Which airflow pattern alteration occurs when air ascends rapidly at the Intertropical Convergence Zone?

💡 Explanation

When rapid air ascent occurs at the ITCZ, vertical motion dominates over horizontal, weakening the Coriolis effect aloft because the deflection only occurs with sustained horizontal movement. Therefore, the Coriolis effect weakens, rather than albedo reduction, ozone loss, or jet stream convergence which are caused by different atmospheric mechanisms.

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