Southern Nigeria's coastal regions experience a double rainfall maximum with a noticeable drop in precipitation during July and August known as the 'August Break' (Little Dry Season). Which atmospheric mechanism accounts for this temporary dry spell while the Inter-Tropical Convergence Zone (ITCZ) is located at its northernmost position over West Africa?
- AThe deflection of rain-bearing South-West Monsoon winds away from the Atlantic coast toward the Jos Plateau due to orographic suction.
- The inland migration of the ITCZ deep into northern Nigeria, placing coastal areas under stable marine air with lower sea surface temperatures and atmospheric divergence.Answer
- CThe temporary southward surge of the dry North-East Trade Winds bringing Continental Tropical (cT) air across southern Nigeria.
- DThe complete weakening and collapse of the Tropical Maritime (mT) air mass over the Gulf of Guinea during the summer solstice.
Answer
The inland migration of the ITCZ deep into northern Nigeria, placing coastal areas under stable marine air with lower sea surface temperatures and atmospheric divergence.
The correct option identifies that as the ITCZ advances to its northernmost position over West Africa during July and August, southern Nigeria is positioned well behind the main convective rain belt. Localized oceanic upwelling along the Gulf of Guinea brings cooler water to the coast, creating atmospheric stability, subsidence, and divergence that temporarily suppresses rain-producing convective clouds in the south.
Step-by-Step Solution
Key Concept
Atmospheric mechanisms underlying the double rainfall maximum and August Break in Southern Nigeria
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