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Which thermal profile develops during Antarctic Bottom Water formation?

A)Surface water cools through brine rejection
B)Deep water warms from geothermal vents
C)Surface wind accelerates mixing of strata
D)Salinity stratification inhibits convective overturning

💡 Explanation

Surface water cooling causes brine rejection because salt is excluded during ice formation, increasing the density of surrounding waters; this Density-Driven Circulation then sinks to form Antarctic Bottom Water. Therefore, A is correct rather than destabilization from geothermal vents, surface mixing, or stratification.

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