Background Image
Previous Page  136 / 148 Next Page
Information
Show Menu
Previous Page 136 / 148 Next Page
Page Background

122

Conclusions and Recommendations

• The population in the Zambezi River Basin

is increasing, and is expected to reach

51 million by 2025.

• Some 7.5 million people live in urban centres

in the Zambezi basin. There has been rapid

expansion of Lilongwe and Harare between

1990 and 2011.

• There are some 30 ethnic groups and related

cultures in the Zambezi River Basin. The

cultures in the Zambezi basin include the

Lunda, Luchaze and Quioca in Angola; the

Tswana in Chobe, Botswana; the Chewa,

Tumbuka, Yao, Ngoni, Nyanja and Sena

cultures in Malawi; the Sena in Mozambique;

the Bemba, Tonga, Lozi, Luyana, Lunda, Bunda

and Chewa/Nyanja in Zambia; and Shona,

Ndebele and Tonga cultures in Zimbabwe, as

well as Nambya in Zimbabwe and Namibia.

• Land available per capita is projected to

shrink from 4.16 ha/person in 1998 to

2.72 ha/person by 2025.

• The Basin is endowed with numerous natural

resources including lakes, wetlands, forests

and wildlife, as well as land and minerals.

• The Basin is highly prone to overexploitation

and unsustainable development.

• Climate change coupled with human pressure

on resources is resulting in significant change

of the Zambezi basin’s environment.

• The location, extent and significance of

adverse impacts occurring through changes

in land use are closely related to human

population pressure on the land.

• Seventy-five per cent of the land area in the

Basin is forest and bush while13 per cent

of the land area is cropland, mostly rain

fed. Zimbabwe, Zambia and Malawi have

together 86 per cent of the estimated

5.2 million ha of the cultivated area in the basin.

• Use of fertilizers and agro-chemicals in the

basin is contributing to the eutrophication of

water bodies.

• There has been significant loss of forests in

the last 20 years, with Tanzania, Zimbabwe

and Mozambique recording the highest loss

of 403 350 ha, 327 000 ha and 217 800 ha

respectively. Malawi and Namibia recorded the

least loss of 32 950 ha and 73 600 ha respectively.

Key Findings

• Biodiversity of Mulanje Mountain, particularly

the rare and endemic Mulanje cedar

(

Widdringtonia whiteii

), is under threat from

deforestation and encroachment, poaching,

forest fires and invasive alien species.

Mulanje Mountain is a Global Biosphere

Reserve under UNESCO’s Man and Biosphere

Programme.

• The world famous Victoria Falls on the

Zambezi River between Zambia and

Zimbabwe is an important economic asset

to the two countries through tourism, but is

under some threat from upsteam dams and

other developments that pollute the river.

Victoria Falls is a UNESCOWorld Heritage Site.

• Five countries in the basin have reserved

more than 10 per cent of their total land

area for the conservation of wildlife, with

Zambia and Tanzania having 31 per cent and

28 per cent of their total land area set aside

as protected areas, respectively.

• About 74 per cent of the total energy needs

of the eight Basin states come from biomass.

• Forty hydropower schemes with a total

potential of close to 13 500 MW have been

identified, with more than half of these in

Mozambique. The estimated hydropower

potential of the Zambezi River is 20 000 MW

of which only 4 684 MW has been developed.

• The increase in carbon dioxide per capita

is concurrent with a rise in temperatures,

which has in turn altered weather patterns as

evidenced by shifting seasons within the basin,

droughts and floods, and increased incidence

of pests and diseases such as malaria.

• Regular fire outbreaks, which peak from

August to November, are a major emitter

of carbon dioxide. In Botswana, about 20 to

30 per cent of the country was burnt

between 1996 and 1997. In the Namibian

Caprivi and Kavango regions, about 25 to

30 per cent of the area burns every year.

• Climate change has impacted on the Basin’s

water resources, such as in Lake Liambezi in

Namibia, which has experienced shrinking

over the years. A major positive development

is the flowing again of Savuti river, which had

been dry for long periods of time.

• Deforestation is the most significant factor in

climate change in the Zambezi basin.