— Ch. 1 · Defining The Process —
Desertification.
~5 min read · Ch. 1 of 6
The United Nations Convention to Combat Desertification published a definition in 1995 that described desertification as land degradation in arid, semi-arid and dry sub-humid regions. This text emerged from decades of scientific debate regarding the exact nature of soil loss. Before this agreement existed, more than one hundred formal definitions competed for acceptance among researchers. Princeton University Dictionary offered a widely accepted view in 2005 describing it as fertile land transforming into desert due to deforestation or drought. That original understanding suggested physical deserts were expanding outward like spreading ink. Modern science has since rejected the idea that deserts simply grow larger on their own. Natural processes create deserts over geological time scales spanning thousands of years. Human activities now accelerate these changes through specific actions like tillage and overgrazing. The immediate cause remains the loss of vegetation cover which exposes soil to wind and water erosion.
Drivers And Mechanisms
Studies show that erosion rates decrease exponentially when vegetation cover increases within an environment. Unprotected dry soil surfaces blow away with the wind during storms or wash away during flash floods. These events leave infertile lower layers that bake under the sun and become unproductive hardpan. Early research identified overgrazing by cattle as one of the most common causes of land degradation. Recent analysis suggests drought in the Sahel region results primarily from seasonal rainfall variability driven by sea surface temperature variations. Anthropogenic emissions of aerosols and greenhouse gases also contribute significantly to changing ocean temperatures. Farmers often use intensive farming methods to maximize yields but this depletes soil nutrients rapidly. Continuous use of fertilizers and pesticides further damages the biological composition of the earth. In the Mu Us Desert, soil health accounts for 37% of desertification events while meteorological factors counteract it by 46%. Inner Mongolia shows a different pattern where meteorological contributions make up 24% and soil benefits account for 34.7%.