Our Insight into Botswana's Dynamic Seasonal Waterways

OUR INSIGHT INTO BOTSWANA’S DYNAMIC SEASONAL WATERWAYS

This year, Botswana has experienced above-average rainfall both locally and across the Angolan Highlands catchment. As a result, we predict a stronger-than-usual annual rise in water. Already, the shifts on the ground are remarkable, with high localised rainfall beginning to echo the early stages of one of the planet’s most extraordinary ecological phenomena: Botswana’s dynamic seasonal waterways.

A high water year like 2026 is not a disruption, but an ecological renewal driven by one of Africa’s most vital natural processes.

What this means for the regions we call home, game viewing, and travelers? Botswana’s water becomes part of the story in and of itself: the desert and the delta in full expression. A time of ecological abundance and intensity, renewal, expansion, and connectivity. A rare opportunity to witness the country wide awake, and to engage with the wild as it is meant to be seen: alive. In this newsletter, we summarize Botswana’s greatest miracles in motion, from The Desert to The Delta.

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The Desert

Botswana’s desert systems are shaped primarily by rainfall, but some years, exceptional localized rainfall transforms the landscape in ways that are incredibly special to witness.

This is a season of striking contrasts and rare transition. Rainfall has already triggered widespread greening in the Kalahari and the Makgadikgadi. Typically dry grasslands are rich with growth, offering a desert experience few others get to witness. The land is thriving, the days are cooler, and game viewing is defined by dynamism. In Savuti, expanding marshes are sustained by rising groundwater and regional rainfall, even while channel flows remain unpredictable. Fuller waterholes mean migratory species are lingering longer, joining resident wildlife for epic viewing opportunities. The ancient riverbed in front of Leroo La Tau flows for the first time since 2020/21.

The impact of the Boteti’s return of flowing water on Africa’s second-largest zebra migration will unfold in real time from April, when zebras typically start arriving in their thousands. 2026 Rainfall impacts the landscape in ways that are both immediate and lasting. Seasonal rivers recharge underground water reserves, ephemeral pans hold water for longer, and grasses establish more deeply rooted growth that will support wildlife well into the dry season. When rainfall subsides and animals reconcentrate along remaining water sources, it will likely be in higher densities because of this. This leads to strong herbivore condition, increased movement patterns, and stable—often intensified—predator activity.

The Delta

Botswana’s seasonal rise in water is expressing itself earlier than usual, spreading more widely, and creating increasingly connected channel systems.

For travelers, this is a time when the Delta reveals its full character. From the Panhandle to Moremi and Khwai, the landscape itself becomes part of the experience: reflections, open floodplains, and waterways in their prime. Chobe is influenced by both upstream flow and downstream pressure from the Zambezi River (what has made the Chobe River famous for “flowing in two directions at once”). Wildlife is not absent; it is highly responsive to these conditions. Game viewing and all Delta activities expand with the water. Mokoro excursions explore new shallow channels. Boating expands into deeper lagoons.

Walking safaris enter a new world of island abundance. Rainfall subsides when seasonal water rising gains momentum and the physical landscape transforms once more. Channels deepen further, additional lagoons reconnect, and nutrient-rich silt settles across the floodplains, stabilising soils and stimulating aquatic plant growth. Over time, this renewed inundation redefines the intricate mosaic of islands, channels, and wetlands—sustaining the Delta’s extraordinary pulse of water, driving ecological productivity, improving wildlife survival rates, and creating rare, high-water opportunities for guests