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Which consequence results when deep ocean currents slow?

A)Reduced nutrient upwelling to surface
B)Increased coastal erosion from waves
C)Decreased global average precipitation
D)Weakened thermocline layer formation

💡 Explanation

Slower deep ocean currents reduce the rate of nutrient upwelling because thermohaline circulation brings nutrient-rich water upwards. Therefore, nutrient availability decreases at the surface, rather than increased erosion due to wave action or decreased overall precipitation.

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