Services & Products
- Calculate your carbon emissions Offset your carbon emissions
Sweet solutions: the role of bees and Impact Investments in environmental restoration
A pathway to sustainability for uk enterprises, the vital role of reforestation in bird migration, become shareholder, sustainable investments.
- Become a DGB shareholder Invest in our projects
Nature-based solutions
Stakeholders, how it works, project updates, greenzone reforestation project: big steps in cameroon, dgb’s hongera reforestation project: 600 hectares and growing, final validation received for bulindi chimpanzee habitat restoration project.
- Subscribe to our newsletter Download our favourite ebook
Latest Article
- Calculate carbon footprint Calculate environmental footprint CSRD reporting Case studies
- Carbon credits Biodiversity credits Plastic credits Tree planting for business
- DGB on the stock market Public company as a mission Investor relations
- Green bonds investment Impact investing Investing in carbon credits
- Our projects Updates from the projects Project pipeline
- Landowners and farmers Local communities Regulators and policymakers
- What is a carbon project? What we can do for your land How to start a carbon project
- Blog Newsroom Technology
- Events eBooks Podcasts
It looks like you’re browsing from Netherlands. Click here to switch to the Dutch →
Desertification - Sahel case study
- Share this article:
Desertification in the Sahel region is a pressing environmental issue with far-reaching consequences. In this article, we will explore the causes, effects, and potential solutions to combat desertification, using a case study from the Sahel region. By examining the unique challenges faced in this area, we can gain insights into the broader fight against desertification and the importance of sustainable land management practices. The Sahel is a semi-arid zone stretching from the Atlantic Ocean in West Africa to the Red Sea in the East, through northern Senegal, southern Mauritania, the great bend of the Niger River in Mali, Burkina Faso, southern Niger, northeastern Nigeria, south-central Chad, and into Sudan ( Brittanica ).
It is a biogeographical transition between the arid Sahara Desert to the North and the more humid savanna systems on its Southern side.
Desertification in the Sahel has increased over the last number of years. It has been increasingly impacted by desertification, especially during the second half of the twentieth century. The whole Sahel region in Africa has been affected by devastating droughts, bordering the Sahara Desert and the Savannas.
During this period, the Sahara desert area grew by roughly 10% , most of which in the Southward direction into the semi-arid steppes of the Sahel.
Understanding desertification in the Sahel
The Sahel region, stretching across Africa from the Atlantic Ocean to the Red Sea, is characterized by fragile ecosystems and vulnerable communities. The combination of climate change, overgrazing, deforestation , and improper agricultural practices has resulted in extensive land degradation and desertification. The consequences of desertification in the Sahel are severe, including food insecurity, loss of biodiversity, and displacement of communities.
in the region, for around 8 months of the year, the weather is dry. The rainy season only happens for a few short months and only produces around 4-8 inches of water. The population growth over the years has caused illegal farming to take place over the last few years and has resulted in major soil erosion and desertification to take place.
Examining a specific case study in the Sahel region sheds light on the complexities and impacts of desertification. In a particular community, unsustainable farming methods and drought have led to soil erosion and degradation. The once-fertile land has turned into arid, unproductive soil, forcing farmers to abandon their livelihoods and seek alternative means of survival. This case study highlights the urgent need for intervention and sustainable land management practices in the region.
Addressing the challenges
To combat desertification effectively, a multi-faceted approach is necessary. First and foremost, raising awareness about the issue and its consequences is crucial. Governments, NGOs, and local communities must collaborate to implement sustainable land management practices. This involves promoting agroforestry, conservation farming, and reforestation initiatives to restore degraded land and improve soil health. Additionally, supporting alternative income-generating activities and providing access to water resources can help alleviate pressure on the land and reduce vulnerability to drought.
Read more: Preventing desertification: Top 5 success stories
The impact of humans on the Sahel
The impact of humans on the Sahel region is a critical factor contributing to its current challenges and environmental changes. Human activities, including armed violence, climate change, deforestation, and overgrazing, have had significant consequences for both the ecosystem and the local communities. While the area of the Sahel region is already considered to be a dry place, the impact of the human population in the area has really affected how the area continues to evolve. Towns are popping up all over the place, and because of this, more land is being used than ever before. The ground that they are building their lives on quickly began to die and became extremely unhealthy for any type of growth. This has made headlines everywhere and even caught the attention of the United Nations. In 1994, the United Nations declared that June 17th would be known as the World Day to Combat Desertification and Drought. . This was a result of the large-scale droughts and famines that had been taking place and were at their height between 1968 and 1974.
In conclusion, the impact of humans on the Sahel is a multifaceted issue. The region faces a humanitarian crisis alongside security concerns, with climate change and human activities playing significant roles. Desertification caused by climate change, deforestation, and overgrazing has resulted in land degradation, loss of vegetation, and increased vulnerability to droughts and food insecurity. Implementing sustainable land management strategies is essential to mitigate the impact and promote the resilience of the Sahel's ecosystems and communities.
Droughts, grazing, and recharging aquifers
The Sahel’s natural climate cycles make it vulnerable to droughts throughout the year. But, during the second half of the twentieth century, the region also experienced significant increases in human population and resulting in increases in the exploitation of the lands through (cattle) grazing, wood- and bush consumption for firewood, and crop growth where possible.
These anthropogenic processes accelerated during the 1960s when relatively high rainfall amounts were recorded in the region for short periods of time, and grazing and agricultural expansion were promoted by the governments of the Sahel countries, seeing a good opportunity to use the region’s ecosystem for maximizing economic returns.
