Picture: Twitter — The Angolan highlands, the source region for the Okavango Delta, is also key to two other major river basins in sub-Saharan Africa. The area’s rich peatlands also contribute to the Congo Basin to the north and the Zambezi Basin to the east. #WorldPeatlandsDay
By Mauro Lourenco
Ask most people what they picture when thinking about natural “carbon sinks” – ecosystems that absorb and store greenhouse gases – and they’ll probably describe a forest. Reforestation is a common feature of climate change plans.
But there’s another equally important, often overlooked type of natural carbon sink: peatlands. These are a particular type of wetland ecosystem in which dark, loamy peat soil is produced. Peatlands store more carbon than all the world’s forests combined.
And they do more than store carbon. They conserve biodiversity, purify water and reduce flooding and soil erosion. They also play an important role in agriculture – they’re good for planting certain crops, such as potatoes and carrots.
Despite this, even global scientific bodies have not paid much attention to peatlands until very recently. Global maps and inventories of peatlands are inconsistent, though there is more data for the northern hemisphere compared to the southern hemisphere and the tropics. High quality peatland extent data are only available for a small selection of countries and regions, including Canada, Sweden and West Siberia.
This gap needs to be filled urgently: discovering, quantifying and protecting new peatland deposits is necessary in an uncertain climate future that depends on intact, natural carbon sinks.
That’s why, for my PhD, I set out to quantify and map recently discovered peatland deposits in the drastically understudied Angolan Highlands. This region is hydrologically and ecologically important. One of the reasons is that it’s the primary source of water flowing into the Okavango Delta, a UNESCO world heritage site, in north-west Botswana. The Okavango is a flat, extensive and seasonally flooded alluvial fan that is one of very few large inland delta systems that do not drain into the ocean. Instead, it drains into the desert sands of the Kalahari Basin.
I worked alongside my PhD supervisors, Professor Jennifer Fitchett and Professor Stephan Woodborne, using remote sensing to estimate that there are about 1,634 km² – that’s approximately 230,000 full-sized soccer fields – of peatland in the Angolan Highlands.
It’s a conservative figure, since the mapped area spans just 16 percent of the Angolan Highlands and 4 percent of Angola. For comparison, the largest tropical (and African) peatland deposit, which was also recently mapped in the Democratic Republic of the Congo in the Congo Basin, spans 145,000 km².
This is the first estimate of peatland coverage in Angola. And the study reveals potentially more tropical peatland deposits to discover in the highlands region and surrounding river basins.
In 2015 the National Geographic Okavango Wilderness Project was launched to create a network of newly protected areas to conserve the length of the Okavango Catchment. It has been surveying and collecting scientific data on the river system and working with local communities; NGOs; and the governments of Angola, Namibia, and Botswana to secure permanent, sustainable protection for the greater Okavango Watershed.
The Okavango Delta is dependent on precipitation occurring in the highlands of central Angola, where water flows south into the Okavango River from two tributaries: the Cuito River and Cubango River. The greater Okavango Catchment encompassing these three rivers covers approximately 112,000 km² and spans three countries – Angola, Namibia, and Botswana.
The source waters originate from areas which experienced historical conflicts and wars, and remain unprotected by legislation. The National Geographic Okavango Wilderness Project was created because of concerns about threats to the Angolan region of the Okavango catchment, and the potential downstream consequences to the Okavango Delta.
Mauro Lourenco is a PhD student at the University of the Witwatersrand, South Africa
This article was first published on The Conversation