Africa has the largest landmass
of all continents around the equator and extents from Tunisia at 37°21′ N to Cape Alghulas in South Africa
at 34°51′15″ S. Climate is largely
determined by latitude – and in particular a locations position in relation to
the moving Intertropical Convergence Zone (ITCZ). Rainfall follows the ITCZ,
leaving the areas adjacent to it dry (see role of Hadley cells in distribution
of rainfall here) and generally explains the humid tropic climates, and (semi-)
arid climates of the subtropics.
However, the ITCZ does not remain in place. Over a year, the zone moves
north and south following the Sun’s zenith point on Earth. The movement is
more subtle over the oceans, more defined over land-masses like Africa. Please
follow the link to a visualisation of the annual ITCZ migration. As clearly
shown, regions located between the northernest and southernest location
experience rainfall in much of the year, whereas higher latitude
locations will only ‘get in touch’ with the ITCZ once a year. This explains
the 1) rainfall variability throughout the average year and 2) rainfall
variability between different latitude locations. For more maps, see my
introductory post please!
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