This resulted in the removal of large parts of the natural vegetation, including shrubs, grasses, and trees, and replacing them with crops and grass types that were suitable for (short-term) grazing.
The world effort for the Sahel:
Natural aquifers, which were previously able to replenish their groundwater stocks during the natural climate cycles, were no longer able to do so, and the regions closest to the Sahara desert were increasingly desertified.
Removing the natural vegetation removed plant roots that bound the soil together, with over-exploitation by grazing eating away much of the grass.
Agricultural activity disrupted the natural system, forcing significant parts of the Sahel region to become dry and barren. Before the particularly bad famine of 1984, desertification was solely put down to climatic causes.
As the Sahel dries, the Sahara advances : and it is estimated to advance with a rate of 60 kilometres the Sahel lost and the Sahara desert gained per year. Human influence is an important factor in the Sahel’s desertification, but not all can be attributed to human behaviour, says Sumant Nigam, a climate scientist at the University of Maryland.
'There is an important anthropogenic influence there, but it is also being met with natural cycles of climate variability that add and subtract in different periods', Nigam said. 'Understanding both is important for both attribution and prediction.' Ecologists have been meeting all over the world to discuss the desertification of the Sahel at length. While many possible solutions have been proposed, a few goals have been established and are being worked on. The Food and Agricultural Organization of the United Nations has not become involved and is working to create a long-lasting impact on the Sahel Region. However, after the mid-1980s , human-caused contributions were identified and taken seriously by the United Nations and many non-governmental organizations. Severe and long-lasting droughts followed throughout the 1960s-1980s, and impacted the human settlements in the forms of famine and starvation, allowing the Sahara desert to continue to expand southward. As a result, a barren and waterless landscape has emerged, with the northernmost sections of the Sahel transformed into new sections of the Sahara Desert. Even though the levels of drought have decreased since the 1990s, other significant reductions in rainfall have been recorded in the region, including a severe drought in 2012. It is estimated that over 23 million people in the Sahel region are facing severe food insecurity in 2022, and the European Commission projects that the crisis will worsen further amidst rising social security struggles. Now, the goal is to see change take place by 2063, a year that seems far away but is a start in the efforts to rebuild the Sahel Region.
Before you go...
As DGB Group, our sole purpose is to rebuild trust and serve the public by making the right information available to everyone. By subscribing to our mailing newsletter, you can get the latest tips and trends from DGB Group's expert team in your inbox. Sign up now and never miss the insights.
Popular Topics
- Carbon offsetting (80)
- Sustainability (68)
- Biodiversity (57)
- Carbon credits (53)
- Carbon markets (49)
- Nature conservation (49)
- Net zero (40)
- Tree planting (40)
- Nature-based solutions (37)
- Carbon emissions (34)
Recommended
Desertification in africa and how desertification can affect people in africa, three desertification examples, preventing desertification: top 5 success stories, featured resource, the power of trees.
Read other articles
Did you know that worker bees can fly up to 8 kilometres a day, wearing out their wings after coveri..
As the global focus on reducing carbon emissions intensifies, many UK companies are stepping up thei..
Each year, millions of birds embark on one of nature’s most incredible phenomena: migration. These l..
Belgium’s leading firms in carbon compensation efforts
This week, we spotlight Belgium, a country home to several companies at the forefront of reducing th..
Let’s get to know you
Let's talk about how we can create value together for your sustainability journey.
Stay Updated
- Trees for Businesses
- Green Bonds
- Investor Portal Login
- ESG Reporting
- Carbon Footprint Analysis
- Carbon Footprint Calculator
- Carbon Credits
- Corporate Sustainability Reporting Directive
- Plastic Credits
- Biodiversity Credits
- Monthly Tree Planting
- Carbon Projects for Landowners
- Board of Directors
- Investor Relations
- Investor Events
- Press Releases
- Annual Financial Reports
- Case Studies
- Agriculture
- Biodiversity
- Carbon Offsetting
- Carbon Pricing
- Clean Energy
- Deforestation
- Desertification
- Endangered Species
- Plastic Pollution
- Saving Water
- Sustainability
- Sustainable Development
- Vital Habitats
- Waste Management
- Corporate governance & policies
Case Study: Sahel Desertification
What is desertification: It is the term used to describe the changing of semi arid (dry) areas into desert. It is severe in Sudan, Chad, Senegal and Burkina Faso
What are the causes:
- Overcultivation: the land is continually used for crops and does not have time to recover eventually al the nutrients are depleted (taken out) and the ground eventually turns to dust.
- Overgrazing: In some areas animals have eaten all the vegetation leaving bare soil.
- Deforestation: Cutting down trees leaves soil open to erosion by wind and rain.
- Climate Change: Decrease in rainfall and rise in temperatures causes vegetation to die
What is being done to solve the problem?
Over the past twelve years Oxfam has worked with local villagers in Yatenga (Burkina Faso) training them in the process of BUNDING. This is building lines of stones across a slope to stop water and soil running away. This method preserves the topsoil and has improved farming and food production in the village.
Burkina Faso - desertification
This video shows the Sahel region south of the Sahara is at risk of becoming desert. Elders in a village in Burkina Faso describe how the area has changed from a fertile area to a drought-prone near-desert. The area experiences a dry season which can last up to eight or nine months. During this time rivers dry up and people, animals and crops are jeopardised.
