield. Along permanent rivers like the Niger River, rice is also grown. Another characteristic of agriculture in the Sahel region is the mix of crop farming and livestock farming. A symbiotic system is formed here. After pearl millet or sorghum has been harvested by the crop farmers, the livestock farmers graze their livestock (cows, sheep and goats) in the field and manure is returned to the land.[25] The primary technique for preserving soil fertility is the incorporation of domestic waste into fields that are closer to the village or settlement (less than 1 km). Fields that are farther away from the village or settlement are primarily left fallow, while fields that are closer to the settlement are primarily used for night corralling, a system in which livestock are housed in a field overnight, supplying the field with manure and urine.[37][38]
Economic impact
Great green wall map
Desertification has substantial economic consequences in Africa, particularly in places where agriculture and natural resource utilization are the predominant sources of revenue. Desertification reduces crop yields, causes food shortages, and increases poverty in impacted populations by destroying fertile land and water supplies. People displaced as a result of desertification can lead to increased competition for scarce resources and conflicts, worsening economic issues.[39] Desertification's detrimental effects on ecosystems and biodiversity can have far-reaching consequences for industries like tourism and ecotourism, which rely on healthy ecosystems to attract tourists. Desertification has enormous economic ramifications in Africa, necessitating persistent efforts to minimize the effects of desertification through sustainable land use practices, conservation, and restoration of degraded lands.[40]
Combating desertification
With the Sahel region being the most vulnerable and extensively affected by desertification, a project known as the Great Green Wall was launched in 2007 for the Sahara and Sahel. Its lofty goal is to create an 8,000-kilometer natural wonder over Africa's whole width in order to enhance the quantity of fertile land bordering the Sahara desert. The premise is that, planting more trees will help to prevent desertification, create jobs, improve food security, and return displaced Africans home.[41]
Burkina Faso is a landlocked Sahel country that shares borders with six nations. It lies between the Sahara desert and the Gulf of Guinea, south of the loop of the Niger River, mostly between latitudes 9° and 15°N, and longitudes 6°W and 3°E. The land is green in the south, with forests and fruit trees, and semi-arid in the north. Most of central Burkina Faso lies on a savanna plateau, 198–305 metres (650–1,001 ft) above sea level, with fields, brush, and scattered trees. Burkina Faso's game preserves – the most important of which are Arly, Nazinga, and W National Park—contain lions, elephants, hippopotamus, monkeys, common warthogs, and antelopes. Previously the endangered painted hunting dog, Lycaon pictus occurred in Burkina Faso, but, although the last sightings were made in Arli National Park, the species is considered extirpated from Burkina Faso.
Burundi is located in East Africa, to the east of the Democratic Republic of the Congo, at the coordinates 3°30′S30°0′E.
Desertification is a type of gradual land degradation of fertile land into arid desert due to a combination of natural processes and human activities.
Niger is a landlocked nation in West Africa located along the border between the Sahara and Sub-Saharan regions. Its geographic coordinates are longitude 16°N and latitude 8°E
Overgrazing occurs when plants are exposed to intensive grazing for extended periods of time, or without sufficient recovery periods. It can be caused by either livestock in poorly managed agricultural applications, game reserves, or nature reserves. It can also be caused by immobile, travel restricted populations of native or non-native wild animals.
Mauritania, a country in the Western Region of the continent of Africa, is generally flat, its 1,030,700 square kilometres forming vast, arid plains broken by occasional ridges and clifflike outcroppings. Mauritania is the world’s largest country lying entirely below an altitude of 1,000 metres (3,300 ft). It borders the North Atlantic Ocean, between Senegal and Western Sahara, Mali and Algeria. It is considered part of both the Sahel and the Maghreb. A series of scarps face southwest, longitudinally bisecting these plains in the center of the country. The scarps also separate a series of sandstone plateaus, the highest of which is the Adrar Plateau, reaching an elevation of 500 metres or 1,640 feet. Spring-fed oases lie at the foot of some of the scarps. Isolated peaks, often rich in minerals, rise above the plateaus; the smaller peaks are called Guelbs and the larger ones Kedias. The concentric Guelb er Richat is a prominent feature of the north-central region. Kediet ej Jill, near the city of Zouîrât, has an elevation of 915 metres or 3,002 feet and is the highest peak.
