Desertification (DP IB Geography)
Revision Note
Causes of Desertification
Desertification is:
The process of desert-like conditions spreading into what were previously semi-arid areas, as the quality of soil and its fertility decline over time
It is possible to argue that human activity and climate change may make many of the natural causes worse
Comparison Between Natural and Human Causes
Natural causes | Human causes |
---|---|
Soil erosion leads to the loss of nutrients. Plants are unable to establish and grow | Overgrazing means the vegetation has all gone due to the numbers of animals or the land does not have chance to recover |
Rainfall patterns have become less predictable, leading to drought and any vegetation dying due to lack of water | Over-cultivation leads to all the nutrients being taken up by crops, leaving none for future vegetation to grow |
Reduced vegetation means that nutrients are not added to the soil through the decomposition of dead organic matter | Deforestation removes shade for the soil and means there are no roots which bind the soil together. This increases soil erosion, whilst decreasing infiltration and interception |
Any rain that does fall is often in short, intense bursts, leading to increased surface run off and soil erosion | Population growth puts increased pressure on the land as people raise more animals and grow more crops |
In areas such as Kenya, both human and natural factors lead to desertification
Grazing patterns and traditional lifestyles mean that:
Nomadic Masai farmers have been forced to use smaller and smaller areas of land for grazing
This results in overgrazing, which removes the vegetation
The soil no longer has protection from the wind and rain, which leads to soil erosion and desertification
Population growth increases the demand for food and fuelwood
This leads to over-cultivation and deforestation
Deforestation:
Reduces the amount of nutrients returned to the soil
Exposes the soil to wind and rain
This further increases soil erosion, leading to desertification
In Kenya increasing temperatures and more irregular rainfall are natural causes of desertification
However, these could be the result of the enhanced greenhouse effect (human cause) leading to climate change
Consequences of Desertification
Desertification is a form of land degradation
Land degradation indirectly affects about 350 million people in the developing world
Land degradation occurs through changes in soil character, wind erosion, or water shortages (droughts), which leaves the land unproductive or lost
Soils in arid and semi-arid regions are potentially very fertile, as there is insufficient water to leach minerals from the soil
These soils have high pH values and intense evaporation at the surface results in the capillary rise of soil moisture and minerals; this is salinisation
When irrigation water is added to land and allowed to evaporate, this has the effect of increasing salinisation
This process has made a lot of land in the hot deserts infertile
Increased soil salinity restricts most plant growth and is also phytotoxic when there are high concentrations of sodium in the soil
Soil erosion is the washing away or blowing away of topsoil, which greatly reduces the fertility of the remaining soil
This is a natural process made worse through human activity
There is a link between soil erosion and desertification
Once desertification starts, a pattern follows in a downward spiral that not only affects the physical but also the human aspect
Soil degradation → soil erosion → reduced agricultural output → malnutrition, famine → migration → conflict → soil degradation etc.