This video showcases the Sahel region
Bringing dry land in the Sahel back to life
Facebook Twitter Print Email
Millions of hectares of farmland are lost to the desert each year in Africa’s Sahel region, but the UN Food and Agriculture Organization (FAO) is showing that traditional knowledge, combined with the latest technology, can turn arid ground back into fertile soil.
Those trying to grow crops in the Sahel region are often faced with poor soil, erratic rainfail and long periods of drought. However, the introduction of a state-of-the art heavy digger, the Delfino plough, is proving to be, literally, a breakthrough.
As part of its Action Against Desertification (AAD) programme, the FAO has brought the Delfino to four countries in the Sahel region – Burkina Faso, Niger, Nigeria and Senegal – to cut through impacted, bone-dry soil to a depth of more than half a metre.
The Delfino plough is extremely efficient: one hundred farmers digging irrigation ditches by hand can cover a hectare a day, but when the Delfino is hooked to a tractor, it can cover 15 to 20 hectares in a day.
Once an area is ploughed, the seeds of woody and herbaceous native species are then sown directly, and inoculated seedlings planted. These species are very resilient and work well in degraded land, providing vegetation cover and improving the productivity of previously barren lands.
In Burkina Faso and Niger, the target number of hectares for immediate restoration has already been met and extended thanks to the Delfino plough. In Nigeria and Senegal, it is working to scale up the restoration of degraded land.
Farming seen through a half-moon lens
This technology, whilst impressive, is proving to be successful because it is being used in tandem with traditional farming techniques.
“In the end the Delfino is just a plough. A very good and suitable plough, but a plough all the same,” says Moctar Sacande, Coordinator of FAO’s Action Against Desertification programme. “It is when we use it appropriately and in consultation and cooperation that we see such progress.”
The half-moon is a traditional Sahel planting method which creates contours to stop rainwater runoff, improving water infiltration and keeping the soil moist for longer. This creates favourable micro-climate conditions allowing seeds and seedlings to flourish.
The Delfino creates large half-moon catchments ready for planting seeds and seedlings, boosting rainwater harvesting tenfold and making soil more permeable for planting than the traditional - and backbreaking – method of digging by hand.
“The whole community is involved and has benefitted from fodder crops such as hay as high as their knees within just two years”, says Mr. Sacande. “They can feed their livestock and sell the surplus, and move on to gathering products such as edible fruits, natural oils for soaps, wild honey and plants for traditional medicine”.
Women taking the lead
According to Nora Berrahmouni, who was FAO’s Senior Forestry Officer for the African Regional Office when the Delfino was deployed, the plough will also reduce the burden on women.
“The season for the very hard work of hand-digging the half-moon irrigation dams comes when the men of the community have had to move with the animals. So, the work falls on the women,” says Ms. Berrahmouni.
Because the Delfino plough significantly speeds up the ploughing process and reduces the physical labour needed, it gives women extra time to manage their multitude of other tasks.
The project also aims to boost women’s participation in local land restoration on a bigger scale, offering them leadership roles through the village committees that plan the work of restoring land. Under the AAD programme, each site selected for restoration is encouraged to set up a village committee to manage the resources, so as to take ownership right from the beginning.
“Many women are running the local village committees which organise these activities and they are telling us they feel more empowered and respected,” offers Mr. Sacande.
Respecting local knowledge and traditional skills is another key to success. Communities have long understood that half-moon dams are the best way of harvesting rainwater for the long dry season. The mighty Delfino is just making the job more efficient and less physically demanding.
Millions of hectares lost to the desert, forests under threat
And it is urgent that progress is made. Land loss is a driver of many other problems such as hunger, poverty, unemployment, forced migration, conflict and an increased risk of extreme weather events related to climate change.
In Burkina Faso, for example, a third of the landscape is degraded. This means that over nine million hectares of land, once used for agriculture, is no longer viable for farming.
It is projected that degradation will continue to expand at 360 000 hectares per year. If the situation is not reversed, forests are at risk of being cleared to make way for productive agricultural land.
Africa is currently losing four million hectares of forest every year for this reason, yet has more than 700 million hectares of degraded land viable for restoration. By bringing degraded land back to life, farmers do not have to clear additional forest land to turn into cropland for Africa’s rising population and growing food demands.
When Mr. Sacande talks about restoring land in Africa, the passion in his voice is evident. “Restoring degraded land back to productive good health is a huge opportunity for Africa. It brings big social and economic benefits to rural farming communities,” he says. “It’s a bulwark against climate change and it brings technology to enhance traditional knowledge.”
A version of this story first appeared on the FAO website .
