The Zambezi Basin

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The north of the Zambezi basin has mean annual rainfall of 1100 to 1400 mm which declines to the south, reaching about half that figure in the south-west. The rain falls in a 4 to 6 month rainy season when the Inter-Tropical Convergence Zone moves over the basin from the north. Evaporation rates are high (1600mm−2300 mm) and much water is lost through evaporation in swamps and flood plains, especially in the east and south-east of the basin.

Tributaries, their basin areas, discharge rates, and region drained

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Data from this reference.[1]

Upper Zambezi: 507200 km², discharges 1044 m³/s at Victoria Falls, comprising:

Northern Highlands catchment, 222,570 km², 850 m³/s at Lukulu
Central Plains catchment, 284,630 km², 196 m³/s (Victoria Falls-Lukulu)

Middle Zambezi cumulatively 1,050,000 km², 2442 m³/s, measured at Cahora Bassa Gorge

(Middle section by itself: 542,800 km², discharges 1398 m³/s (C. Bassa-Victoria Falls)
Gwembe Catchment, 156,600 km², 232 m³/s (Kariba Gorge-Vic Falls)
Kariba to C. Bassa catchment, 386200 km², 1166 m³/s (C. Bassa-Kariba Gorge)

Lower Zambezi cumulatively, 1,378,000 km², 3424 m³/s, measured at Marromeu

(Lower section by itself: 328,000 km², 982 m³/s (Marromeu-C. Bassa))
Zambezi Delta, 12,000 km²

TOTAL ZAMBEZI RIVER BASIN: 1,390,000 km², 3424 m³/s discharged into delta

Note that northern tributaries contribute much more water than southern ones, for example: Northern Highlands catchment of upper Zambezi 25%, Kafue 8%, Luangwa and Shire Rivers 16% each, total 65%. The large Cuando basin in the south-east contributes only about 2 m³/s because most is lost through evaporation in its swamp systems.[1]

  1. ^ a b Richard Beilfuss & David dos Santos: Patterns of Hydrological Change in the Zambezi Delta, Mozambique. Working Paper No 2 Program for the Sustainable Management of Cahora Bassa Dam and The Lower Zambezi Valley (2001)