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The major city in the Gap is Accra . Several other cities, such as Kumasi , exist on the fringe of the Gap.


Causes of dryness


The dryness of the Dahomey Gap is unusual, given that it lies surrounded by a very wet Monsoon belt on all sides, and no mountains block moisture. Yet, Accra in the heart of the Gap receives only 720 millimetres (28 inches) of rainfall per year - less than half the amount needed to sustain tropical rainforest (which would be expected at a latitude of 6 ° N).

The cause of the dryness of the Dahomey Gap can simply be explained thus:

  • In northern Winter , high pressure centred on the Sahara sends dry northeasterly Trade Winds over West Africa, creating a general dry season, including over the Gap.


  • In northern Summer , an enormous low pressure system known as the '' Monsoon '' forms over the huge Africa-Asia-Europe landmass. Centred over approximately Rajasthan and prevented by the huge barrier of the Himalayas from moving further west, it extends a strong trough over West Africa. This trough sends warm and saturated westerly winds over West Africa, creating a wet season peaking in June on the coast (as the trough moves north) and in August inland.


  • The coast in the region of the highest rainfall ( Guinea , Sierra Leone , Liberia ) slopes from southeast to northwest. This Aspect means that the moist westerlies are forced to shed enormous quantities of moisture, allowing rainforest to thrive despite a distinct dry Season .


  • In the Dahomey Gap, however, the coast slopes in such a way (''northeast to southwest'') that the rain-bearing westerlies flow '' Parallel to the coast''. This means they are not forced to give up nearly so much moisture, and thus the climate is much drier, with only a brief rainy season in May and June. Consequently, an open savanna prevails adopted to the moderate rainfall and high Evaporation in the hot temperatures.



Geological history


The Dahomey Gap has only existed in its present form for about four thousand years. For most of the Quaternary , dry conditions due to a much colder Atlantic Ocean (aided by extensive cold currents from ice sheets in Europe and North America have meant that the present-day forest zone has supported very little or no rainforest. In Interglacial periods, however, rainfall throughout West Africa has often been so heavy that the Gap has become wet enough to support rainforest, thus eliminating the savanna.