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M. Issa Lélé, Lance M. Leslie, and Peter J. Lamb

equator in the Atlantic Ocean is the primary source of water vapor for the region. The mean southwest transport from these latitudes reaches a maximum around 12°N. It has a well-demarcated region of strong flow, referred to in this study as the “moisture river.” This strong flow originates from the equatorial South Atlantic, moves northeastward across the equator, passes over the Gulf of Guinea region, and then supplies moisture to the central Sudan region. The enhanced southwesterly transport is

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Zewdu T. Segele, Michael B. Richman, Lance M. Leslie, and Peter J. Lamb

. Zaitchik , and A. Dezfuli , 2014 : Subseasonal analysis of precipitation variability in the Blue Nile river basin . J. Climate , 27 , 325 – 344 , doi: 10.1175/JCLI-D-13-00094.1 . Block , P. , and B. Rajagopalan , 2007 : Interannual variability and ensemble forecast of Upper Blue Nile Basin Kiremt season precipitation . J. Hydrometeor., 8, 327–343 , doi: 10.1175/JHM580.1 . Bohn , T. J. , M. Y. Sonessa , and D. P. Lettenmaier , 2010 : Seasonal hydrologic forecasting: Do

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