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INTRODUCTION

BIOSPHERES

CATCHMENTS

CONSERVATION

GEOLOGY

LAND COVER

LAND USE

MORPHOLOGY

OTHER DATA

RAINFALL

RAMSAR

RUNOFF

SENSITIVITY

SHAPE

SOILS

VELD TYPES

 

 

RAINFALL

 

Only about 7% of South Africa has a mean annual precipitation or MAP exceeding 800 mm. When the statistics are reviewed they indicate that KwaZulu-Natal is the wettest province, while the Western Cape has the highest variability of MAP within any of the provinces, and the highest individual point rainfall at an estimate of 3345 mm per annum is located along the southern mountain ranges of the province.

The eastern provinces, KwaZulu-Natal, Eastern Cape to a lesser degree, Mpumalanga, Gauteng and to an extent, Northern Province, receive more rain than the provinces in the west (such as the North West Province, Northern Cape, or the Free State). The Northern Cape receives the lowest mean annual precipitation with Western Cape the second lowest.

 

PROVINCE / COUNTRY

MEAN ANNUAL RAINFALL(mm)

Northern Cape

202

Western Cape

348

North West

481

Northern Province

527

Free State

532

Eastern Cape

552

Gauteng

668

Mpumalanga

736

KwaZulu-Natal

845

Lesotho

701

Swaziland

860

Choose a province to view map or click on province in image

Eastern Cape
Free State
Gauteng
KwaZulu-Natal
Mpumalanga
Northern Cape
Northern Province
North West
Western Cape Northern Province Mpumalanga North West Gauteng KwaZulu Natal Free State Northern Cape Western Cape Eastern Cape

 

Drylands and desertification

Nearly 91% of South Africa falls within the United Nations' definition of affected drylands. These are extraordinarily dry areas where the rainfall is low, and the potential evaporation is high. Dryland systems are often very sensitive to change and therefore need to be managed carefully. For example, crops grown in these areas are usually not irrigated, and therefore depend on rainfall. Drought-induced crop failure can result in direct food shortages at a local level, usually affecting subsistence agriculturists the hardest. Removal of vegetation (ground cover) from dryland areas can increase the risk of soil erosion, making the soil less fertile, and less able to support (natural and cultivated) crops in future.

Desertification refers to the degradation of land in the dry areas of the world, primarily caused by human activities. Desertification is not the spread of existing deserts. It is the destruction of productive land in dry areas mainly as a result of misuse or overuse. Desertification affects 900 million people in 99 countries, by destroying the capacity of the soil to support livestock or crops. According to a recent national survey, land in nearly 25% of the magisterial districts of South Africa has already been badly degraded.