- Burkina Faso
- agriculture and food security
- Desertification
- climate action
Advertisement
The causes, effects and challenges of Sahelian droughts: a critical review
- Original Article
- Published: 18 May 2013
- Volume 14 , pages 145–156, ( 2014 )
Cite this article
- Epule Terence Epule 1 ,
- Changhui Peng 1 ,
- Laurent Lepage 1 &
- Zhi Chen 2
3048 Accesses
74 Citations
4 Altmetric
Explore all metrics
This paper is a critical synthesis of the causes, effects and challenges of the Sahelian droughts. The results show that the four main causes of the Sahelian droughts are as follows: sea surface temperature changes, vegetation and land degradation, dust feedbacks and human-induced climate change. However, human-induced climate change is seen as the major drought-determining factor because it controls sea surface temperatures, dust feedbacks and vegetation degradation. Increase rainfall and greening have been observed in the Sahel since the 1990s; yet, food yields remain low while tree mortality rates are high. The implication of this is that the rainfall is not available for agriculture since various human-induced climate change processes such as deforestation and the expansions of arable farms do not make the moisture available for agriculture. The increase in tree mortality has also been found to increase atmospheric CO 2 in the study area. However, this study hypothesizes that the increase in CO 2 might be responsible for the increase in greening and rainfall observed. This can be explained by an increased aerial fertilization effect of CO 2 that triggers plant productivity and water management efficiency through reduced transpiration. Also, the increase greening can be attributed to rural–urban migration which reduces the pressure of the population on the land. The remittances from migrant urban workers may make farming more sustainable in the rural areas, thus enhancing greening. The principal challenges in overcoming the effects of the droughts are HIV/AIDS and Malaria, political instability, data availability, proliferation of extensive non-mechanized farms and lack of adequate observations.
This is a preview of subscription content, log in via an institution to check access.
Access this article
Subscribe and save.
- Get 10 units per month
- Download Article/Chapter or eBook
- 1 Unit = 1 Article or 1 Chapter
- Cancel anytime
Price includes VAT (Russian Federation)
Instant access to the full article PDF.
Rent this article via DeepDyve
Institutional subscriptions
Similar content being viewed by others
The relationship between drought activity and vegetation cover in northwest china from 1982 to 2013.
Climate Change and Drought in the Dryland Areas of Nigeria
Drought Indices, Drought Impacts, CO 2 , and Warming: a Historical and Geologic Perspective
Adhikari M, Ishizaka Y, Minda H, Kazaoka R, Jensen JB, Gras JL, Nakajima T (2005) Vertical distribution of cloud condensation nuclei concentrations and their effect on microphysical properties of clouds over the sea near the southwest islands of Japan. J Geophys Res 110:D10203. doi: 10.1029/2004JD004758
Article Google Scholar
Allen CD, Macalady A, Chenchouni H, Bachelet D, McDowell N, Vennetier M, Kitzberger T, Rigling A, Breshears DD, Hogg EH, Gonzalez P, Fensham R, Zhang Z, Castro J, Demidova N, Lim JH, Allard G, Running SW, Semerci A, Cobb N (2009) A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests. Forest Ecol Manag 259:660–684. doi: 10.1016/j.foreco.2009.09.001
Antwi-Agyei P, Fraser EDG, Dougill AJ, Stringer LC, Smelton E (2012) Mapping the vulnerability of crop production to droughts in Ghana using rainfall yield and socioeconomic data. Appl Geogr 32:324–334. doi: 10.1016/j.apgeog.2011.06.010
Anyamba A, Eastman J (1996) Interannual variability of NDVI over Africa and its relation to El Niño/Southern Oscillation. Inter J Remote Sens 17:2533–2548
Anyamba A, Tucker CJ (2005) Analysis of Sahelian Vegetation dynamics using NOAA-AVHRR NDVI data from 1981–2003. J Arid Environ 63:595–614
Asch F, Dingkuhn M, Sow A, Audebert A (2005) Drought-induced changes in rooting patterns and assimilate partitioning between root and shoot in upland rice. Field Crops Res 93:223–236. doi: 10.1016/j.fcr.2004.10.002
Bader J, Latif M (2003) The impact of decadal-scale Indian Ocean sea surface temperature anomalies on Sahelian rainfall and the North Atlantic Oscillation. Geophys Res Lett 30:2165–2169
Baldocchi D (2008) Breathing of the terrestrial biosphere: lessons learned from a global network of carbon dioxide flux measurement systems. Aust J Bot 56(1):1–26
Article CAS Google Scholar
Biasutti M, Giannini A (2006) Robust Sahel drying in response to late 20th century forcings. Geophys Res Lett 33:L11706
Camberlin P, Janicot S, Poccard I (2001) Seasonality and Atmospheric dynamics of the teleconnection between African rainfall and tropical sea-Surface temperature: Atlantic vs ENSO. Inter J Clim 21:973–1005. doi: 10.1002/joc.673
Charney JM, Quirk WJ, Chow SH, Kornfield J (1977) A comparative study of the effects of albedo change on drought in semi-arid regions. J Atmos Sci 34(9):1366–1386
