Fig. 3: Spatial differences in future climate changes in DUP.
From: Capturing convection essential for projections of climate change in African dust emission

JJA dust uplift potential anomalies (m3 s–3, filled contours) and 925 mb geopotential height gradient anomalies (m, line contours) at a, c, e 0600–1200 UTC and b, d, f 1300–0300 UTC for a, b P25FC-P25, c, d CP4FC-CP4, e, f (P25FC-P25)-(CP4FC-CP4). Grey shading represents non-statistically significant differences at the 5% level.