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Alan Brammer, Chris D. Thorncroft, and Jason P. Dunion

( Janiga and Thorncroft 2013 ). Therefore, regions with closed circulations at the level of the AEJ will likely not have a closed circulation above or below the vortex at this stage of the life cycle ( Wang and Hankes 2014 ). Convective activity within the AEW trough can therefore be influenced by the surrounding environment. Intensifying MCSs around the West African coastal region typically experience increased low-level southerly moisture flux associated with the downstream AEW trough ( Dieng et al

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