The Okavango Delta flood cycle
37 years of satellite data, one interactive map
Watch Africa’s largest inland delta transform month by month as floodwaters from Angola’s highlands spread across the Kalahari. Satellite data from 37 years of Landsat observations reveals the delta’s seasonal pulse.
Understanding the Okavango Delta flood cycle
The Okavango Delta’s annual flood cycle is one of the most counterintuitive natural events in Africa. While most river systems flood during the local rainy season, the Okavango does the opposite — its waters peak in the middle of the dry season, when rainfall in Botswana has stopped entirely and the surrounding Kalahari is at its most parched. It’s this paradox that makes the delta one of the most dynamic safari destinations on the continent, and understanding the cycle is the key to planning when — and where — to visit.
The story begins over 1,000 kilometres to the northwest, in Angola’s central highlands. Summer rains between November and March feed the Cubango and Cuito rivers, which merge to form the Okavango. That water then makes a slow, four-month journey south — through Namibia’s Zambezi Region (still widely known as the Caprivi Strip) and into Botswana at the Panhandle, the narrow upper section of the delta. By April, the flood pulse enters the main delta fan, and the landscape begins to change.
What happens next is extraordinary. Dry floodplains fill with crystal-clear water. Channels that were bone-dry weeks earlier become deep enough for mokoro and motorboats. The surrounding desert vegetation gives way to lush, water-filled grasslands, and wildlife concentrates in enormous numbers along the advancing flood front. By July, satellite data shows the delta’s visible open water reaching over 7,000 km² — roughly fourteen times the area visible during the driest months. Then, just as steadily, the water retreats southward, and the cycle begins again.
No two years are the same
If you’re using this map to plan a trip, it’s worth knowing that the flood extent shown for each month represents a long-term average — the area where satellite data has detected water in at least 20% of years for that calendar month, drawn from 37 years of Landsat observations. It gives you a reliable picture of the delta’s typical seasonal rhythm, but individual years can vary significantly.
The scale of the flood depends primarily on rainfall in the Angolan highlands, which fluctuates from year to year. The period between 2010 and 2012 saw some of the largest floods in recent memory, filling channels and lagoons that had been dry for decades and even pushing water into Lake Ngami for the first time since the 1980s. By contrast, the 2019 flood season was among the lowest on record, with significantly reduced water coverage across the delta. These variations affect everything from which camps can offer water-based activities to which concession areas deliver the best game viewing in a given year.
What the flood means for your safari
The flood cycle isn’t just a geographical curiosity — it’s the single most important factor shaping your Okavango experience. It determines which activities are available, where the wildlife concentrates, and what the landscape looks and feels like at any given time of year.
During high water (roughly May to September), the delta is at its most visually spectacular. Mokoro excursions glide through lily-covered channels, motorboat safaris open up areas inaccessible by land, and the contrast between the flooded delta and the bone-dry Kalahari is at its most dramatic. Game drives still run on the larger islands and higher ground, and predator sightings improve steadily as the dry season progresses and vegetation thins.
As the water retreats (September to November), the remaining pools and channels become magnets for wildlife. This is when you’ll see the most intense predator-prey interactions — animals crowding around shrinking water sources with nowhere to hide. It’s raw, dramatic, and visually arresting, though the heat (regularly exceeding 40°C in October) is not for everyone.
The wet season (November to March) brings a different delta entirely. The landscape turns vivid green, over 200 migratory bird species arrive from Europe and North Africa, and antelope calving season attracts predators. Visitor numbers drop, rates are lower, and you may have your camp — and your sightings — largely to yourself. For a detailed month-by-month breakdown, see our guide to the best time to visit the Okavango Delta.
A system under pressure
The Okavango Delta’s flood cycle depends on an unbroken chain of water flowing from Angola through Namibia and into Botswana. That chain is increasingly under scrutiny. Proposed water extraction projects upstream — including irrigation schemes in Angola and a debated hydropower station in Namibia — could reduce the volume of water reaching the delta. Climate modelling suggests the Okavango catchment is likely to experience decreasing annual rainfall and rising temperatures in the coming decades.
For now, the delta remains remarkably intact — one of the few large wetland systems in the world that functions much as it has for thousands of years. Botswana’s concession model, in which tourism revenue directly funds conservation and community livelihoods, has been central to that protection. Every visit to the Okavango contributes to the economic case for keeping this extraordinary system alive.
About the data
This interactive map draws on the European Commission’s Joint Research Centre Global Surface Water dataset, produced in partnership with Google. The underlying data spans 37 years of Landsat satellite imagery (1984–2021), with each 30-metre pixel classified as water or non-water across every month of the observation period. The flood extents shown represent the monthly recurrence — areas where water has been detected in at least 20% of years for a given calendar month. The open water figures (in km²) are calculated directly from the satellite-derived polygons displayed on the map.
Frequently asked questions
Why does the Okavango Delta flood in the dry season?
Because the floodwaters originate from summer rainfall in Angola’s highlands, over 1,000 km to the northwest. The water takes roughly four months to travel south through Namibia and into the delta, arriving in Botswana between March and May — well after the local rains have stopped. The result is a peak flood in the middle of Botswana’s dry winter, which is what makes the delta so unusual among the world’s wetland systems.
How big does the Okavango Delta get?
At its driest (typically January to February), the delta’s visible open water covers roughly 500–700 km². At peak flood (July), that figure rises to over 7,000 km² — an increase of more than tenfold. The total area of land that is seasonally or permanently inundated, including water beneath vegetation that satellites cannot detect, is larger still, with estimates ranging from 6,000 to 15,000 km² depending on the year and methodology.
Does the Okavango Delta flood every year?
Yes, though the extent varies considerably. Years of heavy rainfall in Angola produce large floods that fill channels and lagoons across the delta, while low-rainfall years result in significantly reduced coverage. The 2010–2012 period saw exceptionally high floods; 2019 was among the lowest on record. The overall pattern — rising water from March, peaking around July, retreating by November — is consistent, but the magnitude is not.
When is the best time to see the flood?
The flood is at its most visually spectacular from June to August, when water levels are highest, skies are clear, and temperatures are pleasant. May and September offer a similar experience with fewer visitors and lower rates. For the full picture, explore the month-by-month breakdown on the map above or read our best time to visit guide.