Chelliah M, Bell GD (2004) Tropical multidecadal and interannual climate variability in the NCEP–NCAR reanalysis. J Clim 17:1777–1803
Clover J (2010) Food security in sub-Saharan Africa. Afr Food Rev 12(1):5–15. doi: 10.1080/10246029.2003.9627566
Google Scholar
De Rouw A (2004) Improving yields and reducing risks in pearl millet farming in the African Sahel. Agric Syst 81:73–93
Dilley M, Chen RS, Deichmann U, Lerner-Lam AL, Arnold M (2005) Natural disaster hotspots: a global risk analysis. Disaster Risk Management Series No, 5. The World Bank, Washington
Dinku T, Ceccato P, Grover-Kopec E, Lemma M, Connor SJ, Ropelewski CF (2007) Validation of satellite rainfall products over East Africa’s complex topography. Inter J Remote Sens 28(7):1503–1526
Eklundh L, Olsson L (2003) Vegetation index trends for the African Sahel 1982–1999. Geophys Res Lett 30(8):1430. doi: 10.1029/2002GL016772
Epule TE, Peng C, Lepage L, Chen Z (2011) Forest loss triggers in Cameroon. A quantitative assessment using multiple linear regression approach. J Geogr Geol 3(1):30–40. doi: 10.5539/jgg.v3n1p30
Epule TE, Peng C, Lepage L, Chen Z (2012a) Rainfall and deforestation dilemma for cereal Production in the Sudano-Sahel of Cameroon. J Agric Sci 4(2):1–9. doi: 10.5539/jas.v4n2p1
Epule TE, Peng C, Lepage L, Balgah SN, Mafany NM (2012b) Can the African food supply model learn from the Asian food supply model? Predictions with selected variables and quantitative methods. Environ Deve Sus 593–610. doi: 10.1007/s10668-012-9341-0
Food and Agricultural Organization of the United Nations (2010) Forest resource assessment. FAO Forestry paper no 163, FAO, Rome. [Online] Available http://www.fao.org [12 January 2013]
Food and Agricultural Organization of the United Nations, FAO (2006) Global forest resources assessment 2005—progress towards sustainable forest management. Rome. FAO Forestry Paper No. 147
Food and Agricultural Organization of the United Nations, United Nations Industrial Development Organization (2008) Agricultural mechanization in Africa…Time for action. Planning investment for enhanced agricultural productivity report of an expert group meeting in January 2008, Vienna Austria. FAO, Rome. Available from http://www.unido.org/fileadmin/user_media/Publications/Pub_free/agricultural_mechanization_in_Africa.pdf . Accessed 1 Feb 2013
Frelich LE, Reich PB (2010) Will environmental changes reinforce the impact of global warming on the prairie–forest border of central North America? Front Ecol Environ 8(7):371–378. doi: 10.1890/080191
Fuller DO, Ottke C (2002) Land cover, Rainfall and Land-Surface Albedo in West Africa. Clim Chang 54:181–204
Giannini A, Saravanan R, Chang P (2003) Oceanic forcing of Sahel Rainfall on interannual to interdecadal timescales. Science 302:1027–1030
Giannini A, Saravanan R, Chang P (2005) Dynamics of the boreal summer African monsoon in the NSIPP1 atmospheric model. Clim Dyn 25:517–535. doi: 10.1007/s00382-005-0056-x
Giannini A, Biasutti M, Held IM, Sobel AH (2008) A global perspective on African climate. Clim Chang 90:359–383. doi: 10.1007/s10584-008-9396-y
Glantz MH (1994) Drought, desertification and food production. In: Glantz MH (ed) Drought follows the plow. Cambridge University Press, Cambridge, pp 9–30
Gleckler PJ, Taylor KE, Doutriauz C (2008) Performance metrics for climate models. J Geophys Res 113:D06104. doi: 10.1029/2007JD008972
Gonzalez P (2001) Desertification and a shift of forest species in the West African Sahel. Clim Res 17:217–228
Gonzalez P, Tucker CJ, Sy H (2012) Tree density and species decline in the African Sahel attributable to climate. J Arid Environ 78:55–64. doi: 10.1016/j.jaridenv.2011.11.001
Hagos SM, Cook KH (2008) Ocean warming and the late-twentieth century Sahel drought and recovery. J Clim 21:3797–3814. doi: 10.1175/2008JCLI2055.1
Haile M (2005) Weather patterns, food security and humanitarian response in sub-Saharan Africa. Philos Trans R Soc 360:2169–2182. doi: 10.1098/rstb.2005.1746
Held IM, Delworth TL, Lu J, Knutson T, Findell K (2005) Simulations of Sahel drought in the 20th and 21st centuries. PNAS 102(50):17891–17896. doi: 10.1073/pnas.0509057102
Herrmann SM, Anyamba A, Tucker CJ (2005) Recent trends in vegetation dynamics in the African Sahel and their relationship to climate. Glob Environ Chang 15:394–404
Hiernaux P, Diarra L, Trichon V, Mougin E, Soumaguel N, Baup F (2009) Woody plant population dynamics in response to climate changes from 1984 to 2006 in Sahel (Gourma, Mali). J Hydrol 375:103–113
Hoerling MP, Hurrell JW, Eischeid J, Phillips AS (2006) Detection and attribution of 20th century Northern and Southern African monsoon change. J Clim 19:3989–4008. doi: 10.1175/JCLI3842.1
Hui WJ, Cook B, Ravi S, Fuentes JD, D’Odorico P (2008) Dust-rainfall feedbacks in the West African Sahel. Water Resour Res 44:W05202. doi: 10.1029/2008WR006885
Hulme M (2001) Climatic perspectives on Sahelian desiccation: 1973–1998. Glob Environ Chang 11:19–29
Hurrell JW (1995) Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269:676–679
