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← GeographyWhich 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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