Deep-ocean currents, also known as thermohaline circulation, are primarily driven by differences in water temperature and salinity. This phenomenon is part of the global ocean conveyor belt, which plays a crucial role in regulating the Earth's climate. Let's explore how water temperature influences these currents:
- Water Temperature: Temperature differences lead to variations in water density. Colder water is denser than warmer water, causing it to sink. This sinking motion is a key driver of deep-ocean currents. As the cold, dense water moves along the ocean floor, it pushes warmer, less dense water upwards, creating a continuous flow and circulation pattern.
Therefore,
water temperature is the correct factor influencing deep-ocean currents, as it directly affects water density and the movement of oceanic waters across the globe.