The consequences of desertification include:
Loss of topsoil through exposure to wind and rain
Over-exploitation of biodiversity through agricultural practices
Vegetation is destroyed, leading to the migration of animals (and people)
Water sources are depleted through over-abstraction and/or lack of precipitation, and biodiversity is lost
Increased levels of soil salinity through poor irrigation practices
Desertification changes the landscape:
Reduced sand dune formation as less vegetation to trap loose material
Landslides on destabilised slopes where vegetation is removed
Vegetation slows wind speeds - as vegetation reduces, wind speeds increase leading to more frequent sandstorms
Soil moisture evaporation increases; the soil dries quickly
Plant root mat is lost; soil becomes unstable
Increased erosion eventually exposes bedrock
A combination of higher wind speeds and mobile sediment, transports sand, etc. into other areas, burying vegetation and soil
Soil and sand encroachment impacts the ecosystem:
Land becomes less fertile, impacting flora and fauna as less organic matter is returned to the soil, further reducing growth and biodiversity decreases
Distribution of species has/is changing - flora and fauna populations that were present before desertification have either died out or migrated to less degraded areas
The process of species adaptation is slow, and inward-moving, already adapted species outcompete native species
Desertification destroys soil and vegetation carbon sinks, releasing it back into the atmosphere, enhancing global warming and further changes in climate conditions
Impacts on People in the Desert
Changes to hot desert ecosystems and landscapes have a knock-on effect on human populations
Social impacts
Dust clouds (from soil erosion) affect air quality and health
Reduction in clean water supplies creates hygiene issues and increases water-borne diseases
People are forced to migrate, with many people—young men in particular—leaving to work in cities and towns
This adds pressure on already limited urban resources
Disputes occur over land between herdsmen and farmers
Food shortages lead to malnutrition and famine, e.g. in Ethiopia
This can also result in increased movement to refugee camps, e.g. Syria to Jordan
Economic impacts
As the land becomes unproductive, farm income falls
This leads to widespread poverty and an increased reliance on overseas aid
Desertification also reduces vegetative productivity, leading to long-term declines in agricultural yields, livestock yields, plant standing biomass, and plant biodiversity
Reduced agricultural exports, increased dependency on government grants
People and communities suffer the loss of income, further reducing the ability to produce food, which affects the economy of the country
Climate change and desertification
By 2050, temperatures in the world’s drylands could rise by 2 to 5°C, accelerating and increasing desertification impacts
Precipitation rates will decrease; moving semi-arid areas into arid regions
Extreme weather events are likely to become more frequent
Increased migration to already overcrowded cities
Less productive soils will lead to rural areas becoming less viable, forcing more people to migrate further afield, This adds pressure on other countries to provide food, water and shelter when they themselves may be struggling
Some may stay and adapt by using soil conservation strategies or changing agricultural practices
Management of Desertification
Desertification is a very difficult process to reverse while rainfall remains low
Halting and reversing desertification means tackling the causes
There are a variety of possible methods that can be used
Water management
Contour stones or bunds can be used to increase infiltration
Earth dams can be used in the wet season to store water
Drip irrigation can be used to water crops more efficiently
Education
Education including:
Sustainable farming methods, including agroforestry and crop rotation, which help to keep the soil healthy
Family planning to reduce population growth
Agroforestry
This combines agriculture with forestry, which means some trees remain, which:
Decreases deforestation
Provides shade as well as increasing infiltration and interception, which reduces soil erosion
Provides organic matter from the trees and adds nutrients to the soil
Afforestation
Tree planting, such as the Great Green Wall across the Sahel, helps to reverse desertification in several ways:
The roots help to bind the soil together, reducing soil erosion
The canopy offers shade, helping to prevent the soil from drying out and also reducing soil erosion from rainfall landing directly on the soil
Falling leaves and branches replace nutrients in the soil
The trees increase animal and insect activity, which helps improve soil quality
Contour stones or bunds
These help to reduce soil erosion by:
Preventing the soil from being blown or washed away
Reduce overland flow
Ensuring that dead organic matter stays in one place and can decompose, adding nutrients to the soil
Additionally, they increase infiltration of water into the soil
Alternatives futures
The future for those living in areas of desertification depends on the action taken to mitigate and ameliorate land degradation
No one plan or action can solve the issue of desertification and this means there are two possible outcomes:
Desertification continues (business as usual)
Human intervention stops or reverses desertification
Table Showing Possible Futures
Desertification Continues | Intervention |
---|---|
If no action is taken or strategies are not appropriate or insufficient, then the rate of desertification may increase, leading to larger areas of degraded land | Appropriate and sufficient action taken may reduce or reverse desertification and areas could return to previous conditions |
Reduction in agricultural output increases malnutrition and famine and this lack of food security hinders the development | Improved farming techniques and education reduce the impact of wind erosion, improve soil fertility and reduce the effect of land degradation |
Migration can lead to overcrowding in receiving areas, which can lead to sanitation and health issues, along with increased pressure to find housing, jobs and food can lead to conflict within and between countries | Global responses to climate change could have a major impact, but requires commitment on a global scale and not every country agrees with cutting emissions of greenhouse gases |
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