The Sahel region, or Sahelian acacia savanna, is a biogeographical region in Africa. It is the transition zone between the more humid Sudanian savannas to its south and the drier Sahara to the north. The Sahel has a hot semi-arid climate and stretches across the southernmost latitudes of North Africa between the Atlantic Ocean and the Red Sea. Although geographically located in the tropics, the Sahel does not have a tropical climate.
Land degradation is a process where land becomes less healthy and productive due to a combination of human activities or natural conditions. The causes for land degradation are numerous and complex. Human activities are often the main cause, such as unsustainable land management practices. Natural hazards are excluded as a cause; however human activities can indirectly affect phenomena such as floods and wildfires.
The Sahel region of Africa has long experienced a series of historic droughts, dating back to at least the 17th century. The Sahel region is a climate zone sandwiched between the Sudanian Savanna to the south and the Sahara desert to the north, across West and Central Africa. While the frequency of drought in the region is thought to have increased from the end of the 19th century, three long droughts have had dramatic environmental and societal effects upon the Sahel nations. Famine followed severe droughts in the 1910s, the 1940s, and the 1960s, 1970s and 1980s, although a partial recovery occurred from 1975-80. The most recent drought occurred in 2012.
The Great Green Wall or Great Green Wall for the Sahara and the Sahel is a project adopted by the African Union in 2007, initially conceived as a way to combat desertification in the Sahel region and hold back expansion of the Sahara desert, by planting a wall of trees stretching across the entire Sahel from Djibouti, Djibouti to Dakar, Senegal. The original dimensions of the "wall" were to be 15 km wide and 7,775 km long, but the program expanded to encompass nations in both northern and western Africa. The concept evolved into promoting water harvesting techniques, greenery protection and improving indigenous land use techniques, aimed at creating a mosaic of green and productive landscapes across North Africa. Later it adopted the view that desert boundaries change based on rainfall variations.
African environmental problems are problems caused by the direct and indirect human impacts on the natural environment and affect humans and nearly all forms of life in Africa. Issues include deforestation, soil degradation, air pollution, water pollution, coastal erosion, garbage pollution, climate change, Oil spills, Biodiversity loss, and water scarcity. These issues result in environmental conflict and are connected to broader social struggles for democracy and sovereignty. The scarcity of climate adaptation techniques in Africa makes it the least resilient continent to climate change.
Michael Mortimore was a British geographer and a prolific researcher of issues in the African drylands. He was an academic in Nigerian universities for over 25 years. He ran a British research consultancy, Drylands Research. He is best known for an anti-Malthusian account of population-environment relationships, More People, Less Erosion, and field-based studies of adaptation to drought.
Andrew Warren is a British physical geographer. He is Emeritus Professor of Geography at University College London, UK.
Senegal's environmental issues are varied. According to the CIA world factbook pressing problems exist with: diminishing wildlife populations which are threatened by poaching, deforestation, overgrazing, soil erosion, desertification, and overfishing.
Climate change in Senegal will have wide reaching impacts on many aspects of life in Senegal. Climate change will cause an increase in average temperatures over west Africa by between 1.5 and 4 °C by mid-century, relative to 1986–2005. Projections of rainfall indicate an overall decrease in rainfall and an increase in intense mega-storm events over the Sahel. The sea level is expected to rise faster in West Africa than the global average. Although Senegal is currently not a major contributor to global greenhouse gas emissions, it is one of the countries most vulnerable to climate change.
Natural disasters in Nigeria are mainly related to the climate of Nigeria, which has been reported to cause loss of lives and properties. A natural disaster might be caused by flooding, landslides, and insect infestation, among others. To be classified as a disaster, there is needs to be a profound environmental effect or human loss which must lead to financial loss. This occurrence has become an issue of concern, threatening large populations living in diverse environments in recent years.