Ifejika Speranza CI (2006) Droughts and famines: the underlying factors and the causal link among agro-pastoral households in semi-arid Makueni district, Kenya. Glob Environ Chang 18:220–233
Janicot S, Mounier F, Gervois S, Sultan B, Kiladis GN (2010) The dynamics of the West African Monsoon. Part V: the Detection and role of the dominant modes of convectively coupled equatorial Rossby waves. J Clim 23:4005–4024. doi: 10.1175/2010JCLI3221.1
Kang SM, Held IM, Frierson DWM, Zhao M (2008) The response of the ITCZ to extratropical thermal forcing: idealized slab-ocean experiments with a GCM. J Clim 21:3521–3532. doi: 10.1175/2007JCLI2146.1
Kaufman YJ, Tanré D, Boucher O (2002) A satellite view of aerosols in the climate system. Nature 419:215–223. doi: 10.1038/nature01091
Knorr W, Gobron N, Scholze M, Kaminski T, Schnur R, Pinty B (2007) Impact of terrestrial biosphere carbon exchanges on the anomalous CO 2 increase in 2002–2003. Geophys Res Lett 34:L09703. doi: 10.1029/2006/GL029019
Knutson TR, Delworth TL, Dixon KW, Held IM, Lu J, Ramaswamy V, Schwarzkopf MD, Stenchikov G, Stouffer RJ (2006) Assessment of twenty-century regional surface temperature trends using the GFDL CM2 coupled models. J Clim 19:1624–1651. doi: 10.1175/JCLI3709.1
Koepke D, Kolb T, Adams H (2010) Variation in woody plant mortality and dieback from severe drought among soils, plant groups, and species within a northern Arizona ecotone. Oecologia (Berl.) 163(4):1079–1090. doi: 10.1007/s00442-010-1671-8
Lamb PJ (1982) Persistence of Sub-Saharan drought. Nature 299:36–47
Lamprey HF (1975) Report on the desert encroachment reconnaissance in northern Sudan, 21 Oct. to 10 Nov. UNESCO/UNEP, pp 16
Leuzinger S, Quinn TR (2011) How do we improve Earth system models? Integrating Earth system models, ecosystem models, experiments and long-term data. New Phytol 191(1):15–18. doi: 10.1111/j.1469-8137.2011.03778.x
Li X, Maring H, Savoie D, Voss K, Prospero JM (1996) Dominance of mineral dust in aerosol light-scattering in the North Atlantic trade winds. Nature 380:416–422
Lindell L, Astrom M, Oberg T (2010a) Land-use versus natural controls on soil fertility in the Subandean Amazon. Peru Sci Total Environ 408(4):965–975
Lindell L, Astrom M, Oberg T (2010b) Land-use change versus natural controls on stream water chemistry in the Subandean Amazon. Peru Appl Geochem 25(3):485–495
Lintner BR, Chiang JCH (2006) Adjustment of the remote tropical climate system to El Nino conditions. J Clim 20:2544–2557. doi: 10.1175/JCLI4138.1
Lohmann U, Feichter J (2005) Global indirect aerosol effects: a review. Atmos Chem Phys 5:715–737
Lu J, Delworth TL (2005) Oceanic forcing of the late 20th century Sahel drought. Geophys Res Lett 32:L22706. doi: 10.1029/2005GL023316
Lwanga JS (2003) Localized tree mortality following the drought of 1999 at Ngogo, Kibale National Park, Uganda. Afr J Ecol 41:194–196
Mahowald NM, Kiehl LM (2003) Mineral aerosol and cloud interactions. Geophys Res Lett 30(9):1475. doi: 10.1029/2002GL016762
Maranz S (2009) Tree mortality in the African Sahel indicates an anthropogenic ecosystem displaced by climate change. J Biogeogr 36:1181–1193
Maynard K, Royer JF, Chauvin F (2002) Impact of greenhouse warming on the West African summer monsoon. Clim Dyn 19:499–514
McKee TB, Doesken NJ, Kleist J (1993) The relationship of drought frequency and duration to time scales. In: Proceedings of the 8th conference on applied climatology, Anaheim, California. 17–22 January 1993. American Meterological Society
Meir P, Metcalfe DB, Costa ACL, Fisher RA (2008) The fate of assimilated carbon during drought: impacts on respiration in Amozon rainforests. Phil Trans Roy Soc B 363:1849–1855
Molen MK, Dolman AJ, Ciais P, Eglin T, Gobron N, Law BE, Meir P, Peters W, Phillips OL, Reichstein M, Chen T, Dekker SC, Doubkova M, Friedi MA, Jung M, Hurk BJJM, De Jeu RAM, Kruijt B, Ohta T, Rebels KT, Plummer S, Seneviratne SI, Sitch S, Teuling AJ, Weri GR, Wang G (2011) Droughts and ecosystems carbon cycling. Agric For Meteo 151:765–773. doi: 10.1016/j.agrformet.2011.01.018
Muller TR (2004) HIV/AIDS and agriculture in sub-Saharan Africa. Wageningen Academic Publishers, Netherlands
Book Google Scholar
N’Tchayi MG, Bertrand JJ, Nicholson SE (1997) The diurnal and seasonal cycles of wind-borne dust over Africa north of the equator. J Appl Meteo 36:868–882. doi: 10.1175/1520-0450(1997)036<0868:TDASCO>2.0.CO;2
Neelin JD, Su H (2005) Moist teleconnection mechanisms for the tropical South American and Atlantic sector. J Clim 18:3928–3950. doi: 10.1175/JCLI3517.1
Niang AJ, Ozer A, Ozer P (2008) Fifty years of landscape evolution in Southwestern Mauritania by means of aerial photos. J Arid Environ 72:97–107
Nicholson SE (1995) Sahel, West Africa. Encycl Environ Biol 3:261–275
Nicholson SE (2001) Climate and environmental change in Africa during the last two centuries. Clim Res 14:123–144
Nicholson SE, Trucker CJ, Ba MB (1998) Desertification, drought and surface vegetation: an example from the West African Sahel. Bull Am Meteo Soc 79(5):815–829
