9 MAIN CHARACTERISTICS OF DESERTIFICATION

9 MAIN CHARACTERISTICS OF DESERTIFICATION




Desertification refers to the development of desert-like conditions in an area and more so in a region adjacent to a desert.

desertification may be expressed as the advancement or extension of the desert.

Desertification refers to the development of desert-like conditions in an area and more so in a region adjacent to a desert. It may be expressed as the advancement or extension of the desert. Desertification has been commonly experienced in the Sahel region of Africa. In East Africa desert-like conditions have been experienced or developed in parts of Northern Kenya, Central and Northern Tanzania, N. Eastern Uganda, and the Ankole-Masaka corridor and parts of Western Uganda adjacent to Lake Albert, Lake George, Albert Nile, and within the East African rift valley.

Desertification has been commonly experienced in the Sahel region of Africa.




it is the term used to describe how once productive land gradually changes into a desert-like landscape.

the process is not necessarily irreversible and is usually taking place in semi-arid land on the edge of the existing hot desert.

the worrying message is that large areas of the world are at risk from desertification.

the most conspicuous includes much of southern Asia, the middle east and north Africa




In East Africa desert-like conditions have been experienced or developed in parts of Northern Kenya, Central and Northern Tanzania, N. Eastern Uganda, and the Ankole-Masaka corridor and parts of Western Uganda adjacent to Lake Albert, Lake George, Albert Nile, and within the East African rift valley.

9 Indicators of desertification 

Decreasing rainfall amounts

one of the key indicators of desertification is the decrease of the amount of rainfall year after year. many areas which experience desertification today were once getting enough rainfall but due to deforestation and overgrazing which causes desertification these areas are now experiencing a small amount of rainfall




Rainfall becomes more unreliable

that is more recurring cycles of drought start being experienced.

Increasing temperatures

due to deforestation and loss of vegetation, the temperature tends to increase over time

Reducing relative humidity

due to loss of vegetation which is important in maintaining humidity in the atmosphere desertification lead to a decrease in the humidity in the atmosphere




indicators of desertification
Decreasing rainfall amounts.
Rainfall becomes more unreliable i.e. more recurring cycles of drought start being experienced.
Increasing temperatures i.e. temperatures tend to rise.
Reducing relative humidity i.e. the amount of water vapour in the atmosphere reduces.

Increasing diurnal range of temperature.

Reducing the thickness of cloud cover

that is the skies tend to become clearer and clearer with each passing year.

loss of water soil and vegetation water retention capacity

There is loss of water retention capacity of the vegetation and soils i.e. there are increasing evapotranspiration rates

 Reduced biodiversity

that is there is the degradation of the biological productivity of the land i.e. reduced plant and animal species.




Increasing wind and run off erosion

hence consequently resulting in reduced soil fertility.

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mwaikusa

IAM experienced geography teacher with more than three years of teaching and creating content related to geography and other subjects for both high school and college students. hope you will find the content of this website useful to your studies and daily life

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