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Which risk increases when glacial meltwater disrupts North Atlantic circulation?

A)Weakened oceanic carbon sequestration rates
B)Increased thermocline layer oxygenation
C)Strengthened deep-sea nutrient upwelling
D)More predictable coastal geostrophic currents

💡 Explanation

Reduced salinity from meltwater slows down the Thermohaline Circulation due to decreased density differences at high latitudes; this inhibits North Atlantic Deep Water formation because the density gradient weakens; therefore the ocean absorbs less CO2, rather than alternatives related to oxygen, nutrients, or coastal currents.

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