Nyariki DM, Wiggins S (1997) Household food insecurity in sub-Saharan Africa: lessons from Kenya. Br Food J 99(7):249–262
Olsson L (1986) Report on reports-continuing the commitment: agricultural development in the Sahel. Environ 29:25–27
Olsson L (1993) On the causes of famine: drought, desertification and market failure in the Sudan. Ambio 22:395–403
Olsson L, Mryka H (2008) Greening of the Sahel. The Encyclopedia of Earth. Available from http://www.eoearth.org/article/Greening_of_the_Sahel . Accessed 23 Feb 2012
Olsson L, Eklundh L, Ardo J (2005) The recent Greening of the Sahel-trends, patterns and potential causes. J Arid Environ 63(3):556–566
Palmer WC (1965) Meteorologic drought. US Department of Commerce. Weather Bureau, Research Paper No. 45. pp 58
Peng C, Ma Z, Lei X, Zhu Q, Chen H, Wang W, Liu S, Li W, Fang X, Zhou X (2011) A drought-induced pervasive increase in tree mortality across Canada’s boreal forests. Nat Clim Chang 1:467–471. doi: 10.1038/NCLIMATE1293
Prince SD, Brown De Coulston E, Kravitz LL (1998) Evidence from rain-use efficiencies does not indicate extensive Sahelian desertification. Glob Chang Biol 4:359–374
Prospero JM, Lamb PJ (2003) African drought and dust transport to the Caribbean: climate change implications. Science 302:1024–1027
Ramanathan V, Crutzen PJ, Kiehl JT, Rosenfeld D (2001) Aerosols, climate, and the hydrological cycle. Science 294:2119–2124. doi: 10.1126/science.1064034
Reij C, Tappan G, Belemvire A (2005) Changing land management practices and vegetation on the Central Plateau of Burkina Faso (1968–2002). J Arid Environ 63:642–659
Reynolds JF, Stafford SDM, Lambin EF, Turner BL II, Mortimore M, Batterbury SP, Downing TE, Dowlatabadi H, Fernández RJ, Herrick JE, Huber-Sannwald E, Jiang H, Leemans R, Lynam T, Maestre FT, Ayarza M, Walker B (2007) Global desertification: building a science for dryland development. Science 316:847–851
Roncoli MC, Ingram KT, Kirshen PH (2002) Reading the rains: local knowledge and rainfall forecasting among farmers of Burkina Faso. Soc Nat Resour 15:411–430
Rosegrant MW, Cline SA (2003) Global food security: challenges and policies. Science 302:1917–1919
Rosenfeld D, Rudich Y, Lahav R (2001) Desert dust suppressing precipitation: a possible desertification feedback loop. PNAS 98:5975–5980. doi: 10.1073/pnas.101122798
Rotstayn LD, Lohmann U (2002) Tropical rainfall trends and the indirect aerosol affect. J Clim 14:2103–2116
Runnstrom M (2003) Rangeland development of the Mu Us Sandy Land in semiarid China: an analysis using Landsat and NOAA remote sensing data. Land Deg Deve Stud 14:189–202
Schwalm CR, Williams CA, Schaefer K, Arneth A, Bonal D, Buchmann N, Chen JQ, Law BE, Lindroth A, Luyssaert S, Reichstein M, Richardson AD (2010) Assimilation exceeds respiration sensitivity to drought: a FLUXNET synthesis. Glob Chang Biol 16(2):657–670
Seaquist JW, Olsson L, Ardo J, Eklundh L (2006) Broad-scale increase in NPP quantified for the African Sahel, 1982e1999. Inter J Remote Sens 27:5115–5122
Shanahan TM, Overpeck JT, Anchukaitis KJ, Beck JW, Cole JE, Dettman DL, Peck JA, Scholz CA, King JW (2009) Atlantic forcing of persistent drought in West Africa. Science 324:377–380
Simelton E, Fraser EDG, Termansen M, Forster PM, Dougill AJ (2009) Typologies of crop-drought vulnerability: an empirical analysis of the socioeconomic factors that influence the sensitivity and resilience to drought of three major food crops in China (1961–2001). Environ Sci Policy 12(4):438–452
Thiaw WM, Bell GD (2005) Mechanisms associated with the June–September 2003 Sahel rainfall and implications for seasonal climate forecasts. CLIVAR Exchang 10(1):29–31
Thiaw WM, Mo K (2005) Impact of sea surface temperature and soil moisture on seasonal rainfall prediction over the Sahel. J Clim 18:5330–5343
Tippett MK (2006) Filtering of GCM simulated Sahel precipitation. Geophys Res Lett 33:01804. doi: 10.1029/2005GL024923
UNAIDS (2002) Report on the global HIV/AIDS epidemic 2002. UNAIDS, Geneva
Vecchi GA, Soden BJ (2007) Global warming and the weakening of the tropical circulation. J Clim 20:4316–4340. doi: 10.1175/JCLI4258.1
Vicente-Serrano SM, Begueria S, Lopez-Moreno JI, Angulo M, El Kenawy A (2010) A new global 0.5° gridded dataset (1901-2006) of multiscalar drought index: comparison with current drought datasets based on the Palmer Drought Severity Index. Am Meteo Soc. doi: 10.1175/2010jhm1224.1
Vincke C, Diedhiou I, Grouzis M (2010) Long term dynamics and structure of woody vegetation in the Ferlo (Senegal). J Arid Environ 74:268–276
Wang B, Ding Q, Fu X, Jin K, Shukla J, Doblas-Reyes F (2005) Fundamental challenge in simulation and prediction of summer monsoon rainfall. Geophys Res Lett 32:15711. doi: 10.1029/2005GL022734
Weldeab S, Lea DW, Ralph R, Schneider RR, Andersen N (2007) 155,000 years of West African monsoon and ocean thermal evolution. Science 316(1):1303–1307
Wezel A, Lykke AM (2006) Woody vegetation change in Sahelian West Africa: evidence from local knowledge. Environ Deve Sust 8:553–567
