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The potential influence of Asian and African mineral dust on ice, mixed-phase and liquid water clouds

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Academic year: 2017

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Fig. 1. Circles show the locations of Asian (left) and African (right) trajectory starting points (42 per region) used in this study, superim- superim-posed on a map (adapted from Tegen, 2003) of preferential dust source areas (in blue) derived from potent
Fig. 2. Zonal and annual mean potential temperature (thin solid lines), absolute temperature (thin dashed lines), and tropopause (thick solid line)
Fig. 3. Trajectories started from 700 hPa in African dust plume regions R1 and R2 (a) and in Asian dust plume region R3 (b) that ascended to altitudes above the 450-hPa level
Fig. 4. Schematic of cloud types (Roman numerals: (i) water, (ii) mixed-phase, (iii) cirrus, (iv) COLD HET, (v) WARM HET, (vi) clear sky) and cloud formation processes (Arabic numerals: (1) WATER, (2) MPC’, (3) WARM HET, (4) MPC, (5) CIRRUS’, (6) COLD HET,
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