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Daily Levels of the Harmattan Dust near the Gulf of Guinea over 15 Years: 1996 2011

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Figure

Figure 1b.  A typical Harmattan trajectory derived from NOAA HYSPLIT model of 96 h (4-day) backward trajectory of winds ending in the Bodele depression on Jan
Figure 1c.  Typical wind streamlines during winter in West Africa, derived from NOAA ARL
Table 1.  The Harmattan dust average particle number concentration at Kumasi, Ghana (1996-2011)
Figure 3a.  Mean daily particle mass concentration distribution at Kumasi, 1996-2011
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