3.1.2.4 desertification

Cards (21)

  • Desertification
    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