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A sensitivity study on the role of the swamps of southern Sudan in the summer climate of North Africa using a regional climate model

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Abstract

We used the regional climate model RegCM3 to investigate the role of the swamps of southern Sudan in affecting the climate of the surrounding region. Towards this end, we first assessed the performance of a high resolution version of the model over northern Africa. RegCM3 shows a good skill in simulating the climatology of rainfall and temperature patterns as well as the related circulation features during the summer season, outperforming previous coarser resolution applications of the model over this region. Sensitivity experiments reveal that, relative to bare soil conditions, the swamps act to locally modify the surface energy budget primarily through an increase of surface latent heat flux. Existence of the swamps leads to lower ground temperature (up to 2 °C), a larger north–south temperature gradient, and increased local rainfall (up to 40 %). Of particular importance is the impact on rainfall in the surrounding regions. The swamps have almost no impact on the rainfall over the source region of the Nile in Ethiopia or in the Sahel region; however, they favor wetter conditions over central Sudan (up to 15 %) in comparison to the bare desert soil conditions.

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Acknowledgments

This work has been supported by the Earth System Physics (ESP) in the International Centre for Theoretical Physics (ICTP), the STEP program, and the International Atomic Energy Agency (IAEA). The authors would like to acknowledge Dr. Gulilat Diro, Dr. Erika Coppola, and Dr. Laura Mariotti for their support in using the model and sharing their modeling calibration and experience. Finally, the authors would like to thank all the staff of the ESP and the RegCM team for their support.

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Correspondence to Modathir A. H. Zaroug.

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Zaroug, M.A.H., Sylla, M.B., Giorgi, F. et al. A sensitivity study on the role of the swamps of southern Sudan in the summer climate of North Africa using a regional climate model. Theor Appl Climatol 113, 63–81 (2013). https://doi.org/10.1007/s00704-012-0751-6

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