The persistent degradation of dryland ecosystems, arid, semi-arid and dry sub-humid areas, by human activities + climate change, resulting in desert like conditions
Desertification
It is an example of positive feedback
Leaves land unproductive
Regions worst affected by desertification
Africa
Asia
Latin America
1/3 of land worldwide is at risk from desertification
250 million people are already affected by desertification
46% of Africa is at risk of desertification
25% of Africa is already desertified according to the UN
12 million hectares of land lost to desertification annually according to the UN
Desertification reduces the wellbeing of at least 1 billion people in 100 countries
Hot deserts
Since the last glacial period ended 11,500 years ago, the climate became more wet, reducing the amount of land covered by deserts
Hot deserts
9,000 years ago, only deserts were on the west coast of South America and South Africa
The extent of deserts have increased over the past few thousand years
Late Holocene (approximately 4,000 years ago to present)
Desert landscapes have continued to evolve in response to climate fluctuations, human activities, and other factors
Some regions have experienced desertification due to factors such as deforestation, overgrazing, soil erosion, and changes in land use practices
Human civilization has also influenced desert distribution through activities such as irrigation, agriculture, urbanization, and infrastructure development
The Sahara desert
5,000-9,000 years ago, it was a 'green Sahara' with lakes, vegetation, and animals like antelope, giraffes, and cattle
Ancient cypress trees up to 2,000/3,000 years old survived due to long taproots and the water table
The Sahara's precipitation decreased as the belt of rains moved northwards across Europe
Most deserts were formed during the last glacial period, around 6,000-4,000 years ago
Climate change as a physical cause of desertification
Less and more unpredictable rainfall, especially in the Sahel region
Reduced water supply as rivers dry up and water tables are lowered
Increased evapotranspiration and vegetation loss due to higher temperatures
Human activities increasing the rate of desertification/land degradation
Population growth and increased pressure on the land
Over-cultivation reducing soil productivity and fertility
Deforestation for agriculture, fuel, and building materials
Over-grazing leading to soil depletion and erosion
Unsustainable irrigation practices depleting surface water and groundwater, and causing salinization
Irrigation can cause desertification
River channels can be diverted to irrigate crops, depleting water sources like the Aral Sea
Irrigation depletes surface water and/or fossil aquifer systems, lowering water levels and availability
The Nubian Sandstone Aquifer System in North Africa is the world's largest known fossil water aquifer system, spanning four countries, and is an important but contested water source
Impacts of desertification on ecosystems, landscapes, and populations
Loss of topsoil through exposure to wind and rain
Over-exploitation of biodiversity through agricultural practices
Vegetation destruction leading to animal migration
Water source depletion and increased soil salinity
Landscape changes like reduced sand dune formation, increased erosion, and soil/sand encroachment
Dust clouds affecting air quality and health
Reduction in clean water supplies and increased water-borne diseases
Forced migration and disputes over land
Food shortages leading to malnutrition and famine
Reduced farm income and agricultural productivity, leading to poverty and increased reliance on aid
Climate change and desertification
Temperatures in drylands could rise by 2-5°C by 2050, accelerating desertification
Precipitation rates will decrease, moving semi-arid areas into arid regions
Extreme weather events are likely to become more frequent
Increased migration to overcrowded cities
Less productive soils will force more people to migrate, adding pressure on other countries