The Algerian Green Dam refers to a project initiated in Algeria in the 1960s to plant millions of trees to stop desertification, specifically to prevent the northward advancement of the Sahara Desert.
Rainwater harvesting in the Sahel is a combination of "indigenous and innovative" agricultural strategies that "plant the rain" and reduce evaporation, so that crops have access to soil moisture for the longest possible period of time. In the resource-poor drylands of the Sahel region of Africa, irrigation systems and chemical fertilizers are often prohibitively expensive and thus uncommon: so increasing or maintaining crop yields in the face of climate change depends on augmenting the region's extant rainfed agriculture systems to "increase water storage within the soil and replenish soil nutrients." Rainwater harvesting is a form of agricultural water management. Rainwater harvesting is most effective when combined with systems for soil regeneration and organic-matter management.
The majority of Ghana's income and jobs are produced directly and indirectly by the land, which is a vital resource for our nation's prosperity. It sustains the provision of ecosystem services as well as the agricultural, forestry, and fishing livelihoods of the vast majority of people, particularly those living in rural areas. Despite these advantages, there are a number of temporal and spatial factors contributing to the degradation of our land resources, such as deforestation, erosion, declining soil fertility and productivity, deterioration of rangelands, desertification, and deterioration of water bodies.
The severity of desertification in the drylands of the world made the United Nations Organization to adopt a Convention to Combat Desertification (CCD) in 1994. Nigeria approved the National Action Programme (NAP) as a primary tool for the implementation of the Convention in 1997.
↑ Grove, A.T. (1973). Desertification in the African Environment. In Drought in Africa: Report of the 1973 Symposium (D. Dalby and R.J. Harrison Church, eds.) London, School of Oriental and African Studies.
↑ Lal R (1993). Soil erosion and conservation in West Africa. In World Soil Erosion and Conservation, Ed. Pimentel D , pp. 7–25. Cambridge Univ. Press, Cambridge.
1 2 3 4 5 6 7 Ikazaki, K. (2015). Desertification and a new countermeasure in the Sahel, West Africa. Soil Science and Plant Nutrition, 61(3), 372-383.
↑ Daniel HA , Langham WH (1936). The effect of wind erosion and cultivation on the total nitrogen and organic matter content of soils in the Southern High Plains. J. Am. Soc. Agron., 28, 587–596. doi:10.2134/agronj1936.00021962002800080001x
↑ Zobeck TM , Fryrear DW (1986). Chemical and physical characteristics of windblown sediment: II. Chemical characteristics and total soil and nutrient discharge. Trans. ASAE , 29, 1037–1041. doi:10.13031/2013.30266
↑ Michels K, Sivakumar MVK , Allison BE (1993). Wind erosion in the southern Sahelian zone and induced constraints to pearl millet production. Agric. For. Meteorol., 67, 65–77. doi:10.1016/0168-1923(93)90050-R
↑ United Nations-Environmental Programme UNEP (1984) Desertification Control in Africa (2 Völs.), UNEP, Nairobi.
↑ Rapp, A. and Hellden, U. (1979) Research on Environmental Monitoring Methods for Land use Planning in African Drylands, Department of Geography, University of Lunds, Sweden.
↑ Hayashi K 2005: Practical technology development for farmers in the Sahel, West Africa: Proposing a new soil fertility management method for degrading sandy soil through the use of conventional information. Japan Assoc. Int. Collaboration Agric. For. (JAICAF) Expert Bull., 25, 12−26 (in Japanese).
↑ Hayashi K , Shinjo H , Tanaka U , Tahirou A , Matsunaga R 2006: Actual situation of local soil fertility management on agricultural land in the Sahel, West Africa. JIRCAS Res. Highlights , 13, 17−18.
↑ DARKOH, M. B. K. (1998). THE NATURE, CAUSES AND CONSEQUENCES OF DESERTIFICATION IN THE DRYLANDS OF AFRICA. Department of Environmental Science, University of Botswana, Gaborone: John Wiley & Sons, Ltd. p.15.
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