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Which process limits coastal upwelling efficiency during El Niño events?

A)Thermocline deepening inhibits nutrient transport
B)Trade wind intensification increases stratification
C)Equatorial countercurrent strengthens surface divergence
D)Rossby wave propagation enhances coastal downwelling

💡 Explanation

During El Niño, weakened trade winds cause the thermocline to deepen, diminishing the upwelling of nutrient-rich deep waters because vertical mixing is suppressed. Therefore thermocline deepening restricts coastal upwelling, rather than stronger winds, surface divergence, and downwelling which exacerbate upwelling under normal conditions.

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