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. 2022 Oct 27;58(11):e2021WR031721. doi: 10.1029/2021WR031721

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© 2022 The Authors.

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(a) Annual P (mm) over the Senegal basin between 1981 and 2016; (b and c) Annual contribution of E _t to P in mm and fractional contribution to total rainfall, respectively. Full line represents local sources, dashed line represents remote sources; (d and e) Annual contribution of E _d in mm and fractional contribution to total rainfall, respectively. Full line represents local sources, dashed line represents remote sources. (f and g) Annual contribution of ocean E to P in mm and fractional contribution to total rainfall, respectively. Note the different scaling of the x‐axes corresponding to local (left y‐axis) and remote (right y‐axis) sources of E _t and E _d contributions.