The coastal belt of southern Nigeria experiences a distinct climate marked by two rainfall peaks in June and September, separated by a brief dry spell in August commonly known as the 'August Break'. Which of the following factors primarily accounts for this double rainfall maximum?
- The temporary southward movement of the Inter-Tropical Discontinuity (ITD) during mid-summerCevap
- BThe year-round dominance of the dry North-East Trade Winds over coastal southern regions
- CThe continuous influence of high orographic barriers along the Atlantic coastline
- DThe sharp drop in sea surface temperatures caused by the cold Canaries Current
Cevap
The temporary southward movement of the Inter-Tropical Discontinuity (ITD) during mid-summer primarily accounts for the double rainfall maximum in southern Nigeria.
The double rainfall maximum in southern Nigeria occurs because the moist South-West Trade Winds bring a primary peak of rainfall as the ITD migrates northwards in June/July, followed by a second peak as the ITD retreats southwards in September. In August, when the ITD is at its northernmost position, the coastal zone experiences stable air and a temporary lull in heavy rainfall known as the August Break.
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Double Rainfall Maximum and ITD Dynamics in Southern Nigeria
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