Wolff C, Haug G, Timmermann A, Damste JSS, Brauer A, Sigman DM, Cane MA, Verschuren D (2011) Reduced interannual rainfall variability in East Africa during the last Ice Age. Science 333:742–747
Woomer PL, Tieszen LL, Tappan G, Toure A, Sall M (2004) Land use and terrestrial carbon stocks in Senegal. J Arid Environ 59:625–642. doi: 10.1016/j.jaridenv.2004.03.025
Zeng N (2003) Drought in the Sahel. Science 302:999–1000
Zeng N, Neelin JD, Lau KM, Tucker CJ (1999) Enhancement of interdecadal climate variability in the Sahel by vegetation interaction. Science 286:1537–1540
Zeppel MJB, Adams HD, Anderegg WRL (2011) Mechanistic causes of tree drought mortality: recent results, unresolved questions and future research needs. New Phytol 192(4):800–803. doi: 10.1111/j.1469-8137.2011.03960.x
Zhang R, Delworth TL (2006) Impact of Atlantic multidecadal oscillations on India/Sahel rainfall and Atlantic hurricanes. Geophys Res Lett 33:17712. doi: 10.1029/2006GL026267
Zhao L, Chen Z, Lee K (2011) Modelling the dispersion of wastewater discharges from offshore outlets review. Environ Rev 19:107–120. doi: 10.1139/A10-025
Download references
Acknowledgments
The authors wish to thank two anonymous reviewers for their valuable comments and suggestions. This study was supported by the National Science and Engineering Research Council of Canada (NSERC) Strategic Network (ForValueNet) and an NSERC discovery grant.
Author information
Authors and affiliations.
Institut des Sciences de l’Environnement, Université du Québec à Montréal, Case Postale 8888, Succ Centre-Ville, Montreal, QC, H3C 3P8, Canada
Epule Terence Epule, Changhui Peng & Laurent Lepage
Department of Building, Civil and Environmental Engineering, Concordia University, Montreal, QC, H3G 2W1, Canada
You can also search for this author in PubMed Google Scholar
Corresponding authors
Correspondence to Epule Terence Epule or Changhui Peng .
Electronic supplementary material
Below is the link to the electronic supplementary material.
Supplementary material 1 (DOCX 213 kb)
Rights and permissions.
Reprints and permissions
About this article
Epule, E.T., Peng, C., Lepage, L. et al. The causes, effects and challenges of Sahelian droughts: a critical review. Reg Environ Change 14 , 145–156 (2014). https://doi.org/10.1007/s10113-013-0473-z
Download citation
Received : 28 November 2012
Accepted : 29 April 2013
Published : 18 May 2013
Issue Date : February 2014
DOI : https://doi.org/10.1007/s10113-013-0473-z
Share this article
Anyone you share the following link with will be able to read this content:
Sorry, a shareable link is not currently available for this article.
Provided by the Springer Nature SharedIt content-sharing initiative
- Human-induced climate change
- Tree mortality
- CO 2 emissions
- Food yields
- National security
- Find a journal
- Publish with us
- Track your research
IMAGES
VIDEO
COMMENTS
Desertification in the Sahel region is a pressing environmental issue with far-reaching consequences. In this article, we will explore the causes, effects, and potential solutions to combat desertification, using a case study from the Sahel region.
This video shows the Sahel region south of the Sahara is at risk of becoming desert. Elders in a village in Burkina Faso describe how the area has changed from a fertile area to a drought-prone near-desert.
Case study - the impact of drought in a developing country: the Sahel. The Sahel is located directly south of the Sahara desert and stretches from the east to the west of Africa. The...
Two case studies are developed here: the pastoral system of the arid to semi-arid Gourma in Mali, and the mixed farming system of the semi-arid Fakara in Niger. The pastoral landscapes are resilient to droughts, except on shallow soils, and to grazing, following a non-equilibrium model.
Millions of hectares of farmland are lost to the desert each year in Africa’s Sahel region, but the UN Food and Agriculture Organization (FAO) is showing that traditional knowledge, combined with...
According to data, a prediction is that 50 million people may be displaced within the next ten years due to the desertification of the Sahel region. The communities might experience food insecurity due to reduced agricultural yields.
The Sahel desertification narrative is not recent and has evolved in time (Benjaminsen and Hiernaux 2019). Its roots lie at the beginning of the twentieth century when France, England and Portugal were establishing their colonial power throughout sub-Saharan.
We review the evidence that connects drought and desertification in the Sahel with climate change past, present and future. Advances in climate modeling point to the oceans, not land, as the cause of the recent persistence of drought in the Sahel.
This paper is a critical synthesis of the causes, effects and challenges of the Sahelian droughts. The results show that the four main causes of the Saheli.
Two case studies are developed here: the pastoral system of the arid to semi-arid Gourma in Mali, and the mixed farming system of the semi-arid Fakara in Niger. The pastoral landscapes are...