Deserts And Desertification The Causes And Consequences

8,932 views

Published on

Poverty eradication & sustainability
CAUSES AND CONSEQUENES

United Nations Convention to Combat Desertification Global warming and climate change have led to desertification, drying of water sources and change of climatic patterns, thus leading to scarcity of food production as a result of diminishing arable land and long periods of drought

Published in: Career, Technology
3 Comments
0 Likes
Statistics
Notes
  • Be the first to like this

No Downloads
Views
Total views
8,932
On SlideShare
0
From Embeds
0
Number of Embeds
28
Actions
Shares
0
Downloads
200
Comments
3
Likes
0
Embeds 0
No embeds

No notes for slide

Deserts And Desertification The Causes And Consequences

  1. 1. Desertification comes about by a complex interaction between the natural environment and human activities. The cause may vary from region to region on account of economic conditions, population pressure, agricultural practices, and politics. Human activities that destroys surface vegetation, degrades soil structure and fertility, impedes water infiltration, and causes soil drying promotes desertification. This is especially true for the fragile transition zone between arid and semiarid land where human activity has stretched the ecosystem to its limit causing expansion of deserts. Desertification is a global problem occurring in many places but is prevalent along the margins of semiarid and arid lands in Asia, central Australia, portions of North and South America, and Africa. A world map prepared by the United States NRCS shows just how widespread the problem is. PHENOMENON OF DESERTIFICATION United Nations Convention to Combat Desertification
  2. 2. Desertification Desertification is the expansion of dry lands due to poor agricultural practices (e.g. overgrazing, degradation of soil fertility and structure), improper soil moisture management, salinization and erosion, forest removal, and climate change. Desertification in Africa Two common misconceptions prevail about desertification, that it spreads from a desert core and drought is responsible. Desertification spreads outward from any where excessive abuse of the land occurs and far from any climatic desert. Droughts do increase the possibility of desertification if the carrying capacity of non-irrigated land is exceeded. Well-managed land can recover from the effects of drought. Combining drought with land abuse sets the stage for desertification. United Nations Convention to Combat Desertification
  3. 3. Cause of Desertification Desertification comes about by a complex interaction between the natural environment and human activities. The cause may vary from region to region on account of economic conditions, population pressure, agricultural practices, and politics. Human activities that destroys surface vegetation, degrades soil structure and fertility, impedes water infiltration, and causes soil drying promotes desertification. This is especially true for the fragile transition zone between arid and semiarid land where human activity has stretched the ecosystem to its limit causing expansion of deserts. Population growth and its demand on agricultural resources has promoted the desertification process. Over cultivation, for example, causes declining soil fertility leading to falling crop yields. Over use leads to crusting of exposed topsoil by rain and sun that increases runoff, water erosion and gullying. Soil drying promotes wind erosion and encroachment of sand dunes on arable land. United Nations Convention to Combat Desertification
  4. 4. <ul><li>Overgrazing has several effects. It: </li></ul><ul><li>Causes a decline in pasture vegetation and palatable grass species. </li></ul><ul><li>Replaces perennials with short-lived annual species that do not hold soil against erosion. </li></ul><ul><li>Compacts soil under trampling hoofs. </li></ul><ul><li>Destabilizes dunes when crest vegetation is eaten. </li></ul><ul><li>Forest cutting for fuel wood has deforested large tracks of land in Africa and Asia encouraging desertification. </li></ul><ul><li>Desertification around the world </li></ul><ul><li>The United Nations Conference on Desertification ranks desertification hazard on the basis of a drop in agricultural productivity: </li></ul><ul><li>None - less than 10% </li></ul><ul><li>Moderate - 10% to 25 % </li></ul><ul><li>High - 25% to 50% </li></ul><ul><li>Very high - more than 50% </li></ul><ul><li>Desertification is a global problem occurring in many places but is prevalent along the margins of semiarid and arid lands in Asia, central Australia, portions of North and South America, and Africa. </li></ul><ul><li>A world map prepared by the United States NRCS shows just how widespread the problem is. </li></ul>United Nations Convention to Combat Desertification
  5. 5. DESERT AND DESERTIFICATION CHALLENGE AND OPPORTUNUITIES Africa has been significantly impacted by desertification. Almost three quarters of Africa's agricultural drylands are already degraded to some degree. The impact on desertification on the greatest number of people occurs in Asia. Degraded regions include the sand dunes of Syria, the eroded mountain slopes of Nepal, and the deforested and overgrazed highlands of Laos. The Northern Mediterranean region is the cradle of civilization and has borne the effects of poor agricultural practices. Salinized, infertile soils are the result of natural hazards e.g. droughts, floods and forest fire, as well as overtilling and overgrazing. Soil degradation is high through much of Central and Eastern Europe, and very high in some areas, for example along the coast of the Adriatic Sea. Poor irrigation practices and the unsustainable exploitation of water resources are contributing to chemical pollution, soil salinization and aquifer depletion. Nearly a quarter of the inhabitants of Latin America and the Caribbean live below the poverty line fueling practices that lead to land degradation. Erosion and water shortages are intensifying in many East Caribbean islands. United Nations Convention to Combat Desertification

×