|
Agroecosystem Topics Page |
Agroecosystems Home Page
| Site Contents
Desertification
Photo taken in Burkina Faso during the dry season shows free-roaming
cattle, evergreen trees, and millet residues. Cattle graze on
seedlings, reducing shrub and tree cover. In turn there is less
fodder during the dry season, and more runoff and erosion when
it rains. |
|
Prepared by Kate Hopfner
(1998 class)
CONTENTS
Agroecosystems Home Page
Overview
Desertification is a serious problem in the Sahel Region of Africa. However, pinpointing the precise cause of desertification
is impossible at this time. The cause of desertification was once
thought to be simply lack of rainfall, however extensive research
has shown it may be much more complex (* DESERTIFICATION AND CLIMATE
CHANGE). As the phenomenon of desertification was further studied,
more theories as to its cause emerged, many claiming unsuitable
agricultural practices in the affected areas as the cause. This
agricultural mismanagement usually centered around three separate
factors as the cause of desertification whether alone or combined
*(PRECIOUS EARTH) These are:
- overgrazing by livestock
- slashing and burning of forests to clear land for agriculture
- separation of perennials from annual crops.
The intercropping of perennials with annual food crops reduces
erosion, and shelters annuals from extremes of climate. The removal
of perennials leaves annual crops vulnerable.
More recent literature, however. suggests that desertification
is not the result of local agricultural mismanagement, but is
a natural phenomenon (Mearns, 1997). Some global processes have
also been connected to desertification in the Sahel region and
elsewhere, including climate change and changes in oceanic circulation.
(*DESERTIFICATION AND CLIMATE CHANGE). Regardless of the precise
cause of desertification, it is obvious that the effects are very
detrimental to local populations of both humans and wildlife.
The effects of desertification can be widely seen in the Sahel.
Desertification also has global significance. On a regional scale,
desertification threatens local residents by land degradation, reducing the productivity of the land (*DESERTIFICATION - A
THREAT TO THE SAHEL). Land degradation occurs by way of erosion and salinization (*IMAGES OF THE CHANGING SAHEL). This causes strain on residents
as poor harvests cause hunger, and residents are often forced
to move on to new land. The new land often has to be "created"
by the destruction of preexisting vegetation, increasing the area
of land which is of poor quality. Regionally and globally, desertification
can cause extinctions of indigenous plant and animal species (*IMAGES
OF THE CHANGING SAHEL). The links between desertification and
climate change have also been extensively researched; climate
change can be seen in some cases as a cause of desertification
and in other cases, an effect of desertification (Williams et
al., 1996).
Solutions to desertification in the Sahel region are neither simple
nor quickly implemented. This is apparent when one recognizes
that the actual cause of desertification is not clear. Regardless,
local farming practices can accentuate desertification in the
Sahel (*DESERTIFICATION - A THREAT TO THE SAHEL). Unfortunately,
to change local farming practices is not a simple matter because
there is a tangled web of historical, economic and social factors
contributing to desertification in the Sahel (Dregne, 1995). Many
countries affected by desertification are developing countries
and are the countries which can least afford to implement solutions,
especially large-scale ones. Small-scale, local solutions are
necessary to change local farming practices. NGOs therefore play a key role, and one we need to support as regional
improvements would affect the entire world for the better.
Contents
Key Facts and Figures on Desertification
DESERTIFICATION: Land area affected globally
From: *PRECIOUS EARTH - CHAPTER 1.2.
(See Key Facts and Figures for global land area in agriculture).
Land Type |
Moderate Desertification
(million ha) |
Severe Desertification
(million ha) |
Rangelands |
3,100 |
1,300 |
Rainfed Cropland |
335 |
170 |
Irrigated Land |
40 |
13 |
Other Key Facts and Figures About Desertification:
- Nine-hundred million people in about 100 countries are at risk
from desertification (CIDA, 1997).
- The countries most affected by desertification are often, economically,
the least equipped to solve the problems associated with it (CIDA,
1997).
