Desertification is a growing problem in our world, due to a mix of climate change and poor land management. In this article we will define desertification, its causes, its impacts, and what can be done to stop it.
What is desertification?
The definition of desertification is when fertile land in arid conditions becomes drier, transitioning to a desert environment.
For such a transition to be considered desertification, the land must:
Undergo land degradation – land’s loss of current or future productive capabilities.
Be dryland – land in an arid, semi-arid, or dry sub-humid climate.
Desertification is a global problem - 17 countries, which are home to nearly 2 billion people, have highly stressed aquifers. That means water, food, and land for a quarter of the world’s population is at serious risk.
On the continental U.S., desertification is a threat to approximately 40% of the land, with 17 states being considered dryland.
If desertification and climate change are not taken seriously, it is likely that millions of people will choose to leave their homes for areas with more consistent access to food and water.
What are the causes of desertification?
Desertification is caused by a multitude factors that often compound each other. Variations in the climate play a part in the phenomenon, as do human activities.
Urbanization and improper agriculture and land management practices drive factors that cause desertification, including:
Deforestation
Forest fires
Pesticide use
Excessive irrigation
Overgrazing
Drylands, by definition, get little rain. Therefore, the groundwater supply of drylands is typically a fragile resource. As droughts intensify, lengthen, and become more common with climate change, the aquifers holding the groundwater will shrink year by year, even when they are refilled by rains.
Climate change intensifying droughts
Since the early 1900s, global drought has been steadily increasing due to greenhouse gas emissions by humans.
The addition of more greenhouse gases to our atmosphere has been steadily warming our planet and contributing to climate change. Warmer temperatures make more water evaporate from earth’s surface. This means plants have a harder time holding on to moisture and staying hydrated in arid areas.
Climate change has also been making weather and climate patterns more extreme – wetter areas have been getting wetter, and drier areas have been getting drier. That means that in drylands, droughts have been longer and more severe, rainy periods have been more intense, and highs and lows of temperature have been more extreme. All of this contributes to a harsher world for life to survive in.
When drought-affected areas are well managed, the land can rebound when rain inevitably comes.
But drylands that are poorly managed during drought have a much harder time recovering to pre drought stability. Heavy use of groundwater for irrigation, drinking water, putting out forest fires, or urbanization needs can limit the water available for plants to rely on during drought.
Two other big factors of poor land management are overgrazing of cattle and excessive use of pesticides. These common practices contribute to desertification by deteriorating soil health and texture.
Overpopulation can also lead to improper land management. It creates greater demands on the soil for food than it can sustainably give. Overuse can easily trigger erosion of quality soil, which will put more stress on nearby land to compensate for this loss.
Desertification, impacts
One of the main impacts of desertification is biodiversity loss. As dry land ecosystems get drier and more inhospitable, fewer plants and animals can adapt and survive.
Biodiversity loss has adverse effects beyond the loss of each individual species – the ecosystem as a whole becomes more fragile. Fewer species will exist to fill niches. So if disease or any other disaster strikes the only species filling a niche, the ecosystem could crumble.
Forest fires and low soil quality, as we have discussed, are also common consequences of desertification. An area becoming more arid makes it more fire friendly. And as soil deteriorates with erosion, it cannot hold as much moisture, further adding to forest fire potential.
Habitat loss is inevitable when an ecosystem is ravaged by forest fires, depleting soil, increased temperatures and more sparce precipitation. Animals and plants are forced to migrate but finding new homes can be challenging – it depends on environmental conditions and competition for resources.
Impact on humans
Of course, land becoming desert makes the area less hospitable to humans as well.
The productivity of crops and livestock tends to go down due to desertification. Wildfires are more likely to spark as drylands become drier, threatening humans themselves, their crops, and their livestock.
When the rare rains eventually do come, poor soil conditions can lead to flooding and polluted water sources, compounding water stress on communities.
You may be wondering where desertification is happening or where it is likely to occur.
As we know, desertification happens only in areas that are already particularly dry. While not all drylands are near a desert, desertification is most likely to happen on the shoulder of the desert – where precipitation is as or more sparce than on the dryland itself.
Desertification is creeping its way across California
The Golden State, as an agricultural capital of the U.S., is particularly thirsty for water. Unfortunately, a good chunk of California has experienced drought for much of the last decade.
It’s fair to say that during this period, the land has not been managed very well - parts of the state’s central valley have sunk as much as two feet each year due to excessive groundwater use.
If California were to eventually run out of groundwater, it would be a death sentence to farming and fertile soils across the state. That is why California passed a law in 2014 to try to balance defending its aquifers from overuse with prioritizing agriculture.
Africa
Two thirds of the continent of Africa is currently classified as either dryland or desert. That was not always the case – but with desertification increasing, transitionary land between desert and non-desert has become less and less habitable.
For example, the Sahel, a long band of dryland separating the Sahara Desert from the humid savannas to the South, becomes more barren each year. Desertification happens there partly due to growing populations’ greater demands on the land for sustenance. Also, the cattle commonly overeat the limited supply of grass, leaving the soil exposed to erosion when rainfall comes.
Another way to limit desertification is by protecting windy areas. We can do this by building a wind fence or planting an ecological border, which will be key to limiting soil erosion.
Of course, lowering our greenhouse gas emissions in order to stop climate change and limit drought intensity is another important angle to tackling desertification. We can limit the harshest impacts, worst case scenarios, and spread of desertification if we work together to stop global warming.
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