Answer:
Option A: They create density differences that cause dense deepwater currents to flow toward the equator where they displace less dense, warmer water above them.
Step-by-step explanation
Temperature and salinity affect deepwater currents by creating density differences in the ocean water. Cold and salty water is denser than warm and less salty water. This denser deepwater tends to flow toward the equator, where it displaces the less dense, warmer water above it, leading to the circulation patterns observed in the ocean. This process is an essential component of the thermohaline circulation system, also known as the "Great Ocean Conveyor Belt."