- Desertification is occurring in 70% of all drylands, and affects
25% of the total land area of the globe (*BASIC FACTS ON DESERTIFICATION).
- Desertification has degraded 73% of the world's rangeland (*BASIC
FACTS ON DESERTIFICATION).
Contents
Important Terms
- Annual Crops
- Crops which grow from a seed to maturity, then die within one
year.
- Desertification
- "degradation of land resources in arid, semiarid and dry sub-humid
areas resulting from various factors including climatic variations
and human activities" (as defined at the United Nations Conference
on Environment and Development, 1992)
- Erosion
- The process by which land is worn away by action of water, wind
waves and other forces.
- Land Degradation
- Loss of soil, water and biodiversity on land.
(*IMAGES OF THE CHANGING SAHEL)
- NGOs
- Non-governmental organizations (examples range from well-known
global organizations like Greenpeace and Red Cross, to local community
organizations)
- Perennials
- A plant which has a life cycle which lasts more than two years.
- Sahel Region
- Area just south of the Sahara Desert in northwestern Africa which
serves as a transition zone between the desert and wetter lands
to the south
(*BRIGHT EDGES OF THE EARTH)
- Salinization
- This refers to accumulation of salts in arid
region soils to the point that crop growth is significantly impaired. It
is commonly associated with irrigation of arid region soils - salts tend
to accumulate because evaporation removes water, leaving the salts
behind. If the drainage system is not designed properly or if there is
not a season of excess precipitation, or annual floods to wash the salts
away away, soils become progressively more salty
Contents
Useful Literature
- Canadian International Development Agency. 1997. Desertification: Meeting the Challange. Ministry of Public Works and Government Services
Canada. Hull, Canada.
- Ludwig, J. , D. Tongway, D. Freudenberger, J. Noble amd K. Hodgkinson.
1997. Landscape Ecology. Function and Management. CSIRO Australia. Dal Lib. QH 541.5 R3 L35.
This
book develops a landscape approach to managing rangelands, based on
principles of landscape ecology, and experience derived from Australian
rangelands.
- Mearns, R. 1997. Livestock and environment: potential for complementarity. World Animal Review :
88: 2-14.
- Williams, M. and R. C. Balling Jr. 1996. Interactions of Desertification and Climate. Arnold Publishing, London.
Contents
Useful Links
Contents
Cited Literature and Links
- BASIC FACTS ON DESERTIFICATION
(http://rolac.unep.mx/deselac/esp/) United
Nations Environment Program, Spons. (Viewed 6 Feb. 2001) Note: Spanish
Site
- BRIGHT EDGES OF THE WORLD
(http://drylands.nasm.edu:1995) United Nations
Environment Program and Smithsonian Institution, Spons. (Viewed 6 Feb. 2001)
- CIDA. 1997. Desertification: Meeting the Challange. Ministry of Public Works and Government Services Canada. Hull,
Canada. Dal. Lib. GB 612 D47 1997
-
DESERTIFICATION - A THREAT TO THE SAHEL
(http://www.eden-foundation.org/project/desertif.html)
Eden Foundation, Spons. (2000, February 3; Viewed 6 Feb.
2001)
- DESERTIFICATION AND CLIMATE CHANGE ( Tiempo Issue 9)
(http://www.cru.uea.ac.uk/tiempo/floor0/archive/issue09/t9art1.html)
Mick Kelly and Mike Hulme, Auth. (1993, August; Viewed 6 Feb.
2001)
- Dregne, H.E. 1995. Desertification control: a framework for action. Environmental
Monitor Assessment 37: 111-121.
- Mearns, R. 1997. Livestock and environment: potential for complementarity. World Animal Review 88: 2-14.
- PRECIOUS EARTH - CHAPTER 1.2
(http://www.giub.unibe.ch/cde/isco/isco12.html)
Department of Geography, University of Berne, Switzerland, Spons. (1995, December; Viewed 6 Feb.
2001)
- Williams, M. and R. C. Balling Jr. 1996. Interactions of Desertification and Climate. Arnold Publishings. London. Dal.
Lib. GB612 W55 1996
Contents |
|