Simulations of the observed ‘jump’ in the West African monsoon and its underlying dynamics using the MIT regional climate model
The observed seasonal migration of rainfall associated with the West African monsoon (WAM) is characterized by two regimes of relatively intense rainfall: an early, intense peak over the Guinean Coast during late May to early July; and a late, less-intense peak over the Sahel during mid-July to mid-...
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Wiley Blackwell
2018
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| Online Access: | http://hdl.handle.net/1721.1/117277 https://orcid.org/0000-0002-6148-7997 |