Impact of the Sudd wetland on the Nile hydroclimatology

doi:doi:10.1029/2004WR003792

Abstract

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Abstract

Impact of the Sudd wetland on the Nile hydroclimatology

Y. A. Mohamed

UNESCO-IHE Institute for Water Education, Delft, Netherlands

B. J. J. M. van den Hurk

Koninklijk Nederlands Meteorologisch Instituut, De Bilt, Netherlands

H. H. G. Savenije

UNESCO-IHE Institute for Water Education, Delft, Netherlands

W. G. M. Bastiaanssen

International Institute for Aerospace Survey and Earth Sciences, Enschede, Netherlands

Large evaporation occurs over the Sudd wetland, a huge swamp located on the upper Nile. Historically, water resources planners have had the intention to reduce the Sudd evaporation by shortcut channels (e.g., Jonglei canal). The question is: What is the effect of draining the Sudd wetland on the regional water cycle and on the Nile water flow? A regional climate model has been applied to the Nile Basin, with a special modification to include routing of the Nile flood over the Sudd. The impact of the wetland on the Nile hydroclimatology has been studied by comparing two model scenarios: the present climatology and a drained Sudd scenario. The results indicate that draining the entire Sudd has negligible impact on the regional water cycle owing to the relatively small area covered by the wetland. The runoff gain would then be up to ∼36 Gm³ yr⁻¹. However, the impact on the microclimate is large. The relative humidity will drop by 30–40% during the dry season, and temperature will rise by 4°–6°C. The impact during the wet season is small.

Received 6 November 2004; accepted 18 May 2005; published 23 August 2005.

Citation: Mohamed, Y. A., B. J. J. M. van den Hurk, H. H. G. Savenije, and W. G. M. Bastiaanssen (2005), Impact of the Sudd wetland on the Nile hydroclimatology, Water Resour. Res., 41, W08420, doi:10.1029/2004WR003792.

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