The Okavango Delta in northern Botswana is characterised by ongoing morphological, hydrological, and ecological adjustment and change over seasonal, interannual, and longer timescales. Understanding the natural, historical range of variability in the Okavango is critically important for implementing successful management strategies. The Okavango Panhandle is a ~10 km-wide entry corridor of permanent swamps with a meandering trunk channel that is anabranching in some reaches. By using historical aerial photographs for detailed geomorphological mapping and morphological analysis of channel variables, we investigated the types and rates of change occurring in the anastomosing channels of the Okavango Panhandle. Throughout the second half of the 20th century the main Okavango channel has been progressively losing water to the Filipo channel to the east. Vegetation encroachment into the failing Okavango channel has reduced the channel width from ~40-50 m to ~20 m, whilst the Filipo channel has either remained stable or increased in channel width up to ~55 m. Changes to the water balance between channels is largely manifest in channel width changes, and there is no evidence of discernible lateral channel migration along any of the channels investigated. Given low historical rates of channel migration, meander belts likely take decades to centuries to develop, but given the current rate of vegetation encroachment along the Okavango River, we estimate that the failing Okavango channel may be blocked in various sections and essentially abandoned in the near future. Our findings have implications for the community of Sepopa and local tourism lodges that rely on the failing Okavango channel for water and transport.
|Title of host publication||WIDS2017 Dynamic Landscapes|
|Subtitle of host publication||proceedings of the Wetlands in Drylands Research Network Conference|
|Editors||Timothy J. Ralph|
|Place of Publication||Sydney, Australia|
|Number of pages||1|
|Publication status||Published - 24 Jul 2017|
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