Upper Zambezi

Upper Zambezi National Park and Game Management Area covers approximately 2,460 km² in Zambia's Western Province, protecting a section of the upper Zambezi River floodplain north of Livingstone and north of the Victoria Falls area. The Game Management Area designation allows for community resource use alongside wildlife conservation. The area protects part of the Barotse floodplain system — the vast seasonal floodplain of the upper Zambezi that forms the heartland of the Lozi kingdom. The upper Zambezi here flows through an extensive floodplain of exceptional wildlife and bird value before entering the incised gorge section leading to Victoria Falls. The area encompasses some of the most significant seasonal floodplain habitats in southern Africa.

The upper Zambezi floodplain system supports exceptional wildlife. Red lechwe are the dominant antelope, wading through the shallow floodwaters in large herds. Puku, common in riparian areas, are abundant. Hippos and Nile crocodiles are plentiful in the river. Elephants range across the woodland areas adjacent to the floodplain. Buffalo are present. The floodplain is extraordinary for birds — wattled cranes, African spoonbills, straw-necked ibis, and enormous flocks of ducks and waders exploit the seasonal floodwaters. Pel's fishing owl hunts along the riverbanks. The African fish eagle is common. African skimmers nest on sandbanks in the river. Large flocks of carmine bee-eaters nest in riverbank colonies in season.

The area's vegetation is dominated by the annual flood cycle of the Zambezi. The floodplain itself is covered with aquatic and semi-aquatic grassland species, primarily Echinochloa, Vossia, and other water-tolerant grasses that provide forage for lechwe and other grazers. As floodwaters recede, a succession of plant communities establishes on the exposed wet soils, providing fresh green growth through the dry season. Mopane and Kalahari teak (Baikiaea) woodland cover the higher ground flanking the floodplain. Riparian forest of large trees lines the permanent river channels. Water lilies and other aquatic plants cover the shallower floodplain areas.

The upper Zambezi flows through the Barotse basin — a shallow structural depression overlying Kalahari sands and ancient Precambrian basement. The river's gradient in this section is extremely gentle, causing it to spread across a vast floodplain during the wet season. The floodplain sands and silts are the product of millennia of river deposition. The Kalahari Sand substrate, highly permeable, allows rapid drainage of the floodplain once river levels drop. The river channel meanders across the floodplain, with islands and channels shifting over time. The transition from the flat Barotse plain to the incised gorge leading to Victoria Falls occurs south of the park area.

The area has the semi-arid to sub-humid climate of western Zambia. Annual rainfall is 600–900 mm, falling mainly from November to April. The Zambezi River rises dramatically in response to this rainfall, flooding the plain from approximately January to May. The dry season (June–October) sees the river drop and the floodplain dry progressively, concentrating wildlife. Temperatures are hot — the dry season can see daytime highs of 40°C in October. The cool dry season (June–August) is the most comfortable for visiting. The floodplain's flood dynamics are the ecological engine driving the area's extraordinary wildlife productivity.

The Barotse floodplain is the heartland of the Lozi kingdom, one of sub-Saharan Africa's most sophisticated pre-colonial states. The Lozi developed their kingdom's governance, culture, and economy around the annual flood cycle of the Zambezi. The Kuomboka ceremony — when the Litunga (Lozi king) moves his royal barge from the flooded plain to high ground — is one of Zambia's most important cultural events, involving elaborate royal barges, drumming, and thousands of participants. The floodplain also supported traditional fishing and agriculture on the recession floodplain edge. British colonization in 1900 incorporated Barotseland under a treaty with the Lozi kingdom.

The Upper Zambezi National Park and Game Management Area was established to protect the wildlife and ecological values of the upper Zambezi floodplain while accommodating the Lozi community's traditional use of the floodplain. The Game Management Area model allows hunting (on quota), fishing, and other resource uses by communities in the buffer zone, while the national park core is more strictly protected. Management of the area has been challenging given the Lozi kingdom's parallel governance structure and the strong community rights to the floodplain. Conservation organizations have worked with the Lozi kingdom and DNPW on wildlife management.

Boat safaris on the upper Zambezi are the area's signature activity — drifting through the floodplain in a mokoro (traditional dugout canoe) or motorized boat, watching lechwe, hippos, and extraordinary birds. Sunset on the Zambezi, with the flat floodplain stretching to the horizon and the sky ablaze with color, is a quintessential African experience. The Kuomboka ceremony (usually March–April) is a once-in-a-lifetime cultural experience when attendance is possible. Fishing for tigerfish and other species is excellent. Camping on the river bank offers spectacular night sounds and dawn bird activity.

The area is accessible from Livingstone (approximately 2 hours north) or via flights to Mongu (the Western Province capital) which has connections to Lusaka. Mongu is the gateway to the Barotse floodplain. Several lodges and houseboat operations along the river provide accommodation and boat safari experiences. DNPW entry fees apply. The best time to visit is the dry season (July–October) for wildlife concentration; March–April for the Kuomboka ceremony. A 4WD vehicle is recommended for road access to the floodplain.

Upper Zambezi's conservation challenges center on balancing wildlife protection with the Lozi community's traditional rights to the floodplain. Overfishing of the Zambezi is a concern. Hippo and crocodile management alongside community fishing is an ongoing challenge. The natural flood regime of the upper Zambezi has been modified by the Itezhi-Tezhi Dam (on the Kafue tributary) and by water management in the broader basin. Climate change threatens to alter the Zambezi's flood dynamics, which are the ecological foundation of the floodplain's wildlife productivity. Community-based fisheries management programs have been developed to align community livelihoods with conservation.