True
Convection Currents.
Continents can block the flow of surface currents, creating barriers that deflect the currents in different directions. They can also influence the direction and speed of currents by shaping the coastlines and creating deep ocean basins that can channel currents. Additionally, continents can impact the distribution of heat and moisture, which can affect the intensity and direction of surface currents.
The western coasts of continents tend to be warmer than the eastern coasts because of ocean currents. In the Northern Hemisphere, warm ocean currents move from the equator towards the poles along western coastlines, raising temperatures. Meanwhile, cold ocean currents flow from the poles towards the equator along eastern coastlines, bringing cooler temperatures.
Ocean currents are deflected to the right in the Northern Hemisphere due to the Coriolis effect, a result of the Earth's rotation. As water moves northwards, it is deflected to the right, creating clockwise-flowing currents.
Mantle convection currents beneath a continental-continental convergent boundary would likely be disrupted and deflected due to the collision of the continental plates. This collision would create intense compression and thickening of the crust, altering the flow patterns and direction of the mantle convection currents in the affected region.
The coriolis effect makes ocean currents move in a curved path.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
Eastern boundary currents in gyres are broad and shallow, with slow, wide flows and transport cold water towards the equator. Western boundary currents, on the other hand, are narrow and deep, with fast, concentrated flows that transport warm water away from the equator. Eastern boundary currents often have higher productivity due to upwelling, while western boundary currents are associated with strong western intensification.
The movement of Earth's plates and continents can cause changes in sea level, ocean currents, and the distribution of marine life. It can also affect the shape of ocean basins and the location of coastlines.
In the northern hemisphere, the Coriolis effect causes ocean currents to be deflected to the right. In the southern hemisphere, the Coriolis effect causes ocean currents to be deflected to the left. This deflection leads to the clockwise rotation of ocean currents in the northern hemisphere and counterclockwise rotation in the southern hemisphere.